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Journal articles on the topic 'Gabrovo'
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1
Donkov, Lazar. "Parc-musée ethnographique Etar, Gabrovo." Museum International (Edition Francaise) 28, no. 1 (April 24, 2009): 9–14. http://dx.doi.org/10.1111/j.1755-5825.1976.tb01468.x.
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Hinkova, Nikolinka, and Nikolay Nenov. "Enhancing the General and Special Skills of Students." Environment. Technology. Resources. Proceedings of the International Scientific and Practical Conference 3 (August 9, 2015): 16. http://dx.doi.org/10.17770/etr2013vol3.871.
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Sapunov, Ivo, Platon Tchoumatchenco, and Vladimir Shopov. "Jurassic stratigraphy and geodynamics in the eastern part of the Central Balkan Mountains (Gabrovo and Kazanluk Districts), Bulgaria." Geologica Balcanica 29, no. 3-4 (December 30, 1999): 3–24. http://dx.doi.org/10.52321/geolbalc.29.3-4.3.
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Seven instructive Jurassic sections in the Gabrovo and the Kazanluk Districts are described. It was established that in the Gabrovo District the lower part of the Ozirovo Formation belongs to the Lower Sinemurian, and the underlying Kostina Formation to the Hettangian. In the Kazanluk District (section in the locality Ikischa) the lower part of the Ozirovo Formation belongs to the Lower Pliensbachian, and the Kostina Formation to the Upper Sinemurian. The sections in the Gabrovo District are situated within the limits of the Kostina Step (second order block) of the Izdremets Complex Graben of the Moesian Early- Middle Jurassic Platform. The sections in the Kazanluk District are situated within the Neshkovtsi Step of the same graben. The marine ingression on the Moesian Early-Middle Jurassic Platform began during the Hettangian with the most descended Kostina Step. The sea advanced from the Toundzha Fault-Angle Valley. During the Sinemurian and the Early Pliensbachian the ingression expanded and covered all the rest, more uplifted steps of the Izdremets Graben. The sea gradually overflowed the Sevlievo Graben and the western part of the Veliko Turnovo Graben of the Moesian Early-Middle Jurassic Platform. At the initial stage of the marine ingression the supplying dryland was active, therefore quite shallow water terrigenousclastic sediments and very little amount of more or less sandy calcareous silts with bioclasts were deposited. Later on (at the end of the Sinemurian and in the beginning of the Pliensbachian) the calcareous silts began to prevail over the terrigenous sediments, the shallow-water environments having remained. More or less significant Middle Jurassic and Early Jurassic stratigraphic breaks were established in all of the described sections. They realized in marine conditions. Strong submarine currents led to a marine abrasion. As a result, condensed Middle-Upper Callovian limestones lie at present over Lower Bajocian or Lower Sinemurian sediments, or directly overlay Upper Triassic rocks. In the section near the Sokolski Monastery, Gabrovo District, Middle Kimmeridgian limy shales to marls and a quite limited amount of thin layered limy sandstone intercalations directly overlie Lower Sinemurian, sandy bioclastic limestones.
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Minkovska, Pavlina, and Tatiana Drenska. "DEVELOPMENT OF AUTHOR’S CURRICULUM IN CIVIC EDUCATION “ME AND GABROVO”." Education and Technologies Journal 12, no. 2 (August 1, 2021): 385–89. http://dx.doi.org/10.26883/2010.212.3541.
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Our reasons for choosing and developing the scope of this Program is our understanding of the need for children to acquire a set of knowledge, skills and attitudes to the world around us and specifically to the city in which we live through modern pedagogical strategies, techniques, approaches and methods in the conditions of application of an interdisciplinary complex, implemented in all age groups, integrated in additional forms of pedagogical interaction, as an independent educational field in an author’s program system, and is aimed at acquiring social, civic and intercultural competencies and competencies related to health and maintaining a sustainable environment. We pay special attention to work with children with SEN and children from vulnerable groups. Determining the expected results will be the framework requirements for the results of civic education for preschool education according to the texts of Ordinance № 13 of 21.09.2016 on civil, health, environmental and intercultural education, with at least two areas of competence in each additional form. Key importance and emphasis in the Program are partnership interactions with Gabrovo cultural, educational and other institutions for enrichment of the educational process in the kindergarten.
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Tsonkov, Nikolay. "Challenges and opportunities for green economy transformation of Gabrovo District." SHS Web of Conferences 120 (2021): 01007. http://dx.doi.org/10.1051/shsconf/202112001007.
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The process of restructuring European economies has begun over the last decade. This process is related to the implementation of strategies and policies at all levels in the countries for sustainable development in context of climate change and reduction of natural resources usage. Logically, European course to decarbonizing economies was adopted two years ago. In this regard, it is important to monitor the transition of the economies of individual countries and regions to neutrality and what problems arise. In this sense, Bulgaria is part of this process, and it is important to develop policies, aiming to reformulate regional policy and achieving sustainable development of the Bulgarian regions. The aim of the present research is to analyze the state of the economy in Gabrovo district in the context of the concept of sustainable development and outlining the difficulties and opportunities of the local economy in the transition to neutrality. The author achieves the goal, using various approaches and research methods - systematic, territorial approaches and descriptive, comparative, statistical and other methods.
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Amtonova, Alexandra. "Second Lecture on the Bulgarian Literary Critic’s Digital Library Project." Bulgarski Ezik i Literatura-Bulgarian Language and Literature 64, no. 4 (August 2, 2022): 429–32. http://dx.doi.org/10.53656/bel2022-4-9-digaa.
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The scientific report presents the lecture given to 11th grade students at the National Aprilov High School – Gabrovo, which compared the thematic accents and structural features of two literary-historical portraits of Vasil Aprilov, created by two critics from two literary generations – Boyan Penev and Georgi Konstantinov. The students were shown the intentions and techniques of the literary-historical portrait, the influence of temporal distance on its structure and language, the artistic value of the authentic document.
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Medarov, Georgi K. "Crises in Official and Popular Festivities: on the Cases of Gabrovo, Varshets and Kosti." Postmodernism Problems 12, no. 1 (April 3, 2022): 7–31. http://dx.doi.org/10.46324/pmp2201007.
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The article analyzes the potential of local festivals to serve as an instrument to overcome crises in three particular case studies, namely Gavrovo's Festival of Humour and Satire, Varshets' Resort, Mineral Water and the Balkan Mountains Festival and Kosti's fire dancing. The analysis is based on the results of an empirical research conducted in the summer of 2021 within the project “Local festivals: a resource of local communities for crisis management,” supported by the Bulgarian National Science Fund. The main argument is that in all of these cases the festivals cannot be subsumed under the logic of coping with economic underdevelopment. Nevertheless, the festivals have a direct effect on coping with the coronavirus crises both in terms of the practical realization of its irreversibility, as well as in terms of using it as a medium to renegotiate local contradictions and conflicts. Lastly, the article demonstrates the efficacy (and limits) of Bakhtin's theory of the carnavalesque for the understanding of local festivals' role in coping with crises.
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Ntolou, Kalliopi, Jacob Fantidis, Despoina Parasyri, and Panagiotis Kogias. "Machine Building and Mechatronics Field in The Industry 4 for 5 Regions in Europe." Journal of CIEES 2, no. 1 (July 22, 2022): 44–48. http://dx.doi.org/10.48149/jciees.2022.2.1.7.
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The article presents the needs for professional training of technicians and engineers in mechanical engineering and mechatronics was conducted in two areas of Bulgaria - Gabrovo and Plovdiv, Kavala, Greece, Pomorskie Region, Poland and Nis region, Serbia. These regions are very different, both in area and population and the most developed sectors of the economy. The survey was realized under an Erasmus+ KA2 programme which duration from 1.09.2020 up to 31.08.2022 with title Active Learning Community for Upskilling Technicians and Engineers. This works presents the basic data about the training proposals both for engineers and technicians. Last but not least illustrates the preferences of companies about the most suitable training method.
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Lazov, Lybomir, and Nikolay Angelov. "Application of the Multicomponent Method of Assessment o f Student ’ s Progress in Physics." Environment. Technology. Resources. Proceedings of the International Scientific and Practical Conference 3 (August 9, 2015): 26. http://dx.doi.org/10.17770/etr2013vol3.874.
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The multicomponent method of assessing the progress in physics of students from the Technical University of Gabrovo is discussed in the paper. It is shown that tests papers as a modern form of examining students can successfully be combined with other traditional forms of examination. In that way the teacher can get important feedback on how students understand lectures and laboratory teaching material during the semester and to adjust their work so that they can in time adapt to the necessary level. Thus, students are actively involved in the learning process, which improves the results they show at the final exam. These conclusions are based on the results of the last decade, ever since the method was introduced.
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Muchinov, Ventsislav. "Impact of the Changes in the Administrative and Territorial Structure of the Ottoman Empire on the Development of Cities in the Bulgarian Lands During the 19th Century (Until 1878)." Epohi 30, no. 1 (June 29, 2022): 34–48. http://dx.doi.org/10.54664/pjcb9715.
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During the 19th century, significant changes occurred in the administrative and territorial structure of the Balkan provinces of the Ottoman Empire. The article analyzes the impact that these changes have had on the development of cities in the Bulgarian lands under Ottoman rule. The administrative rise of cities, such as Plovdiv, Bitola, and Ruschuk (Ruse), stimulated their economic and demographic development instead of other urban centres that were important in the past, such as Sofia, Nikopol, and Silistra. At the local level, the changes in the Ottoman administrative system have also had a significant impact, contributing to the upward development of settlements proclaimed as cities in the Stara Planina, Sredna Gora, and Sub-Balkan regions, such as Gabrovo, Koprivshtitsa, Panagyurishte, etc.
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Petrova, Desislava, and Lyubomir Lazov. "HIGHER EDUCATION IN THE REPUBLIC OF BULGARIA AT THE CROSSROAD - PROBLEMS AND MEASURES TO PREVENT THEM." SOCIETY. INTEGRATION. EDUCATION. Proceedings of the International Scientific Conference 2 (May 20, 2020): 214. http://dx.doi.org/10.17770/sie2020vol2.5158.
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This report identifies some of the problems of higher education in the Republic of Bulgaria related to the demographic crisis in the transition process and measures to overcome them. Emphasis is placed on the legislative framework, the rating system, the financing of higher education institutions and the science in them, the quality of training, the demand for staff from business and the supply of staff from universities, the admission of students and the offered forms of training. The analysis made by the authors is based on summarized data, which has been officially published, on the actual state of higher education in Bulgaria. Measures are proposed to overcome the problems, some of which are based on experience at the Technical University of Gabrovo.
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Polyvyannyy, Dmitriy. "The Athos Bulgarian history writing of the 18th century between the Middle Ages and Early Modern Period." Vestnik of Kostroma State University, no. 4 (2019): 14–19. http://dx.doi.org/10.34216/1998-0817-2019-25-4-14-19.
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The article is dedicated to three Bulgarian historical works created at Athos in the second half of the 18th c. – "Slavo-Bulgarian History" by Saint Paisius of Hilendar, anonymous "Zograf History" and "Brief History of the Bulgarian Slav People" by monk-priest Spyridon of Gabrovo. By the author’s opinion, these works, on the one hand, were born in the atmosphere of rivalry between the monasteries of Athos and their Greek, Bulgarian and Serbian clergy, and on the other, were actualised by the strengthening contacts of Hilandar and Zograf with Bulgarian lands. If the first affected the contents of the mentioned works, the second lead to sufficient enlargement of their audience, which, in its turn, became a precondition of the growing interest to the national history among the Bulgarian population of Rumelia in the first half of the 19th c.
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Polimenova, Zinaïda, and Bertrand Tillier. "Exposer le comique à l’époque communiste : la Maison de l’humour et de la satire de Gabrovo (Bulgarie)." Sociétés & Représentations N°47, no. 1 (2019): 137. http://dx.doi.org/10.3917/sr.047.0137.
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Petrova, Desislava. "INTELLIGENT, INNOVATIVE AND SUSTAINABLE INDUSTRY IN BULGARIA – PROSPECTS AND CHALLENGES." ENVIRONMENT. TECHNOLOGIES. RESOURCES. Proceedings of the International Scientific and Practical Conference 1 (June 20, 2019): 210. http://dx.doi.org/10.17770/etr2019vol1.4188.
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The report analyzes industrial transfor-mation through smart and sustainable growth, as well as building a culture of innovation in a new digital age. Innovative enterprises from Bulgaria are presented with their respective modern organizational structures and forms of innovative cooperation between them - Sofia Techpark, Trakia Economic Zone, Technological Park at the Technical University of Gabrovo. The barriers to innovation development of SMEs in Bulgaria are outlined. An example of a high technology center funded under the EU Operational Programs is presented. Answers to questions such as: what are the role of the innovation centers in the innovation ecosystem in Bulgaria; how to stimulate the transfer of talent between university and business; how the market for innovation of the future changes; why de-literacy is a factor of success; how to support innovation and digitization; what are the European policies in the field of innovation and digitization?
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Demireva, Radoynova Dobrinka, Miteva Radostina Dimitrova, Irina Slavcheva Burulyanova, Ganchev Dimitar Ivanov, Dokov Wiliam Viktorov, Ivanov Teodor Ivanov, and Kolev Yanko Geogiev. "Comparative Investigations of the Incidence of Sexual Assault in Three Regions of the Republic of Bulgaria During 1997–2006." Acta Facultatis Medicae Naissensis 30, no. 2 (June 1, 2013): 85–92. http://dx.doi.org/10.2478/v10283-012-0041-3.
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SUMMARY Sexual abuse is considered as a crime against the person all over the world. Despite the age of victims, it could trigger serious physical and psychological consequences, psychoactive substances and drug abuse, reproductive disorders, suicides and even death. The aim of retrospective investigation was to analyze the incidence of sexual assault in the regions of Varna (V), Silistra (S) and Gabrovo (G) in the period 1998-2006. The material used in the study involved the archive records of the Forensic Medicine Wards in the three studied regions. The comparative study employed inquiries and the documental interpretation method. The data of the investigations are filled in questionnaires in Microsoft Excel and compared. In conclusion, we could state that: 1. The female age group, most affected by sexual assault, was that of 14-17 years. 2. Most commonly, the sexual crimes are performed by persons familiar to the victims (50.10%). 3. Among men, the most affected age group was that under 14 years of age.
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DAMASCENO, Fábio Bezerra, Carlos Dinges MARQUES DE SÁ, Bruno Luiz Leite MARTINS, Danilo dos Santos BARRETO, and Luan Kellvin Canuto da MOTA. "SULFETOS DO COMPLEXO GABRÓICO CANINDÉ, SISTEMA OROGÊNICO SERGIPANO." Geosciences = Geociências 39, no. 03 (September 29, 2020): 675–83. http://dx.doi.org/10.5016/geociencias.v39i03.14528.
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O Domínio Canindé, localizado na porção norte do Sistema Orogênico Sergipano, é composto por rochas metavulcânicas e metassedimentares do Complexo Canindé, sendo estas intrudidas pelo corpo gabroico denominado Complexo Gabroico Canindé. A ocorrência de mineralizações sulfetadas de Cu-Ni nos gabros já foi documentada anteriormente e será detalhada neste trabalho no que se refere à sua mineralogia e mineraloquímica, através de utilização microscopia óptica de transmissão e reflexão, de microssonda eletrônica e microscopia eletrônica de varredura. Análises por estes métodos microanalíticos permitiram identificar, em amostras coletadas nos afloramentos do Complexo Gabroico Canindé, a presença de pirita, calcopirita, pirrotita, pentlandita, esfalerita, violarita e spionkopita, com análises para os teores em elementos maiores e menores neles presentes. Entre os sulfetos identificados, a violarita (FeNi2S4) e a spionkopita (Cu39S28) ainda não haviam sido descritas anteriormente no Domínio Canindé. Evidências de alteração hidrotermal tardia nos gabros apontam para gênese dos minerais secundários violarita e spionkopita por alteração dos sulfetos primários de Ni e Cu respectivamente.
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Belivanova, Veneta, and Ivo Sapunov. "The pre-Callovian stratigraphic gap in the Central Balkanids: a key for the interpretation of other Early-Middle Jurassic gaps in Bulgaria." Geologica Balcanica 33, no. 1-2 (June 30, 2003): 17–33. http://dx.doi.org/10.52321/geolbalc.33.1-2.17.
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The pre-Callovian stratigraphic gap in the Central Balkanids is distributed in the Etropole, Teteven, Troyan, Kazanluk, Gabrovo and Turgovishte Districts. To the west (village of Gintsi, Sofia District) and to the east (the section of well R-3 Yunak, District of Yarn a) of the gap uninterrupted Bathonian-Callovian rock successions exist. In its western and eastern parts the pre-Callovian stratigraphic gap is a diastem. In these localities the gap embraces minimum duration. In the western diastem the duration of the gap is from the Late Bathonian to the Early Callovian. In the eastern diastem the duration of the gap is probably in the framework of the Late Bathonian. In many localities where the gap is diastem the boundary between the basement and the cover is marked by hardgrounds. In its central part (Troyan, Kazanluk and Gabrovo Districts) the pre-Callovian stratigraphic gap is with much longer duration. This is caused by the intensive submarine washout of the earlier deposited Middle and Lower Jurassic sediments. In limited localities the Callovian from the cover lies directly even above Upper Triassic rocks. Almost everywhere the cover of the gap is represented by condensed Middle-Upper Callovian micritic limestones. They are rich of ammonites. The main microfacies type is mudstone/wackestone with filaments from thin-shelled bivalves. It is correlated with the Standard Microfacies Type 3 (SMF 3) - "pelagic mudstone and wackestone". It is formed in the lower part of the deep sublittoral, which is in consent with the ba thymetric interpretations based on the characteristics of the respective faunal spectra. The Callovian limestones in conditions of uninterrupted sedimentation show similar microfacies characteristics. In the localities where the pre-Callovian gap is a diastem, the conclusions for the microfacies characteristics and for the faunal spectra of the Bathonian sandy bioclastic limestones are similar. The microfacies type is bioclastic-lithoclastic packstonelrudstone, which can be attributed to some extent to the SMF 4 - "bioclastic-lithoclastic packstone". It may be supposed that the features of this texture direct to a more shallow parts of the deep sublittoral. Almost the same characteristics have the Bathonian limestones and marls in conditions of uninterrupted sedimentation. In general, the pre-Callovian gap is realized in submarine conditions, which are connected with the deep sublittoral. There are four stages in the transition between normal sedimentation and submarine gap: normal sedimentation (in which biostratigraphic superposition is traceable) → slow sedimentation (condensations) → submarine stratigraphic gaps (as a result of non-deposition - diastems) → submarine stratigraphic gaps (as a result of submarine washout).
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Ciesiółka, Przemysław, and Angel Burov. "Paths of the urban regeneration process in Central and Eastern Europe after EU enlargement - Poland and Bulgaria as comparative case studies." Spatium, no. 46 (2021): 1–10. http://dx.doi.org/10.2298/spat2146001c.
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The enlargement of the EU towards Central-Eastern Europe in the years 2004 and 2007 and the related EU funds provided new opportunities and created new challenges to both big metropolitan cities and smaller settlements. One of the particularly important challenges was to define appropriate national and local policies for the urban regeneration of neglected areas, which were abundant in this part of Europe. The objective of the paper is to analyze and evaluate actions taken in Bulgaria and Poland at the national and local level in the field of urban regeneration after the countries? accession to the EU. The paper compares the general national and local planning approaches and capacity building for urban regeneration in the context of regulative and procedural issues. The local case studies represent two types of urban areas under regeneration: the metropolitan core cities Pozna? and Sofia and medium-sized non-core towns of Pi?a and Gabrovo. The results are in the form of a concurrent evaluation of both the achievements and negative effects resulting from the national and local processes in the envisaged and the recently implemented activities with regard to the regeneration of deprived urban neighborhoods and areas.
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Petkova, Kamelia. "The Energy of Local Festivals for the Preservation of Cultural and Historical Heritage: an Empirial View." Cultural and Historical Heritage: Preservation, Presentation, Digitalization 8, no. 1 (June 30, 2022): 80–90. http://dx.doi.org/10.55630/kinj.2022.080107.
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The report analyzes the results of in-depth interviews and focus group discussions held in the fall of 2021 in Sadovo, Elin Pelin, Gabrovo, Bolyartsi, Novi Han, Elin Pelin and Pozharevo within the project "Local Holidays: a resource for local communities to deal with crises", funded by the NSF of the Ministry of Education and Science (KP-06-H45 / 5 of 30.11.2020). The research focuses on local festivals and in particular the way in which their organizers view them as a mechanism for preserving the traditions of the local community. Particular attention is paid to the importance of these events for the presentation and preservation of cultural and historical heritage. The various points of view of representatives of local authorities, organizers of local holidays and representatives of the Roma ethnic community are presented without claiming to be exhaustive. Local holidays in the Bulgarian context, regardless of their thematic focus, have their own energy, which distinguishes them from other similar events and in this sense are the antithesis of fear and social isolation, especially in crises such as the Covid pandemic 19. In most cases, these events can be seen as part of the process of building local identities, which draw their resources from what is imagined, reconstructed and argued as local heritage.
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Petkova, Kamelia. "Local Festivals - the Visible and Invisible Benefits for Local Communities: an Empirical View." Postmodernism Problems 12, no. 1 (April 3, 2022): 82–103. http://dx.doi.org/10.46324/pmp2201082.
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The article presents the results of in-depth interviews and focus group discussions held in Sadovo, Elin Pelin, Gabrovo, Bolyartsi, Novi Han and Pozharevo within a project “Local festivals: A resource of local communities for coping with crises”, funded by National Science Fund – Ministry of Education and Science of Republic of Bulgaria (KP-06-H45/5 from 30.11.2020). The aim of the text is, based on the main essential features and characteristics of local festivals, to prove and derive empirically the importance of “visible” and “invisible” benefits of these events for the preservation of local communities. The various points of view of representatives of local authorities, organizers of local festivals, and representatives of the Roma ethnic community will be presented without claiming to be exhaustive. Numerous studies are available in the literature, focusing on the benefits of holding these events and the various effects they produce on the cultural, social and economic life of local communities. Local festivals in the Bulgarian context, regardless of their thematic focus, in most cases combine the festivities of traditional society, combined with new forms of collective gatherings. In most cases, these events can also be seen as part of the process of building local identities, which draw their resources from what is imagined, reconstructed and argued as local heritage.
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Σωτηρόπουλος, Λ., E. Λυμπέρης, Α. Σιγάλας, Α. Ντουρούπη, Κ. Προβιά, and Γ. Ντουνιάς. "LANDSLIDE AT TSAKONA AREA IN ARKADIA PREFECTURE. GEOLOGICAL CONDITIONS AND ACTIVATION MECHANISM." Bulletin of the Geological Society of Greece 36, no. 4 (January 1, 2004): 1862. http://dx.doi.org/10.12681/bgsg.16661.
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The geological conditions of the landslide's area, at Tsakona, in Arkadia Prefecture, are examined, as well as the factors that influenced the landslide's evolution. The landslide occurred at a distance of 15 km south of Megalopoli, on the New Highway, connecting Tripoli to Kalamata and constitutes one of the larger road landslides that have ever taken place. It occupies an area of a length of 1200m and a width of 300m. Geotectonically the landslide's region is placed in a block of the Pindos zone, thrusted on the Gabrovo-Tripoli zone. The geological formations that comprise the closer geological frame, consist of the formation of "First Flysch", Upper Jurassic - Lower Cretaceous and of the Upper Cretaceous limestones. The geological factors that drastically influenced the landslide's activation are lithological, tectonic, hydrogeological and morphological. The mainly siltstone lithology of the flysch, the intense tectonic deformation that occurred during the alpidic horogenetic phase, the morphological depression that is formed by the landslide's region and the large quantities of groundwater supplied by the uphill limestone, are the main geological reasons that activated the landslide. It should be emphasised that the activation and evolution of the landslide were greatly influenced by human activity during the road construction.
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Ivanov, Marin, Bernard Peybernès, Todor Nikolov, Richard Ciszak, Krystalina Stoykova, and Vera Minkovska. "Essai de corrélations séquentielles au Barrémien-Aptien dans un système plateforme-bassin-plateforme le long d'un transect Danube-Gabrovo (Bulgarie du Centre-Nord)." Comptes Rendus de l'Académie des Sciences - Series IIA - Earth and Planetary Science 325, no. 12 (December 1997): 967–72. http://dx.doi.org/10.1016/s1251-8050(97)82377-4.
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Malchev, Svetoslav, and Katya Vasileva. "Bulgarian Local Cherry Genetic Resources towards Sustainable Agriculture." Sustainability 15, no. 1 (December 22, 2022): 174. http://dx.doi.org/10.3390/su15010174.
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In the conditions of global climate change and invasion of new diseases and pests, the utilisation of the local gene pool is a vital step towards sustainable agriculture. Local cultivars and forms are generally considered as better adapted to the conditions of the originating region than widely spread commercial cultivars bred elsewhere. In order to collect, study, and preserve old and local fruit and vine cultivars and forms, a series of expeditions have been conducted throughout Bulgaria under the frame of project KP-06-N46/3 funded by the National Science Fund of the Bulgarian Ministry of Education and Science. During these scientific expeditions, several local cherry forms were discovered without visual symptoms of brown rot Monilinia laxa (Aderh. and Ruhl.) Honey or cherry leaf spot Blumeriella jaapii (Rehm) Arx. To confirm the degree of resistance/low susceptibility of the specimens, laboratory tests with artificial inoculations of fruits and leaves were conducted. In the current study, two specimens found in Damyanovo region (a village in the municipality of Sevlievo, Gabrovo Province, in northern central Bulgaria) were included. They were compared to two old local cherry cultivars, ‘Volsko sartse’ and ‘Ranna cherna edra’, and two new selections of FGI-Plovdiv, ‘Asparukh’ (El.17-90) and ‘Kossara’, using ‘Bigarreau Burlat’ as reference cultivar for resistance to economically important diseases. The artificial inoculations confirmed the field observation of the cherry specimen with designation SM-58 with 0.00% of infected fruits. Therefore, it is recommended for use in the breeding programme of the Fruit Growing Institute, Plovdiv for the creation of new cultivars.
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MOREIRA, César Augusto, Alice Marques PEREIRA, and Mara Lia Dias CAVALHEIRO. "Caracterização geoelétrica do gabro Santa Catarina, São Sepé (RS)." Pesquisas em Geociências 41, no. 1 (April 27, 2014): 15. http://dx.doi.org/10.22456/1807-9806.78029.
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Os métodos geofísicos são largamente empregados na pesquisa dos mais diversos tipos de depó- sitos minerais. Quando combinados com estudos diretos como geoquímica em amostras de solos ou rochas, possibilitam um aumento substancial na probabilidade de descoberta de jazimentos. Os métodos geofísicos elétricos são particularmente promissores em estudos voltados à busca de sulfetos devido ao contraste das propriedades físicas resistividade elétrica e cargabilidade. Este trabalho apresenta os resultados da aplica- ção dos métodos eletrorresistividade e polarização induzida, por meio da técnica de caminhamento elétrico, com o objetivo de avaliar o potencial mineral do gabro Santa Catarina, localizado no município de São Sepé (RS), numa região onde foram descritas várias ocorrências de ouro e sulfetos. Este gabro é classificado no domínio de Corpos Básico-Ultrabásicos Estratiformes, que reúne peridotitos, gabros e anortositos acamadados. Foram realizadas três linhas de caminhamento elétrico dispostas de forma radial, com cruzamento no centro da área e separação de 60° entre linhas e leituras de resistividade elétrica e cargabilidade em arranjo Wenner- -Schlumberger. A associação de áreas de baixa resistividade e alta cargabilidade obtida a partir de modelos de inversão bidimensionais permitiu definir zonas potencialmente mineralizadas, relacionadas com estruturas que condicionam a rede de drenagem no domínio do gabro. Pintas de ouro detectadas em campanha de prospecção geoquímica em sedimento de corrente à jusante do gabro podem ser originadas da lixiviação de depósitos contidos em fraturas, por ação de águas fluviais no domínio do gabro, possivelmente caracterizados por sulfetos e ouro associado.
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Timich, Marco, Rogério Guitarrari Azzone, Gaston Eduardo Enrich Rojas, Saulo Vieira da Silva Filho, Excelso Ruberti, and Celso De Barros Gomes. "Relações de contato entre rochas alcalinas máficas e sieníticas na Praia do Jabaquara, setor norte da Ilha de São Sebastião, SP." Geologia USP. Série Científica 19, no. 4 (December 20, 2019): 3–22. http://dx.doi.org/10.11606/issn.2316-9095.v19-157121.
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Relações de contato entre as rochas sieníticas do stock de Serraria e as rochas máficas plutônicas e hipoabissais do setor norte da suíte alcalina da Ilha de São Sebastião (Ilhabela) são descritas pela primeira vez, permitindo a indicação de relações temporais entre diferentes pulsos magmáticos. Os afloramentos apresentam variedade sienítica hololeucocrática hospedando mega-, macro- e microxenólitos de diferentes rochas, formando agmatitos. Cinco unidades principais são descritas: álcali feldspato sienitos, melassienitos, diabásios, cumulatos máficos (melagabros/clinopiroxenitos) e gabros heterogêneos. Geoquimicamente,o magmatismo alcalino bimodal encontrado na ilha é bem representado pelas rochas dos afloramentos estudados. A sequência de eventos magmáticos consiste em: colocação e cristalização de pulsos de magmas básicos alcalinos, em ambiente de câmara magmática, gerando as variedades gabroicas cumuláticas, principalmente melagabros e clinopiroxenitos com olivina, e brechas de matriz gábrica com evidências de reequilíbrio textural por ação de temperatura; intrusão de novos pulsos de magma básico alcalino, representados pelos fragmentos de diabásios, que apresentam também, reequilíbrio textural (textura granoblástica predominante); intrusão de pulso sienítico na câmara máfica que fragmentou o gabro já parcial ou totalmente cristalizado, transportando ampla proporção de xenocristais e xenólitos, o que gerou rochas classificadas como melassienitos; nova intrusão de pulso sienítico, que fragmenta todo o sistema formando um agmatito com megaxenólitos e microxenólitos de gabro cumuláticos, diabásios, agmatitos de matriz gabroica (gabros heterogêneos) e melassienitos; veios e diques de pegmatito e aplito de sienitos com quartzo cortam todos os litotipos. Todos os tipos amostrados como xenólitos apresentam algum grau de recristalização e de reação química com o magma sienítico final que os hospeda.
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Godoy, Antonio Misson, Otávio Augusto Ruiz Paccola Vieira, Larissa Marques Barbosa de Araújo, George Luiz Luvizotto, and Jefferson Cassu Manzano. "Ocorrência de Fe-Ti-V associado ao Magmatismo Gabro-Anortosítico da Serra da Alegria, Maciço Rio Apa, Mato Grosso do Sul." Geologia USP. Série Científica 20, no. 2 (April 16, 2020): 19–38. http://dx.doi.org/10.11606/issn.2316-9095.v20-148783.
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O Maciço Rio Apa constitui exposições de rochas paleoproterozoicas na porção extremo sul do Cráton Amazônico. A região é constituída por rochas do Complexo Rio Apa, Grupo Alto Tererê e pelo Grupo Amonguijá, formado pelas suítes Vulcânica Serra da Bocaina e Plutônica do Batólito Alumiador. O segmento norte do batólito é caracterizado por rochas ácidas-básicas da Serra da Alegria, ocorrendo, na parte central, rochas da Sequência Magmática Ácida-Intermediária, representadas pelo granito homônimo. No seu entorno, no sopé das escarpas, aflora a Sequência Magmática Gabro-Anortosítica da Serra da Alegria, composta por magnetita gabro, quartzo gabro a leuco gabro, pegmatito básico e anortosito. Essas rochas gabroides constituem uma ocorrência magmática, cumulática básica, estratiforme, semiconcordante, formada por processos de cristalização fracionada, por flotação dos plagioclásios em anortosito, nas porções superiores da câmara magmática e, na parte inferior, por segregação gravítica, a concentração de cumulus de óxido de ferro constitui magnetita gabro e magnetitito. Os minerais magmáticos identificados correspondem a andesina-labradorita, apresentando teor de anortita entre An36,76– An58,06 e clinopiroxênio cálcico do tipo ferro-augita e augita. Os óxidos de ferro predominantes são ferromagnetita, com valores de FeOt entre 88,03 e 92,98%, e titanomagnetita, com valores de TiO2 entre 1,13 e 6,39%. As fases subordinadas são representadas por vanádio magnetita, com valores de V2O5 entre 0,75 e 0,98%, e ilmenita. O magmatismo básico-anortosítico sin a pós-orogênico foi resultado da cristalização de um magma mantélico primário que, associado a processos de diferenciação, gerou variedades de gabros e diabásios de composições Fe-toleíticas e diferenciados anortosíticos, em ambientes de arco de ilha a intraplaca.
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YILDIRIM, Demet Kıran, and Amr ABDELNASSER. "Geochemical Characteristics of the Pan-African Basement Rocks at Atud Area, Central Eastern Desert, Egypt." Afyon Kocatepe University Journal of Sciences and Engineering 22, no. 4 (August 31, 2022): 944–62. http://dx.doi.org/10.35414/akufemubid.1111229.
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Bu çalışmada, Atud bölgesi’ndeki (Mısır'ın Orta Doğu Çölü) Prekambriyen Pan-Afrikan temel kayaçlarının jeolojik yerleşimlerini, jeokimyasal özelliklerini, saha ilişkilerini, tektonik yerleşimlerini ve petrojenezlerini belirlemek için petrografik ve jeokimyasal özellikleri ortaya konulmuştur. Atud Bölgesi’nde serpantinitler, bunların türevleri ve metatüfler, metagabro-diyorit kompleksi tarafından kesilmektedir. Metagabro-diyorit kompleksi ise olivin gabronoritik kayaçlar tarafından kesilmektedir. Serpantinitler, talk-karbonat ve kalk-silikat kayaçları metamorfik peridotitler olarak adlandırılmıştır. Nadir toprak elementleri (NTE) davranışları, HNTE ve pozitif Eu-anomalisi ile ANTE zenginleşmeleri ile karakterize edilir. Bu durum, hidrotermal akışkanların plajiyoklaz çözünmesi ve/veya sirkülasyonu ile doğada meydana gelen okyanus serpantinleşmesine işaret etmektedir. Metatüfler çoğunlukla en yüksek K/Rb oranına sahip olan bazik ile ortaç dereceli magma odalarından türetilmiştir. NTE paternleri, HNTE açısından zenginleşmiş, ANTE'den yoksun ve negatif Eu anomalilerine sahip genelde toleyitik ve kalk-alkalin kayaçlarla okyanus ada yayının metasedimentlerine benzemektedir. Ayrıca, dalma-batma zonu boyunca manto kaynağına eklenen bileşenler tarafından kirlenmiş bir magmadan kaynak kayaçlarının oluştuğunu ifade etmektedir, yani negatif Eu-, Sr- ve Zr- anomalileri göstermektedir. Metagabro-diyorit kompleksi kayaçlarının sırasıyla kalk-alkalin gabro ve gabro/diyorit ve diyorit ve gabro/diyorit olduğunu ortaya koymaktadır. Bu kayaçlar, sırasıyla metagabrolar ve diyoritler için klinopiroksen ve amfibol fraksiyonasyonuna işaret eden ada yayı ortamlarında meydana gelen kalk-alkali bazalt (CAB) ile karşılaştırılabilir. Öte yandan, olivin gabronorit kayaçları, K toleyitik magmatik afinitelere sahip gabroik kayaçlar olarak sınıflandırılır. NTE paternleri, HNTE ile zenginleşmeyi ve pozitif Eu-, Th-, Pb-, Sr- ve Zr-anomalileri ve plajiyoklaz ve olivin düşük basınçlı fraksiyonasyonunu ima eden negatif P- ve Ti-anomalileri ile ANTE açısından tüketilmeyi ortaya koymaktadır.
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Kostova, Dobrinka. "Trust and solidarity in Bulgarian cooperatives." Sociologija 48, no. 2 (2006): 149–62. http://dx.doi.org/10.2298/soc0602149k.
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The paper analyzes the strategies of people in agriculture, especially in the mountain regions where the fragmentation of land is significant. The quantity of land there is also limited. This leads to important consequences for the agrarian development. The culture of keeping the lands of the predecessors burdens the market of agricultural lands. The renting of lands depends on the types of plants to be cultivated as the law for renting lands allows contracts for the max of five years and for the farmers it is insecure to cultivate perennial plants on such lands. In this situation the survival of the small-scale farmers depends on their ability to coop and support each other. The article describes the emergence of a coop for bioproduction of roses, mint and milk in the "Valley of Roses", Karlovo and Gabrovo regions, the solidarity between the farmers, the stimuli and barriers to their activities. It reveals the culture of mutual support based not so much on economic but rather on other incentives such as love to nature and environment, strong desire to prove that bioproduction could develop in the country and that bioproducts are the future for Bulgarian agriculture. It is a different coop in comparison with the socialist collectives. The now established coop unites the farmers for education, qualification, market and mutual support for objectives, but each farmer produces his/her products alone. The farmers sell the products together and each one depends on the culture of others' conscious cultivation of bioproducts. Until now, the experience has been positive and the coop has sustainable development. This is also due to the creation of three professional organizations - the coop as a producing unit, organization for distributing knowledge on organic production and a certifying organization of bioproducts. The survival of the coop depends on farmers? hard work and solidarity, the strong will to survive, the hope for future significant agricultural support and subsidies when the European Union enlargement involves Bulgaria and the improvement of the economic situation in the country that could bring better buying abilities of the population.
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DEMİR, Selçuk. "DERBEND SİSTEMİNİN NÜFUS VE YERLEŞME ÜZERİNE ETKİSİ: GABROVA KARYESİ ÖRNEĞİ." Social Sciences Studies Journal 4, no. 20 (January 1, 2018): 2732–38. http://dx.doi.org/10.26449/sssj.691.
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Santos, Roseli Dias dos, Marco Antonio Galarza, and Davis Carvalho de Oliveira. "Geologia, geoquímica e geocronologia do Diopsídio-Norito Pium, Província Carajás." Boletim do Museu Paraense Emílio Goeldi - Ciências Naturais 8, no. 3 (February 25, 2021): 355–82. http://dx.doi.org/10.46357/bcnaturais.v8i3.554.
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O Diopsídio-Norito Pium ocorre a sul da Bacia Carajás e é constituído por noritos (± gabronoritos), quartzo-gabros com variações para enderbitos e, de maneira restrita, rochas cumuláticas. Relações de contemporaneidade (magma mingling) são observadas, uma vez que a variedade de composição norítica ocorre ora como enclaves angulosos e de contatos retilíneos no interior das rochas quartzo-gabroicas, evidenciando alto contraste de viscosidade, ora como um enxame de enclaves arredondados (blebs/autólitos) no interior da variedade hornblenda-gabro. Os dados geoquímicos demonstram que estas rochas possuem enriquecimento em FeOt em relação ao MgO, apontando a natureza subalcalina toleítica das mesmas, e uma origem a partir da fusão parcial do manto peridotítico. Diagramas de ambiência tectônica evidenciam que estas rochas possuem afinidades geoquímicas com basaltos intraplacas e apontam para um processo de evolução magmática a partir dos noritos até os enderbitos. Idades Pb-Pb obtidas para estas rochas, entre 2745 ± 1 Ma e 2744 ± 1 Ma, são consideradas suas idades de cristalização. As análises Sm-Nd forneceram idades-modelo TDM entre 3,14 e 3,06 Ga, e valores de εNd (T = 2,74 Ga) entre -2,78 e -1,58, indicando um significativo envolvimento de fontes crustais em sua gênese. As idades-modelo confirmam um importante período de formação de crosta no Mesoarqueano na Província Carajás.
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Kavčič, Jerneja, Kajetan Gantar, Primož Simoniti, Brane Senegačnik, and Janez Orešnik. "In memoriam: prof. dr. Erika Mihevc Gabrovec." Keria: Studia Latina et Graeca 19, no. 1 (December 30, 2017): 7. http://dx.doi.org/10.4312/keria.19.1.7-18.
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Babič, Matjaž. "Ob življenjskem jubileju dr. Erike Mihevc Gabrovec." Keria: Studia Latina et Graeca 4, no. 2 (December 6, 2002): 9. http://dx.doi.org/10.4312/keria.4.2.9-11.
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Dr. Erika Mihevc-Gabrovec, zaslužna profesorica na Oddelku za klasično filologijo Filozofske fakultete Univerze v Ljubljani, praznuje petinsedemdesetletnico. Bogata pedagoška in znanstvena dejavnost slavljenke bi zahtevala več strani, kakor so nam odmerjene na tem mestu, zato se bo pričujoči prispevek ustavil samo na nekaterih križiščih njene dolgoletne poti.
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Akaeva, Tatiana, Karen Mkhitaryan, Ole Vasilkovskaya, and Mikhail Gotovskiy. "New homeopathic preparations in practice." International Journal of High Dilution Research - ISSN 1982-6206 18, no. 02 (June 30, 2021): 14–15. http://dx.doi.org/10.51910/ijhdr.v18i02.994.
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Background One of the most important tasks in anti-age therapy and rejuvenation practice is the regeneration of various tissues, organs and body systems [1,2]. In this study, we evaluated the effectiveness of therapy with the new class of homeopathic and informational preparations “Triton Regeneration” and “Triton Metamorphosis” [3]. The preparations were used both in homeopathic dilutions, and in the form of control signals of the Triton (CSTrit). Aims To apply in practice the homeopathic preparations “Triton regeneration” and “Triton metamorphosis” in the form of homeopathic dilutions and control signals, in order to regenerate the organs of the tissues and systems of the patient and evaluate the results obtained. Methodology A clinical study was conducted on a group of 33-st people aged between 7-75 years of both sexes who received injuries to the skin, connective tissue and / or musculoskeletal system. The study was conducted by a multicenter method in the cities: Moscow (Russia), Gabrovo (Bulgaria), Arad (Romania). All patients gave informed consent for treatment. To write a CS and their applications, for diagnostics and therapy, and the fabrication for the necessary preparations and marker CMH, the integrated system for electropuncture diagnostic « IMEDIS-EXPERT» was used. For the diagnosis method was used vegetative resonance test (VRT). Cultures of the biological material of the triton were used to obtain control signals triton (CSTrit) therapy. The method of bioresonance therapy (BRT) was used to adapt and administer the condition of the patient. Adaptation of the preparations to the patient's body was carried out by electron potentiation of the initial CSTrit until the VRT condition was met:
?MH ? + Pot ? (CSTrit) ?
The marker ?MH-individual constitutional marker represents the sum of signals from the nodal and terminal BAT (biologically active points) located on the main chirohlyphic palm lines of the patient. Patients used the homeopathic remedies of triton and / or adapted CSTrit in individual dosage during the individual course of therapy. At subsequent receptions, a second VRT was re-examined and the degree of recovery of defects in the skin, connective tissue and / or the musculoskeletal system was assessed. Results This clinical study showed a high efficacy of homeopathic and informational preparations of CSTrit in patients who received injuries of the skin, connective tissue and / or musculoskeletal system. A pronounced positive effect was obtained in all cases of treatment of CSTrit: objective processes of regeneration of the connective tissue system of the patients were noted, in particular, restoration of its skin. In the case of treatment therapy for injuries of the musculoskeletal system, marked regeneration processes in the bone and tendon tissues were observed, confirmed by R-studies. Conclusion 1. Homeopathic remedies “Triton regeneration” and “Triton metamorphosis”, as well as the control signals of the Triton (CSTrit), made using the apparatus "IMEDIS-EXPERT", are effective signals of the regeneration of body tissues, as in the case of treatment of skin and connective tissue damage, and in case of damage to bone tissue and tendons. 2. Therapy of patients with CSTrit, potentiated by the ?MH marker, is comparable in effectiveness and end results with mono- and complex homeopathic therapy and in some cases surpasses it. 3. A new class of the preparations - gives a positive result in 96% of cases. Similar results are unattainable with ordinary homeopathy.
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Chương, Văn Đức, Trần Văn Thắng, Văn Đức Tùng, Phan Doãn Linh, and Lê Triều Việt. "Ophiolit zone of Thai Nguyen - Cao Bang." VIETNAM JOURNAL OF EARTH SCIENCES 25, no. 2 (March 19, 2018): 142–49. http://dx.doi.org/10.15625/0866-7187/25/2/11895.
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Ophiolit zone of Thai Nguyen - Cao Bang started from the border of Vietnam with China, then stretched in passing Cao Bang - Dong Khe - SacCan - to Thai Nguyen. The structure of the ophiolit zone devided into five complex :- Dunite - serpentinit - peridotite complex,- Folliation gabros complex,- Gabros - diabaz complex, ·- Bazan toleit complex,- Sediment of marginal complex.The formation of Ophiolit zone occurred in the beginingPermi and ending in the late of Triassis by overslip of Eurasian plate over Song Hien marginal sea.
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Álvarez Agudelo, Jairo. "Serpentinitas y epidota anfibolitas de Ituango, departamento de Antioquia, Colombia." Boletín Geológico 28, no. 3 (October 1, 1987): 91–120. http://dx.doi.org/10.32685/0120-1425/bolgeol28.3.1987.329.
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Las serpentinitas y epidote – anfibolitas del área de Ituango, forman un cuerpo discontinuo, muy largo y delgado, con rumbo norte-sur y 35 km de longitud, que hace parte de la faja máfica-ultramáfica, tipo alpino, relacionada con la zona tectónica de Romeral. Dicho cuerpo está encajado dentro de una secuencia eugeosinclinal plegada (Grupo Valdivia), con metamorfismo de bajo grado y edad posiblemente Paleozoica y los litotipos que lo conforman tienen contactos tectónicos entre si y con la metamorfitas encajantes. La sepentinita, cizallada e internamente fracturada, está constituida por antigorita y/o lizardita y crisotilo. Tiene una razón MgO/MgO + FeO* entre 0,82 y 0,85 y MgO/SiO2 entre 0,92 y 1,07 lo cual sugiere que la serpentinización fue un proceso isoquímico, acompañado solamente por la adición de agua y que el protolito fue principalmente una harzburgita. Las características químicas y mineralógicas relictas insinúm, que esta roca fue residuo de fusión parcial en el manto. Se distinguieron epidota-anfibolitas néisicas y esquistosas que difieren en mineralogía, grado de recristalización y cizalladura; son gradacionales entre sí, predominando el segundo tipo hacia la base del "thrust" ofiolítico. La composición química de estas rocas sigue la tendencia toleítica, es similar a la de los gabros intermedios dragados de la dorsal Atlántica y se sitúa en el campo de las ofiolitas de alto Ti. El protolito fue, quizás, un gabro homogéneo ligeramente rico en magnesio, generado en una dorsal de una Cuenca marginal. El cuerpo de Ituanago fue emplazado en forma sólida, en el cretáceo tradío – terciario temprano, como un fragmento ofiolítico desmembrado, a lo largo de fallas inversas profundas inclinadas hacia el este. Durante el emplazamiento, las rocas fueron recristalizadas y deformadas penetrativamente. El emplazamiento al nivel presente es postmioceno temprano y continúa en la actualidad a causa del movimiento activo de las fallas que limitan dichas rocas.
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Álvarez Agudelo, Jairo. "Geología del Complejo Ofiliolítico de Pácora y secuencias relacionadas de Arco de Islas (Complejo quebrada Grande), Colombia." Boletín Geológico 35, no. 1 (January 1, 1995): 5–49. http://dx.doi.org/10.32685/0120-1425/bolgeol35.1.1995.87.
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El Complejo Ofiolítico de Pácora, situado en el sector central del flanco occidental de la cordillera Central, está constituido en la zona volcánica por lavas almohadilladas variolíticas no vesiculares, brechas en almohadilla y brechas. La zona plutónica contiene una secuencia compleja de gabros isotrópicos y cúmulus, wehrlitascúmulus y serpentinitas. Los protolitos de estas últimas rocas parecen ser harzbwgitas o lherzolitas con plagioclasa cuyas características sugieren un origen en la zona de transición cerca al moho petrológico, en la zona superior de la harzburgita tectónica. Delgados diques de plagiogranito intruyen al gabro. Las diversas unidades ofioliticas fueron fraccionadas tectónicamente, deformadas y inetamorfizadas y sufrieron mezcla estructural con secuencias de arco volcánico (Complejo Quebradagrande). La evidencia mineralógica-geoquímica sugiere que la ofiolita es remanente de corteza oceánica-manto generada en un centro de expansión oceánico. Además, las características geoquímicas de las vulcanitas y las particularidades petrográficas y faunísticas de las sedimentitas epiclásticas y volcanoclásticas del Complejo Quebrada grande insinúan un origen en un arco volcánico oceánico inmaduro separado del continente siálico por una cuenca semioceánica estrecha. Los miembros de la ofiolita experimentaron metamorfismo hidrotermal de fondo oceánico en facies esquisto verde y quizá anfibolita (?) antes del solevantamiento y emplazamiento y durante estos sufrieron metamorfismo en facies prehnita- pumpellyita junto con las secuencias del arco volcánico. El arco volcánico, construido sobre corteza oceánica, fue suturado a la margen continental y obductado en tipos post-albianos. Este fenómeno causó el soldamiento definitivo de la ofiolita y la mezcla tectónica con las rocas del arco. Sin embargo, el emplazamiento de algunos sectores plutónicos de la ofiolita a niveles de exposición es pre-Albiano. Pequeños cuerpos andesíticos-dacíticos neógenos fueron intruídos en zonas de falla simultáneamente con la actividad volcánica en la cuenca post-colisiona) Cauca-Patía. Las litounidades han sido deformadas por fallas rumbodeslizantes a partir del Terciario medio por reorientación de los límites de placas.
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Attallah, Omneya. "GabROP: Gabor Wavelets-Based CAD for Retinopathy of Prematurity Diagnosis via Convolutional Neural Networks." Diagnostics 13, no. 2 (January 4, 2023): 171. http://dx.doi.org/10.3390/diagnostics13020171.
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One of the most serious and dangerous ocular problems in premature infants is retinopathy of prematurity (ROP), a proliferative vascular disease. Ophthalmologists can use automatic computer-assisted diagnostic (CAD) tools to help them make a safe, accurate, and low-cost diagnosis of ROP. All previous CAD tools for ROP diagnosis use the original fundus images. Unfortunately, learning the discriminative representation from ROP-related fundus images is difficult. Textural analysis techniques, such as Gabor wavelets (GW), can demonstrate significant texture information that can help artificial intelligence (AI) based models to improve diagnostic accuracy. In this paper, an effective and automated CAD tool, namely GabROP, based on GW and multiple deep learning (DL) models is proposed. Initially, GabROP analyzes fundus images using GW and generates several sets of GW images. Next, these sets of images are used to train three convolutional neural networks (CNNs) models independently. Additionally, the actual fundus pictures are used to build these networks. Using the discrete wavelet transform (DWT), texture features retrieved from every CNN trained with various sets of GW images are combined to create a textural-spectral-temporal demonstration. Afterward, for each CNN, these features are concatenated with spatial deep features obtained from the original fundus images. Finally, the previous concatenated features of all three CNN are incorporated using the discrete cosine transform (DCT) to lessen the size of features caused by the fusion process. The outcomes of GabROP show that it is accurate and efficient for ophthalmologists. Additionally, the effectiveness of GabROP is compared to recently developed ROP diagnostic techniques. Due to GabROP’s superior performance compared to competing tools, ophthalmologists may be able to identify ROP more reliably and precisely, which could result in a reduction in diagnostic effort and examination time.
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Ovares-Gutiérrez, Tobías. "Un viaje a las intimidades del guión y del guionista. Sobre El guión como profecía, de Gabrio Zapelli-Cerri." Temas de Nuestra América. Revista de Estudios Latinoaméricanos 31, no. 58 (April 8, 2016): 187. http://dx.doi.org/10.15359/tdna.31-58.12.
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Hartosuwarno, Sutarto, Joko Soesilo, Bambang Tri Wibowo, Hafiz Hamdalah, Abdul Majid, and Shabrina Aqiilah N. "Karakteristik dan Pembentukan Batuan Beku di Pegunungan Jiwo, Bayat, Jawa Tengah." Jurnal Mineral, Energi, dan Lingkungan 4, no. 2 (January 13, 2021): 18. http://dx.doi.org/10.31315/jmel.v4i2.3235.
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Pegunungan Jiwo, Bayat merupakan salah satu dari tiga wilayah di Jawa yang memperlihatkan adanya singkapan batuan-batuan metamorf yang berumur Pra-Tersier. Di atas batuan-batuan metamorf tersebut diendapkan tidak selaras batuan-batuan sedimen Tersier yang termasuk kedalam Formasi Wungkal-Gamping. Batuan-batuan metamorf maupun sedimen pada beberapa tempat diterobos oleh batuan-batuan beku diantaranya adalah gabro, diabas, basalt, dan diorite. Keberadaan batuan-batuan beku tersebut menjadi menarik karena sedikit terpisah dari jalur magmatic Pegunungan Selatan Jawa Timur. Batuan-batuan beku hasil kegiatan magmatisme tesebut di atas, hadir sebagai batuan beku plutonik (gabro, gabro mikro atau diabas, diorit), dan batuan beku vulkanik (basalt), yang hadir baik sebai intrusi (retas) maupun lava. Sebagian besar batuan beku tersebut di permukaan dalam keadan lapuk, dan hanya sebagian kecil singkapan yang memperlihatkan keadaan yang fres atau segar, diantaranya pada beberapa inti batuan beku yang mengalamai pelapukan mengulit bawang (spheroidal weathering). Kenampakan mikroskopik, gabro dan gabro mikro umumnya memperlihatkan tekstur equigranular, kumulus, ofitik, subofitik, dan diabasik disusun oleh mineral-mineral primer plagioklas (±52-66%), Olivin (±0-14%), piroksen (±4-18%), mineral opak, baik kemungkinan primer maupun sekunder (±2-12%). Sebagian besar gabro mengalami ubahan hidrotermal lemah-sedang, yang dicirikan oleh terubahnya beberapa mineral primer menjadi mineral-mineral klorit, silica, epidot, karbonat, serpentin,dan aktinolit. Basalt secara mikroskopik, memperlihatkan tekstur inequigranular, porfiritik-porfiroafanitik, disusun oleh mineral-mineral primer plagioklas, olivin, piroksen, mineral opak, baik kemungkinan primer maupun sekunder dengan mineral sekunder seperti klorit dan karbonat . Batuan-batuan beku di Pegunungan Jiwo tersebut, diperkirakan merupakan hasil magmatisme yang berumur Eosen Akhir-Miosen Awal (39,82±1,49 Ma sampai 13.852±5.45 juta tahun) dan merupakan bagian dari busur kepulauan Sunda-Banda. Magmatisme tersebut disebabkan oleh adanya subduksi kearah utara lempeng Hindia-Australia di bawah bagian tenggara lempeng Eurasia yang dikenal sebagai Sundaland.
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Zapata-Villada, Juan Pablo, Wilmer Giraldo, Gabriel Rodríguez, Mauro Cesar Geraldes, and Milton Obando. "Geoquímica y geocronología U-Pb de la cuarzodiorita de Sabanalarga y el gabro de Santa Fe, Colombia." Boletín de la Sociedad Geológica Mexicana 73, no. 1 (April 1, 2021): A280520. http://dx.doi.org/10.18268/bsgm2021v73n1a280520.
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Durante el Cretáceo Superior, el margen noroccidental de Suramérica se caracterizó por presentar un ambiente tectónico complejo, representado por la acreción de múltiples terrenos y la generación de varios eventos magmáticos. La cuarzodiorita de Sabanalarga y el Gabro de Santa Fe, anteriormente descritos como una única unidad denominada “Batolito de Sabanalarga”, presentaban múltiples diferencias entre sí y hoy son considerados dos plutones independientes, exponiendo dos de los eventos magmáticos del cretáceo superior. Ambos plutones emplazados en cortezas de diferente afinidad; el Gabro de Santa Fe emplazado en corteza tipo Plateau y arco de islas, mientras que la cuarzodiorita de Sabanalarga es emplazada en corteza continental del Complejo Cajamarca. Los análisis químicos de roca total realizados, presentaron anomalías de Nb-Ti, patrones de HFSE y REE en los diagramas multielementales característicos de rocas generadas en ambientes de subducción. El gabro de Santa Fe presenta características adakiticas no presentes en la cuarzodiorita de Sabanalarga. El bajo contenido Zr y relaciones (La/Yb)n vs Sr/Y < 10 sugieren que el magma del Gabro de Santa Fe fue formado en ambiente oceánico, contrario a la cuarzodiorita de Sabanalarga con alto Zr y relaciones (La/Yb)n vs Sr/Y > 10 que sugieren para este magma un origen en un ambiente continental. Se realizaron análisis U-Pb LA-ICP-Ms para ambos intrusivos: el Gabro de Santa Fe presentó edades entre 78.4 y 81.8 Ma y la cuarzodiorita de Sabanalarga edades entre 71.5 y 76.7 Ma. A la luz de los nuevos datos geoquímicos y geocronológicos se sugiere en este trabajo que el Gabro de Santa Fe y la cuarzodiorita de Sabanalarga son dos cuerpos diferentes sin relación temporal y cuya relación espacial es todavía debatible. Para el ambiente de formación de estos plutones se sugiere un modelo de doble subducción tipo Molucca.
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Ludka, Isabel Pereira, and Cristina Maria Wiedemann. "Geoquímica do gabro coronítico de Amparo, RJ." Anuário do Instituto de Geociências 25 (January 1, 2002): 44–67. http://dx.doi.org/10.11137/2002_0_44-67.
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The aim of this paper is to present geochemical data and some petrological aspects of the Amparo gabbroic (hyperite) body, located approximately 30 km east of the town, Nova Friburgo, Rio de Janeiro State. Ten samples of these basic rocks were analysed for major, minor and trace elements, and three of these for REE. The data obtained reflect the limited mineralogical range. The contents of the major elements indicate a sub-alkalic tholeiitic magma, as shown by modal analysis, which classified these rocks as an olivine gabbro. Geochemical analysis of the minor, trace and rare-earth elements shows abnormal incompatible enrichment, such as the high LREE, Ba and Sr contents. Similar results for other basic and ultrabasic intrusions are common in this portion of the Ribeira Mobile Belt.
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Pereira, Fabio Santos, Maria de Lourdes da Silva Rosa, and Herbet Conceição. "Condições de colocação do magmatismo máfico do Domínio Macururé, Sistema Orogênico Sergipano: Maciço Capela." Geologia USP. Série Científica 19, no. 3 (August 8, 2019): 3–29. http://dx.doi.org/10.11606/issn.2316-9095.v19-151464.
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O Maciço Capela é intrusivo nas rochas metassedimentares do Domínio Macururé, Sistema Orogênico Sergipano, no sul da Província Borborema. Ele é constituído por dioritos, hornblenditos, gabros e granitos, que hospedam enclaves tonalíticos e hornblendíticos. As formas e os contatos dos enclaves tonalíticos, aliados à presença de texturas de zoneamento inverso e oscilatório em cristais de plagioclásio e ao hábito acicular da apatita nos enclaves e dioritos sugerem coexistência de magmas máfico e félsico. Os piroxênios identificados nos gabros apresentam composições de enstatita, augita e diopsídio. Os anfibólios das rochas máficas são cálcicos e correspondem a pargasita, tschermakita e magnésio-hornblenda. A mica marrom dos hornblenditos, gabros e dioritos é rica na molécula de flogopita, enquanto a dos granitos é mais enriquecida em ferro. A granada, de ocorrência restrita aos hornblenditos e dioritos, é rica na molécula de almandina. O plagioclásio varia de albita a bytownita e o feldspato potássico é a microclina. A presença de titanita e epídoto magmáticos, coexistentes com silicatos máficos magnesianos, indica a cristalização sob condições de alta fO2, próximas ao tampão NNO. As estimativas de pressão forneceram um valor médio de 8,5 kbar, que corresponde a uma profundidade aproximada de 30 km. As temperaturas liquidus, obtidas com as composições de piroxênios e anfibólios, variam de 1.261 a 831°C. Temperaturas solidus, estimadas com o par anfibólio-plagioclásio, situam-se entre 775 e 614°C. Dados de química mineral e estimativas termobarométricas sugerem que as rochas do Maciço Capela cristalizaram-se a partir de magmas basálticos hidratados, em ambiente de arco continental.
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Kampamba, Johnson, Simon Kachepa, Milidzani Majingo, and Kathata Pearl Babitseng. "An Assessment of Property Maintenance in high rise buildings in Gabrone (CBD)." American Research Journal of Civil and Structural Engineering 4, no. 1 (September 22, 2020): 1–11. http://dx.doi.org/10.21694/2577-5944.20002.
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Marković, Julijana N. "Wall Paintings in the Altar of the Holy Trinity Church in Gabrovac." Саопштења = Communications 54 (2022): 223–52. http://dx.doi.org/10.18485/rzzsk_saopstenja.2022.54.9.
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Rodríguez-García, Gabriel, and Jose Gilberto Bermúdez-Cordero. "Petrography, geochemistry and age of Cerro Frontino Gabro." Boletín de Ciencias de la Tierra, no. 38 (July 1, 2015): 25–40. http://dx.doi.org/10.15446/rbct.n38.46053.
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The Gabro de Cerro Frontino was emplaced in the Cañasgordas Block, located in the Northern Segment of the Colombian Western Cordillera. It corresponds to a pluton composed of at least three magmatic pulses, emplaced during a short period of time. Gabbros and diorites are more common in the unit than clinopiroxenites, monzodiorites and monzonites. These rocks are composed of calcic to intermediate plagioclase, augite-egerine type clinopyroxene and biotite; olivine and flogopite may be present in some mafic rocks and alkali feldspar and quartz may be present in some felsic rocks. Sphene, magnetite and apatite are common accessory minerals. The silica content in the rocks varies between 37.08% and 54.4%, with constant values of MnO (0.1% 0.4%), impoverishment of Fe2O3, MgO, CaO, TiO2 and P2O5 as SiO2 increases, and enrichment of K2O, Na2O and Al2O3 as SiO2 increases. The basic and ultrabasic rocks fall in the sub-alkaline series, the rest of the samples fall in the medium to K-rich calc-alkaline series and in the shoshonitic series. The Gabro de Cerro Frontinocorresponds to magmas impoverished on heavy rare earth elements with respect to light rare earth elements, which suggests the contribution of a subduction component in the magma genesis. The LILE (Sr, K, Rb, Pb, Ba) are enriched with respect to the HFSE values that are relatively flat and impoverished; the unit also exhibits a negative anomaly of Nb with respect to Th and Ce, being a magmatic arc the environment of generation. The ages obtained in biotite using the Ar-Ar method fall between 9.87±0.18 Ma and 11.44±0.36 Ma, Middle to upper Miocene (Tortonian-Serravallian), similar to age of other plutons that are part of the Botón Arc.
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Kavčič, Jerneja. "O prispevku slovenskega jezikoslovja k zgodovini starogrškega perfekta." Keria: Studia Latina et Graeca 12, no. 2-3 (December 31, 2010): 201. http://dx.doi.org/10.4312/keria.12.2-3.201-216.
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Pomemben prispevek k zgodovini starogrškega perfekta je dalo delo Erike Mihevc-Gabrovec Propad perfekta v pozni grščini (La disparition du parfait dans le grec de la basse époque). Obravnava perfekt v tedaj slabše poznanih virih cesarske in zgodnje bizantinske dobe. Nekoliko je zamajalo starejše poglede na sovpad med aoristom in perfektom. Vprašanje do danes kljub temu še ni bilo rešeno. Eden od možnih pristopov k reševanju tega problema se odpira tudi v okviru slovenske teorije naravne skladnje.
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SVETOZAROV, GEORGI, and CVETANA MANOVA. "THE SURVAKAR - MASQUERADE GAMES IN THE “SREDNO KRAISHTE” - VISUAL AND VERBAL DISCOURSE." Careers 2, no. 3 (December 27, 2022): 16–20. http://dx.doi.org/10.46687/uwhl2018.
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report given by Georgi Svetozarov and Tsvetana Manova at the geographical conference “Geo Decade” 2020 – 2030, is a presentation of a centuries old Bulgarian tradition, which represents “Surva” feast. This feast is tied to ancient customs and traditions for prosperity, health and fertility. The report on the topic: SURVA’S MASQUERADE GAMES IN “SREDNO KRAISHTE” REGION - VISUAL AND VERBAL DISCOURSE, shows the differences and similarities of an old tradition in one municipality, but in several different villages. The text represents the living traditional masquerade games in the days of Surva in the region of “Sredno Kraishte”. The research is based on photo-documentary materials, which are a complete historical source. They are juxtaposed with life narratives to complete and flesh out the picture. This approach makes it possible to trace the performance of the custom„Survakari” in the villages of Zemen, Elov dol, Berende, Gabrov dol, Divlya and Peshtera from the middle of the last century to the present days.
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VIERO, A. P., A. ROISENBERG, and F. H. S. MAGRO. "Gravimetria de Um Corpo Hipabissal Básico da Formação Serra Geral em Lomba Grande, RS." Pesquisas em Geociências 18, no. 2 (December 31, 1991): 156. http://dx.doi.org/10.22456/1807-9806.21354.
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A operacionalidade dos processos de fracionamento na evolução de corpos intrusivos é influenciada por vários fatores, dentre os quais a espessura e o volume da câmara magmática, que podem ser estimados através da gravimetria. O Complexo Básico de Lomba Grande, encaixado nos sedimentitos gonduânicos das Formações Sanga do Cabral e Botucatu, apresenta um corpo de olivina-gabro que perfaz mais de 95% do volume total do conjunto, mostrando variações químicas e mineralógicas significativas. Foram realizados estudos gravimétricos com aparelhagem Worden Gravity Meter – The Master, modelo 111, que identificam no corpo principal uma forma acanalada com espessura máxima da ordem de 450 metros. Estes resultados permitem inferir que o fracionamento observado no olivina-gabro não decorre de processos de assentamento gravitacional de cristais. O modelo sugerido corresponde a um fracionamento convectivo, originado pela migração de líquidos mais evoluídos e menos densos em direção ao topo da câmara.
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Nanang Sugianto, Refrizon, and Parjuangan Simbolon. "3D Deliniation of Geological Structure of Kepahiang Geothermal Area, Indonesia." Gravitasi 21, no. 2 (December 31, 2022): 69–80. http://dx.doi.org/10.22487/gravitasi.v21i2.16142.
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Deliniasi 3D struktur geologi daerah prospek Geothermal di Kabupaten Kepahiang telah dilakukan. Tujuan Penelitian adalah untuk mendapatkan gambaran subsurface dan geothermal system di Kepahiang serta memetakan zona alterasinya. Pemodelan kedepan dan inversi dilakukan kepada 194 data geomagnetik telah diukur menggunakan Proton Precission Magnetometer. Hasil analisi mendapati bahwa prospek lapangan geothermal di Kepahiang terdistribusi di Babakan Bogor, Barat Wetan, Pematang Donok, Tangsi Duren, Sido Makmur, dan Air Sempiang dengan kedalaman rata-rata reservoir 900 m dengan jenis batuan lapisan penudung yaitu gabro (ketebalan rata-rata 1100 m). Empat jenis formasi batuan ditemukan diantaranya batuan breksi gunung api, batuan basal, batuan gabro, dan batuan teralterasi. Anomali rendah yang berada di Babakan Bogor, Barat Wetan, Kuto Rejo, Pematang Donok, Tangsi Baru, Sido Makmur dan Air Sempiang diduga disebabkan oleh Sesar Segmen Musi yang masih aktif dan termagnetisasi secara induktif akibat reservoir panas bumi dari aktifitas Gunung Kaba
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Manchester, Ralph A. "Artists and Athletes." Medical Problems of Performing Artists 26, no. 1 (March 1, 2011): 1–2. http://dx.doi.org/10.21091/mppa.2011.1001.
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Several articles in this issue touch on some of the more athletic components of the performing arts. The article by Twitchett et al. describes fitness aspects of ballet, Gabrilo et al. discuss lung function in synchronized swimmers, and we also learn about how one flutist prepared for a very difficult piece by exercising (and practicing) in the letter by Borkowski. Of course, these are not the first articles in MPPA that look at performers as individuals who call on a variety of physical skills to create an artistic performance; examples of studies looking at both dancers and musicians dating back nearly a decade or more are easy to find.