Bibliografías temáticas / Klippes

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Literatura académica sobre el tema "Klippes"

Autor: Grafiati
Publicado: 4 de junio de 2021
Última modificación: 4 de febrero de 2022

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Artículos de revistas sobre el tema "Klippes"

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ILUNGA YANTAMBWE, Maurice y Jacques L. H. CAILTEUX. "Geological observations in the Five-Klippes area, northwestern Katanga Copperbelt (Democratic Republic of the Congo)". Geologica Belgica 22, n.º 3-4 (2019): 111–19. http://dx.doi.org/10.20341/gb.2019.006.

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Surface mapping and exploration in the search license PR-2348, northwest of Kolwezi in the Neoproterozoic Katanga Copperbelt, focussed in the poorly documented Five-Klippes area, and showed that the Roan megabreccias occurring at the ground surface in the klippes are composed mostly of Musonoï, Mines (Kamoto Formation) and Kiubo rocks that form km- to mm-size blocks, fragments and matrix. The megabreccias are bordered by rocks of the Kiubo Formation, that are gently dipping south on the northern side, with few approximatively 10 m-size sharp refolding close to the megabreccia, while they are vertically dipping north on the southern side. A 262 m-long exploration core drilling performed under the megabreccia of one of the klippes highlighted a faulting marked by hydraulic-like fractured-deformed Kiubo rocks and by friction breccias. The Kiubo blocks, fragments and matrix in the megabreccia were teared out most likely from the southern limb of the fault. The faulting in depth is interpreted here as the roots of the ground surface megabreccia. This rupture and shearing is questioning the autochthonous character of the surrounding Kiubo and Mongwe rocks. It is suggested that, similarly as for the eastern Mamfwe anticline, the Nguba and Kundelungu groups succession in the klippes area constituted blocks thrust during the fold-and-thrust event of the Katangan orogeny, and extruded the megabreccias of the klippes before suture during the final stage of the northward compression. A nearly north-south transversal faulting and shearing crosscutting the limbs and megabreccias of the klippes marked the end of the compression. These new observations complement other similar ones in that region, and have important implications for future Cu-Co exploration.
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Fabbri, Olivier, Rémi Magott, Marc Fournier y Lucas Etienne. "Pseudotachylyte in the Monte Maggiore ophiolitic unit (Alpine Corsica): a possible lateral extension of the Cima di Gratera intermediate-depth Wadati-Benioff paleo-seismic zone". BSGF - Earth Sciences Bulletin 189, n.º 4-6 (2018): 18. http://dx.doi.org/10.1051/bsgf/2018020.

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At the northern end of the Cap Corse peninsula, several klippes of ultramafic rocks (peridotite and serpentinite), among which the Monte Maggiore klippe is the least serpentinized one, rest upon continental-crust derived rocks (Centuri gneisses) and basic or metasedimentary schists (Schistes Lustrés). The Monte Maggiore ophiolitic klippe shares several characteristics with the Cima di Gratera klippe located 30 km further south. First, the two units are composed of a lherzolitic peridotite. Second, they record the same succession of metamorphic events. Third, in the Cap Corse tectonic pile, the two units occupy the highest structural position. Several differences are also observed. First, mafic rocks are significantly less abundant in the Monte Maggiore unit, where they are restricted to dykes cross-cutting the peridotite, than in the Cima di Gratera unit, where they constitute an entire sub-unit. Second, pyroxenite layers are more common at Monte Maggiore than at Cima di Gratera. Despite these differences, the Monte Maggiore and Cima di Gratera klippes can be considered as possible lateral equivalents of a single ophiolitic unit having covered the entire Cap Corse before subsequent erosion. Pseudotachylyte of seismic origin is newly discovered in the Monte Maggiore klippe. The host rock is a cataclastic serpentinized peridotite affected by a cataclastic foliation that is either flat-lying or steeply dipping. Pseudotachylyte fault veins are parallel to the host rock cataclastic foliation. The small lateral extension and the small thickness of fault veins along with frequent cross-cutting relationships suggest that the exposed pseudotachylyte most likely results from numerous small magnitude seismic events such as swarms or aftershocks rather than from large magnitude shocks. All these characteristics are also observed at the Cima di Gratera klippe where they are interpreted as the testimonies of a fossil intermediate-depth Wadati-Benioff zone at the time of subduction of the Ligurian Tethys oceanic lithosphere. Mineral assemblages that could constrain the depth of formation of the pseudotachylyte lack in the Monte Maggiore area. Despite this uncertainty, and given the similarities with the Cima di Gratera occurrences, the pseudotachylyte veins newly discovered at Monte Maggiore are tentatively related to the seismic activity linked with the subduction of the Piemonte-Ligurian oceanic lithosphere in Eocene times. This interpretation suggests that the fossil Wadati-Benioff zone could be traced further south in Alpine Corsica and further north in the Piemontese zone of the western Alps.
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Antal, András, István Pósa, József Varga, Zoltán Kovács y Gábor Nagy. "Egyszerűsített, gazdaságos laparoszkópos appendectomiar". Magyar Sebészet 60, n.º 2 (1 de abril de 2007): 87–89. http://dx.doi.org/10.1556/maseb.60.2007.2.4.

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Absztrakt A szerzők ismertetik a laparoszkópos appendectomia jelenlegi megítélését. Bemutatják a klippes appendix csonk zárással egyszerűsített műtéti technikát. Beszámolnak az első ötven műtétben szerzett kedvező tapasztalataikról. A műtéti technika az endolooposnál egyszerűbb, gyorsabb, az endoszkópos varrógépesnél lényegesen olcsóbb. Az eredmények alapján az ismertetett endoszkópos műtétet a hagyományos appendectomia értékes alternatívájának tekintik.
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IVANOV, Kirill Svyatoslavich y Victor Nikolaevich PUCHKOV. "On the stratigraphy and tectonics of Zilair synclinorium of the Urals". NEWS of the Ural State Mining University, n.º 4 (20 de diciembre de 2020): 67–72. http://dx.doi.org/10.21440/2307-2091-2020-4-67-72.

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The purpose of the work was to study the tectonic structure of the Zilair synclinorium of the Western slope of the southern Urals, which is important both from the general scientific point of view and for the needs of oil and gas prospecting of the territory. The main method of research was a detailed study of the stratigraphy of key sites with the search for conodonts in siliceous rocks. We also used data from seismic profiling of the territory. Result of work. The Zilair synclinorium of the southern Urals is an asymmetrically different facies structure; its Western and Eastern wings are composed of deposits belonging to different facies zones – the shelf (neritic) in the West and the continental slope and rise (bathyal) in the East. In the axial zone of the synclinorium, among the Famennian graywacke deposits of the Zilair series, several sites composed of cherts are known. It was believed, that the cherts are of Silurian age and are the klippes of a very large overthrust belonging to the ophiolite association. According to occurences of conodonts, we have established that all these cherts have Devonian, mainly Frasnian age. They are not klippes of an overthrust, but the central parts of the anticlinal folds, complicated by steep thrusts. According to our data, the real overthrust with a great horizontal amplitude is Pokrovsky, where two facial zones come into an abrupt contact without any transition between them.
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5

Kravchuk, Yaroslav, Roman Hnatiuk, Myroslav Ivanyk y Yaroslav Khomyn. "General features of relief of Marmaroshi and Pieniny rocks of Ukrainian Carpathians and their place under system of geomorphological regionalization". Visnyk of the Lviv University. Series Geography, n.º 42 (15 de octubre de 2013): 204–20. http://dx.doi.org/10.30970/vgg.2013.42.1860.

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Peculiarities of geological structure and relief of Ukrainian fragment of zones of Marmaroshi and Pieniny rocks located between Outer (Flysch) and Inner Carpathians are considered. Morphostructural differences and common features of relief of these zones are clarified. Territory of zones of Marmaroshi and Pieniny rocks is considered as separate geomorphological region of mountain part of Ukrainian Carpathians – subregion of Intermountain Valleys and Rocky Chains. Expediency of separation and taxonomic class of this geomorphological region are proved, its division into taxonomic units of lower class is realized. Key words: Marmaroshi rocks, Pieniny rocks, klippes (limestone rocks of Jurassic period), morphostructure, geomorphological regionalization, Ukrainian Carpathians.
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6

Puniya, M. K., R. C. Patel y P. D. Pant. "Structural and thermochronological studies of the Almora klippe, Kumaun, NW India: implications for crustal thickening and exhumation of the NW Himalaya". Geological Society, London, Special Publications 481, n.º 1 (19 de diciembre de 2018): 81–110. http://dx.doi.org/10.1144/sp481-2017-74.

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AbstractCrystalline klippen over the Lesser Himalayan Metasedimentary Sequence (LHMS) zone in the NW Himalaya have specific syn- and post-emplacement histories. These tectonics also provide a means to understand the driving factors responsible for the exhumation of the rocks of crystalline klippen during the Himalayan Orogeny. New meso- and microscale structural analyses, and thermochronological studies across the LHMS zone, Ramgarh Thrust (RT) sheet and Almora klippe in the eastern Kumaun region, NW Himalaya, indicate that the RT sheet and Almora klippe were a part of the Higher Himalayan Crystalline (HHC) of the Indian Plate which underwent at least one episode of pre-Himalayan deformation and polyepisodic Himalayan deformation in ductile and brittle–ductile regimes. The deformation temperature pattern within the Almora klippe records a normal thermal profile from its base to top but an inverted thermal profile from the base of Almora klippe down towards the LHMS zone. New fission-track data collected across the RT sheet and Almora klippe along Chalthi–Champawat–Pithoragarh traverse in the east Kumaun region document the exhumation of both units since Eocene times. Zircon fission-track (ZFT) ages from the Almora klippe range between 28.7 ± 2.4 and 17.6 ± 1.1 Ma, and from the RT sheet between 29.8 ± 1.6 and 22.6 ± 1.9 Ma; and the apatite fission-track (AFT) ages from the Almora klippe range between 15.1 ± 1.7 and 3.4 ± 0.5 Ma, and from the RT sheet between 8.7 ± 1.2 and 4.6 ± 0.6 Ma. The age pattern and diverse patterns of the exhumation rates reflect a clear tectonic signal in the RT sheet and the Almora klippe which acknowledge that the Cenozoic tectonics influenced the exhumation pattern in the Himalaya.
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Liu, Demin, Weiran Yang, Tieying Guo, Jiangtao Ru y Aimin Xiong. "Discussion on the Cenozoic tectonic evolution and dynamics of southern Tibet". Earth sciences and subsoil use 43, n.º 3 (7 de octubre de 2020): 307–24. http://dx.doi.org/10.21285/2686-9993-2020-43-3-307-324.

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Opening-closing tectonics is a new idea for exploring the global tectonics, which holds that every tectonic movement of all materials and geological bodies on earth is characterized by opening and closing. The opening-closing tectonic view can be used to explain some geological phenomena developing in continents which cannot be reasonably explained by the theory of plate tectonics. Based on the available basic geological data and combining with the opening-closing view, we analyzed the divisions and characteristics of tectonic units in South Tibet, and propose that Tibet can be divided into gravitational detachment and detachment fault zones, which are superimposed thrust fault zones and reconstructed normal fault zones, respectively. Although the mainstream opinion believed that the Tibetan Plateau is formed by collision-compression orogenesis, field investigation revealed the existence of the Rongbu Temple normal fault in the 1970s. We consider that the Rongbu Temple normal fault and the Main Central Thrust were formed earlier than the South Tibet detachment fault, and the former two faults constitute the two boundaries of the southern Tibet extrusion structure. The South Tibet detachment fault partially superimposes on the Main Central Thrust and manifests a relatively high angle in following the Rongbu Temple normal fault north of the Chomolangma. We suggest that the three fault systems are the products of different periods and tectonic backgrounds. The tectonic units, such as klippes and windows identified by previous researchers in southern Tibet, belong to thrust fault system but usually have no obvious extrusion or thrust characteristics; however, they are characterized by missing strata columns as younger strata overlapping the older ones. These klippes and windows should be the results of later gravitational decollement and must be characterized as extensions and slips, respectively. Based on opening-closing theory, we suggest that since the Cenozoic the study area had undergone multistage development, which can be divided into the oceanic crust expansion (opening) and subduction (closing) and the continental collision (closing) and intracontinental extension (opening) stages. Geothermal energy from the deep earth, gravitational potential energy from the earth’s interior, and additional stress energy from tectonic movements, all played a key role in the multistage tectonic evolutionary process.
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Saksa, Martin y Jozef Minár. "Assessing the natural hazard of gully erosion through a Geoecological Information System (GeIS): a case study from the Western Carpathians". Geografie 117, n.º 2 (2012): 152–69. http://dx.doi.org/10.37040/geografie2012117020152.

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The development of gullies represents a specific type of fluvial erosion that is triggered when surface runoff becomes concentrated during extreme rainfall events. This study investigates a part of the Považské Valley and Strážovské Mountains in Slovakia to assess the potential susceptibility and gully erosion hazard using a Geoecological Information System (GeIS). The landscape of the area was studied through primary field research and the analysis of secondary materials. The GeIS was then constructed in order to undertake specific multidimensional statistical methods. These were used to assess the potential susceptibly and gully erosion hazard. Those areas with the greatest potential susceptibility occur in Butkovská Furrow and the Podmanínska Hills whilst those with the least potential susceptibility occur in Butkovské Klippes and the Trenčianska Upland. The greatest gully erosion hazard was identified on arable land in the Podmanínska Hills and on the river terraces in the Ilavská Basin. It is clear that the majority of the permanent gullies within the study area are controlled by the course of existing anthropogenic linear features such as unpaved field and forest roads and balks in arable land.
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de Wever, P., G. Duee y K. El Kadiri. "Les series stratigraphiques des klippes de Chrafate (Rif septentrional, Maroc); temoins d'une marge continentale subsidente au cours du Jurassique-Cretace". Bulletin de la Société Géologique de France I, n.º 3 (1 de mayo de 1985): 363–79. http://dx.doi.org/10.2113/gssgfbull.i.3.363.

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Dommergues, Jean-Louis y Christian Meister. "Succession des faunes d'Ammonites du Sinémurien supérieurdans le Chablais méridional et les Klippes de Savoie (Préalpes Médianes, Haute-Savoie, France)". Geobios 22, n.º 4 (enero de 1989): 455–83. http://dx.doi.org/10.1016/s0016-6995(89)80099-3.

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Más fuentes

Tesis sobre el tema "Klippes"

1

TROBOUL, FREDERIC. "Le syndrome de klippel-trenaunay : a propos de 12 cas". Angers, 1988. http://www.theses.fr/1988ANGE1024.

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2

MAREY, LUCCHIN CATHERINE. "Syndrome de klippel-trenaunay : a propos d'un cas". Besançon, 1993. http://www.theses.fr/1993BESA3007.

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3

Sciaux-Panisset, Hélène. "Revue de la litterature recente a propos d'un cas de syndrome de klippel-trenaunay". Saint-Etienne, 1989. http://www.theses.fr/1989STET6025.

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4

Lindström, Anton. "Förskolan Klippan". Thesis, KTH, Arkitektur, 2018. http://urn.kb.se/resolve?urn=urn:nbn:se:kth:diva-223226.

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I started the project by doing a workshop with aclassmate using a derivative of the german officeBaupiloten’s methods. The goal of the workshop was toextract their actual needs and wishes.Traditionally when asking a client “What do you want?”,they’ll be constricted by their own reality and context.Taking children as an example they would ask for moreslides or a trampoline. By using an seemingly nonconnectedand abstract task the children can expresstheir actuals needs and wishes for their enviroment.We had a group of 8, 5 year old children that we showed 9pictures of natural phenomena while telling the childrenabout the pictures to spark their imagination. Afterwardwe asked each child to pick the pictures they liked. Withthem and other material we then instructed them to“construct worlds” inside A4-boxes. During the wholeprocess speaking to the children to extract their thoughtprocess as thoroughly as possible.On top of this the concept was based on the ongoingdebate regarding the lack of outdoor areas for childrenin Stockholm as well as the pedagogies of Reggio Emiliaand Montessori. From this I derived four key points.Exploration and independence, denuded architecture,free play outside and children’s inherent creativity.
Jag startade projektet genom att göra en workshop med en klasskamrat med hjälp av ett derivat från tyska arkitekturkontoret Baupilotens metoder. Målet med workshoppen var att extrahera deras faktiska behov och önskemål. Traditionellt när man frågar en klient "Vad vill du ha?", kommer de att vara begränsade av sin egen verklighet och kontext. Ta ett barn som exempel. De skulle be om mer rutschkanor eller en studsmatta. Genom att använda en till synes icke-kopplad och abstrakt uppgift barnen kan uttrycka deras faktiska behov och önskemål för deras omgivningar. Vi hade en grupp av åtta stycken, fem år gamla barn som vi visade nio bilder av naturfenomen samtidigt som vi berättade om bilderna för att tända barnens fantasi. Efteråt bad vi varje barn att välja bilderna som de tyckte mest om. Vi instruerade dem sedan till "Konstruera världar" i A4-lådor. Under hela processen talade vi med barnen för att extrahera deras tankeprocess så noggrant som möjligt. Utöver detta var konceptet baserat på den pågående debatten om bristen på utomhusområden för barn i Stockholm samt pedagogiken i Reggio Emilia och Montessori. Från detta härledde jag fyra huvudpunkter. Utforskning och självständighet, redovisande arkitektur, fri lek utomhus och barns inneboende kreativitet.
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Silva, Mauricio Pavan. "Modelamento metamórfico de rochas das fácies xisto-verde e anfibolito com o uso de pseudosseções: exemplo das rochas da Klippe Carrancas, sul de Minas Gerais". Universidade de São Paulo, 2010. http://www.teses.usp.br/teses/disponiveis/44/44143/tde-06052010-145012/.

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A Klippe Carrancas, frente do Sistema de Nappes Carrancas, está posicionada na borda sul do Cráton do São Francisco. A klippe é composta por rochas do Grupo Carrancas e estruturada da base para topo por quartzitos puros a micáceos, gradando verticalmente para estaurolita-granada-cloritóide-clorita filito ou cianita-estaurolita-granada xisto cinza porfiroblástico, dependendo das condições do metamorfismo. O metamorfismo gravado nas rochas aumenta para sudeste, da fácies xisto verde superior, na Serra da Estância, até a transição das fácies anfibolito-eclogito na Serra das Bicas, próximo a cidade de Carrancas. Os mapas metamórficos precedentes indicam a posição da isógrada da estaurolita nas proximidades de Itutinga, extremo leste da Serra do Pombeiro, e a ausência de biotita na Serra de Carrancas. A presente investigação reconheceu, a sudoeste de Itumirim, rochas com paragêneses da fácies xisto verde (cianita + clorita + cloritóide + muscovita + quartzo) e na Serra da Estância da fácies anfibolito inferior, zona da estaurolita, que é alcançada com a quebra do cloritóide em presença de cianita (granada + estaurolita + clorita +muscovita + quartzo ± cloritóide ± cianita). Na Serra do Pombeiro as condições da fácies anfibolito médio são alcançadas com o desaparecimento da clorita. Nas Serras de Carrancas e das Bicas ocorre paragênese da fácies anfibolito médio formada por cianita + estaurolita + granada + quartzo + muscovita. A influência da composição química da rocha no desenvolvimento das paragêneses foi avaliada em modelagem usando pseudosseções nos sistemas químicos KFMASH e MnKFMASH. O Mn aumenta consideravelmente o campo de estabilidade da granada. A previsão das associações minerais presentes no restante da região foi examinada a partir da composição química de algumas amostras, havendo boa concordância com os dados de campo. Aliadas às pseudosseções, técnicas de geotermobarometria, via razões catiônicas e geotermobarometria otimizada, permitiram determinar com boa confiabilidade as condições de metamorfismo para rochas dos dois extremos metamórficos descritos na Klippe Carrancas. Os resultados obtidos da comparação dos campos de estabilidade das paragêneses das amostras no sistema MnKFMASH, com os intervalos P-T da geotermobarometria otimizada forneceram condições de pico metamórfico para a Serra da Estância em 10,0 ±1,7 kbar e 577 ±8°C. Para a Serra das Bicas o pico metamórfico foi alcançado em 12,9 ±1,0 kbar e 608,5 ±19,5°C, com paragênese retro-metamórfica estabilizada em 7,0 ±2,2 kbar e 541,5 ±25,5°C. As associações minerais das amostras estudadas (estaurolita-granada-clorita-cloritóide-muscovita-quartzo - Serra da Estância; cianita-estaurolita-granada-quartzo-cianita - Serra das Bicas) são paragêneses típicas das fácies xisto-verde superior e anfibolito, respectivamente. No entanto, os resultados da geotermobarometria otimizada indicam que as rochas foram expostas a regimes mais elevados de pressão, colocando-as na transição com a fácies eclogito. Como as rochas são pelitos verdadeiros, de composição química restrita, as associações minerais de fácies anfibolito persistem em condições de maior pressão.
The Carrancas Klippe, front of the Carrancas Nappe System, is positioned at the southern edge of the São Francisco Craton. The klippe is composed of rocks from Carrancas Group and is structured from base to top by a pure to micaceous quartzite, grading vertically to a staurolite-garnet-chloritoid- chlorite phyllite or a gray porphyroblastic kyanite-staurolite-garnet schist, depending on the conditions of metamorphism. The metamorphism recorded in these rocks increases to the southeast, from upper greenschist facies in the Serra da Estância to the transition to eclogite facies on Serra das Bicas, nearby Carrancas town. Previous metamorphic maps indicate the position of the staurolite-in isograd near Itutinga town, at far east of the Serra do Pombeiro, and the absence of biotite in the Serra de Carrancas. In this research it was recognized that to the southwest of Itumirim town, the rocks bear greenschist facies paragenesis (kyanite + chlorite + chloritoid + muscovite + quartz) and in Serra da Estância a low amphibolite facies, in the staurolite zone, which is achieved with the breakdown of chloritoid in the presence of kyanite (garnet + staurolite + chlorite + muscovite + quartz ± chloritoid ± kyanite). At Serra do Pombeiro conditions of intermediate amphibolite facies are reached with the disappearance of chlorite. On Serra de Carrancas and Bicas occurs intermediate amphibolites facies paragenesis, formed by kyanite + staurolite + garnet + quartz + muscovite. The influence of bulk composition in the development of some parageneses was evaluated using pseudo-section modelling in KFMASH and MnKFMASH systems. Mn increases the stability field of garnet. The prediction of mineral associations present in the rest of the region was done using the bulk composition of some samples, which show good agreement with field data. Allied to pseudo-sections, isopleth-geothermobarometry and optimal geothermobarometry allowed to determine, with good reliability, the metamorphic peak conditions for rocks of the two metamorphic extremes described in the Carrancas Klippe. The results of comparing the stability fields of the parageneses in the MnKFMASH system of the samples, with P-T intervals from optimal geothermobarometry, provide reliable conditions for the metamorphic peak. In Serra da Estância, peak metamorphic conditions were at 10.0 ± 1.7 kbar and 577 ± 8?. For Serra das Bicas, metamorphic peak conditions were reached at 12.9 ± 1.0 kbar and 608.5 ± 19.5°C, with retro-metamorphic paragenesis stabilized at 7.0 ± 2.2 kbar and 541.5 ± 25.5°C. The mineral associations of the studied samples (staurolite-garnet-chlorite-chloritoid-muscovite-quartz - Serra da Estância; kyanite-staurolite-garnet-quartz-kyanite - Serra das Bicas) are typical parageneses of the greenschist facies and upper amphibolites facies, respectively. However, the results of optimal geothermobarometry indicate that the rocks were exposed to higher pressure regimes, reaching the transition to eclogite facies. Since the rocks are true pelites, with restricted bulk composition, the mineral associations of amphibolite facies persist through conditions of greater pressure.
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Klippel, Stefan [Verfasser]. "MRI Cell-labeling with Xenon Nanocarriers / Stefan Klippel". Berlin : Freie Universität Berlin, 2015. http://d-nb.info/1074404785/34.

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Thébaut, Jean-François. "Syndrome malformatif lymphangiomateux complexe : syndrome de Klippel Trenaunay ou syndrome de Protée : à propos d'un cas". Bordeaux 2, 1990. http://www.theses.fr/1990BOR25200.

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Peirone, Udriot Luciano. "Urban Building Hornsbruksgatan, Klippan". Thesis, KTH, Arkitektur, 2012. http://urn.kb.se/resolve?urn=urn:nbn:se:kth:diva-96676.

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KLIPPAN Byggnadens form utgår från platsens morfologi och topologi. Konkav mot staden och konvex mot parken, utskjutande mot hornsbruksgatan och fasad mot Högalidsparken. I gränsen mellan natur och stad vill den ta fasta på båda världars egenskaper och styrkor och samtidigt utgöra länken dem emellan. En klippa som sträcker ut sig mot det urbana landskapet med Högalidskyrkan i ryggen. Den skapar möten och förenar inom ramen av sig själv och de cirkulationsflöden den ger. Klippan förlänger parken genom sitt offentliga terrasstak och utgör samtidigt en öppning från stad till park. Ett trappsystem placerat på den södra delen leder in besökaren till de offentliga delarna av byggnaden. Ett centralt system, direkt till parken. Härigenom skapas ett följsamt möte mellan stad och park samtidigt som gränsen mellan privat och offentligt luckras upp inom ramen för byggnadens mixade programmering. Ett bibliotek/ideastore placerat på markplan i riktning mot Hornstull, samsas med kontorsdelar mot tunnelbanan. I de två övre planerna ligger programdelar som direkt har ett utbyte av varandras närhet, uthyrbara kontorsplatser, arbetsförmedling, ateljéer och kafé. Boendedelen är fristående och placerad ovanpå T-banestationen, men ändå integrerad genom det externa cirkulationssystemet -------------------------------------------------------------- Utgångspunkten är mötet mellan stad och natur, park.   Idén är att skapa en byggnad som starkt relaterar till sin gränslandet och samtidigt har en självständig identitet   Platsen har idag en rad olika och i viss mån separerade kvalitéer. Grönområde - urbanitet - närhet till olika noder - T-bana - urban knytpunkt - Hornstull.   Byggnaden ska ta till vara på dessa kvalitéer genom att arbeta med mötet där emellan. Genom att knyta ihop dem kan en tredje sfär skapas inom ramen för byggnaden och dess omgärde.    - Hur koppla ihop delarna?   - Hur få ut något intressant och bra?   Macrostrategi Byggnadens externa relation Öppna upp cirkulationsflödet mellan gaturum och park.   Öppna upp siktlinjer - skapa visuella kopplingar från gaturum till park - från byggnad till sin omgivning.   Distribution av programdelar i relation till plats. Funktionsseparering i olika volymer som placeras optimalt enligt programmatiska krav och behov.   - Arbetsplats och Ideastore mot gata. Kapitaliserar på platsens urbana kvalitéer. Gatans närhet - puls, liv, samt tar vara på existerande siktlinjer. (se diagram)   - Bendet placeras ovanpå tunnelbanestationen och får därigenom privacitet och närhet till grönområde utan att ber ut si på bekostnad av offentligt område.   Microstrategi - byggnadens interna relation Inhysa olika programdelar i samma byggnad. Programdelarna får behålla sin särart samtidigt som viss integrering och korsbefruktning kan ske. Härigenom kapitalisera på utbyte och ömsesidig påverkan mellan programdelar.   byggnaden är organisering är så att de mer statiska programdelarna, kontor och boende, är något mer separerade, medan mer dynamiska programdelar som kan ha stort utbyte av varandras närhet är mer integrerade.placerade i varandras närhet eller i direkt anslutning. Bibliotek/läsesalar, arbetsförmedling, open office och ateljéer samt kafé     Arbetade länge med programmets placering i olika plan utan att bestämma fasadens uttryck. Så småningom valde jag att omsluta allt av ett relativt enhetligt hölje, en fasetterad stålstruktur som håller upp ömsom genomskinliga ömsom frostade glas facetter.  Internt gav det frihet att integrera och separera programdelarinom ramen för ett stort klimatskikt. Skapandet av ett "fjärde rum" den programmatiska intersektionen. Höljet ger också flexibilitet i fråga om programmatiska krav, vad gäller ljusinsläpp, utsikt och insyn.   Exteriört pratar höljet om olika saker. Olikhet och mångfald genom den mosaiska fasetterade ytan och samtidigt ocom enhetlighet och kollektivitet eftersom det är inlemmat ett övergripande system.   IDEASTORE - bibliotek/medialab - learninglab - joblab - restaurang   ARBETSPLATS- corporate- workspace - ateljeer - corporate   BOENDE - studentboende- familjeboende
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Klippel, Nathan John. "The effects of hip angle manipulation on submaximal oxygen consumption in collegiate cyclists". Thesis, Montana State University, 2004. http://etd.lib.montana.edu/etd/2004/klippel/KlippelN1204.pdf.

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Isard, Sierra Juliane. "Origin of the Tower Peak unit in the St. Cyr area, Yukon, Canadian Cordillera". Thesis, University of Iowa, 2014. https://ir.uiowa.edu/etd/4651.

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The Yukon-Tanana terrane (YTT) is a composite arc built on the rifted margin of western North America. The YTT is present in the southeastern part of the St. Cyr area in south-central Yukon, but in the northwest section the structural and lithologic relationships are poorly known. This study describes the structural geometry of the northwest section of the St. Cyr area, west of the Canol Road. The lithological, geochemical, and geochronological characteristics of the Tower Peak unit are investigated in an effort to determine its origin and terrane affinity. In the study area, the Tower Peak unit sits tectonically above a low-grade mafic-ultramafic unit. In turn, this mafic-ultramafic unit is thrust over phyllite and marble creating a composite klippe. Detrital zircons from the marble indicate a maximum depositional age of 368 Ma. This result is consistent with the footwall being part of the Devonian to Mississippian Finlayson assemblage, the oldest arc of the composite YTT. The Tower Peak unit is a massive but fractured, sub-greenschist facies metabasalt. Whole-rock and trace element geochemistry of four Tower Peak samples suggest an oceanic or island arc setting for deposition of the Tower Peak unit. Zircons separated from three samples of the Tower Peak unit give a range of U-Pb ion probe ages. Three distinct age populations exist: 600-2582 Ma, 433-303 Ma, and 140-190 Ma. The preferred interpretation is that the Tower Peak unit is Mesozoic in age and may derive from Stikinia or Quesnellia.
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Libros sobre el tema "Klippes"

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Gasiński, M. Adam. Campanian-Maastrichtian palaeoecology and palaeobiogeography of the Andrychów klippes, Outer Carpathians, Poland. Kraków: Wydawn. Uniwersytetu Jagiellońskiego, 1998.

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Klippies. London: Bloomsbury Methuen Drama, 2015.

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Adam, Olivier. Klippen: Roman. München: SchirmerGraf, 2008.

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Edwards, Deborah. Robert Klippel. Sydney: Art Gallery of New South Wales, 2002.

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Westall, Robert. Das Versteck unter den Klippen. Zürich: Nagel und Kimche, 1993.

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Nenning, Günther. Auf den Klippen des Chaos. Hamburg: Hoffmann und Campe, 1993.

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Murray, Ena. En die klippe sal uitroep. Kaapstad: Tafelberg, 1993.

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Schreyer, Wolfgang. Der Mann auf den Klippen: Roman. Berlin: Militärverlag der Deutschen Demokratischen Republik, 1987.

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Glodde, Britta. Das Haus an den Klippen: Roman. 2a ed. Berlin: Ullstein, 1999.

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Eichhorn, Joachim Samuel. Durch alle Klippen hindurch zum Erfolg. München: OLDENBOURG WISSENSCHAFTSVERLAG, 2009. http://dx.doi.org/10.1524/9783486706550.

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Capítulos de libros sobre el tema "Klippes"

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Hsü, K. J. y U. Briegel. "Die Klippen". En Geologie der Schweiz, 83–98. Basel: Birkhäuser Basel, 1991. http://dx.doi.org/10.1007/978-3-0348-8663-5_7.

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Gilbert, Patricia. "Klippel-Feil syndrome". En The A-Z Reference Book of Syndromes and Inherited Disorders, 172–74. Boston, MA: Springer US, 1996. http://dx.doi.org/10.1007/978-1-4899-6918-7_45.

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Lasanianos, Nick G., George K. Triantafyllopoulos y Spiros G. Pneumaticos. "Klippel Feil Syndrome". En Trauma and Orthopaedic Classifications, 231–33. London: Springer London, 2014. http://dx.doi.org/10.1007/978-1-4471-6572-9_51.

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Menon, Riju Ramachandran. "Klippel-Trenaunay Syndrome". En Chronic Venous Disorders of the Lower Limbs, 229–33. New Delhi: Springer India, 2014. http://dx.doi.org/10.1007/978-81-322-1991-0_23.

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Kaltofen, Heike, Dierk A. Vagts, Uta Emmig y Peter Biro. "Klippel-Feil-Syndrom". En Anästhesie bei seltenen Erkrankungen, 1–2. Berlin, Heidelberg: Springer Berlin Heidelberg, 2018. http://dx.doi.org/10.1007/978-3-662-44368-2_70-1.

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Strölin, Anke. "Maurice Francois Klippel". En Pantheon of Dermatology, 595–98. Berlin, Heidelberg: Springer Berlin Heidelberg, 2013. http://dx.doi.org/10.1007/978-3-642-33224-1_99.

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Vaccaro, Mario, Claudio Guarneri, Richard F. Ambinder, S. Diane Hayward, Marcia Spinelli Casanova, Oladapo Adewuya, Ferid Murad et al. "Klippel-Feil Syndrome". En Encyclopedia of Molecular Mechanisms of Disease, 1124–25. Berlin, Heidelberg: Springer Berlin Heidelberg, 2009. http://dx.doi.org/10.1007/978-3-540-29676-8_3325.

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Chen, Harold. "Klippel-Feil Syndrome". En Atlas of Genetic Diagnosis and Counseling, 1663–72. New York, NY: Springer New York, 2017. http://dx.doi.org/10.1007/978-1-4939-2401-1_142.

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Chen, Harold. "Klippel-Trenaunay Syndrome". En Atlas of Genetic Diagnosis and Counseling, 1673–84. New York, NY: Springer New York, 2017. http://dx.doi.org/10.1007/978-1-4939-2401-1_143.

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Trinidad-Hernandez, Magdiel y Peter Gloviczki. "Klippel-Trenaunay Syndrome". En Vascular Surgery, 535–42. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-65936-7_47.

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Actas de conferencias sobre el tema "Klippes"

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Braga, Murillo y Ari Scussel Junior. "Traumatismo raquimedular na síndrome de klippel-feil". En XXXII Congresso Brasileiro de Neurocirurgia. Thieme Revinter Publicações Ltda, 2018. http://dx.doi.org/10.1055/s-0038-1673080.

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P., Sangeetha R., Nisha Baskar y Sriganesh Kamath. "Craniotomy in Klippel–Trenaunay Syndrome: Concerns and Challenges". En Abstracts of 21st Annual Conference of the Indian Society of Neuroanaesthesiology and Critical Care (ISNACC 2020). Thieme Medical and Scientific Publishers Private Ltd., 2020. http://dx.doi.org/10.1055/s-0040-1709602.

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Candoso Neri de Jesus, S., C. Feldmann, M. Schulze, M. Kalder, BA Stuck, AH Mahnken y U. Geisthoff. "Interdisziplinäres Atemwegsmanagement bei laryngealer Beteiligung bei Klippel-Trénaunay-Syndrom". En Abstract- und Posterband – 91. Jahresversammlung der Deutschen Gesellschaft für HNO-Heilkunde, Kopf- und Hals-Chirurgie e.V., Bonn – Welche Qualität macht den Unterschied. © Georg Thieme Verlag KG, 2020. http://dx.doi.org/10.1055/s-0040-1710446.

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Leung, Enoch, Nesrin Sarigul-Klijn y Rolando F. Roberto. "Characterization of Irregular Stress Distributions Induced by Klippel Feil Syndrome". En ASME 2011 International Mechanical Engineering Congress and Exposition. ASMEDC, 2011. http://dx.doi.org/10.1115/imece2011-63343.

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Klippel Feil Syndrome (KFS) is a congenital disorder characterized by failure of segmentation of cervical vertebrae, resulting in “fusions” at any level of the cervical spine. Clinical diagnosis of KFS occurs at a mean age of 7.1 years, with children diagnosed with KFS often exhibiting reduced motion and function characterized by reduction of upward and downward motions of the head on the neck (flexion/extension), axial rotation, and tilting of the head side to side (lateral bending). More importantly, however, previous KFS studies have acknowledged possible compromises to the structural integrity and overall health of the cervical spine in the presence of abnormal fusion. Instances of instabilities such as fracture and large amounts of mobility at vertebral segments adjacent to fusion have been recorded, both posing significant neurological and physiological dangers to an individual afflicted with KFS. While fusion and instability appear to be interrelated, more intrinsic evaluation of KFS-related instabilities is needed. Current KFS studies, relying predominantly on static radiographic modalities, have been unsuccessful in identifying factors contributing to craniocervical (CC) destabilization in the presence of congenital vertebral fusion. It has been hypothesized that fusion of vertebral bodies induces abnormal stress distributions that catalyze instances of fracture along any KFS spine segment. Using Finite Element (FE) Modeling and Analysis to characterize motion alterations and irregular stress patterns associated with vertebral fusion, a high fidelity computational representation of a KFS affected cervical spine segment spanning the base of the occiput to C6 was constructed. Computer Tomography (CT) images were used for vertebral reconstruction with soft tissue components such as intervertebral discs (IVDs), articular cartilages (ACs), and the transverse ligament were modeled as homogenous solid components.
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Schultz, Art, Fred Webb y Mercer Parker. "FENSTER, KLIPPE, LANDSLIDE, GRABEN, SINKHOLE: WHAT HAPPENED AT BLAND, VIRGINIA?" En 67th Annual Southeastern GSA Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018se-309626.

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Lolic, I., V. Milivojević, VM Zarić, N. Jocić, D. Popovic, T. Glišić, I. Ranković, O. Matejic y D. Tomić. "THINK ABOUT KLIPPEL-TRENAUNAY SYNDROME IN RECURRENT RECTAL BLEEDING PRESENTATION – CASE REPORT". En ESGE Days. © Georg Thieme Verlag KG, 2020. http://dx.doi.org/10.1055/s-0040-1704676.

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Candoso Neri de Jesus, S., C. Feldmann, M. Schulze, M. Kalder, BA Stuck, AH Mahnken y U. Geisthoff. "Airway management of laryngeal manifestation of a patient with Klippel-Trénaunay syndrome". En Abstract- und Posterband – 91. Jahresversammlung der Deutschen Gesellschaft für HNO-Heilkunde, Kopf- und Hals-Chirurgie e.V., Bonn – Welche Qualität macht den Unterschied. © Georg Thieme Verlag KG, 2020. http://dx.doi.org/10.1055/s-0040-1710779.

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Quadros, Danilo, Wagner Tavares, Almir de Andrade, Matheus Yamaki y Bruno Reis. "Caso ilustrativo: síndrome de Klippel-Feil e fratura traumática longitudinal de vértebras cervicais fundidas". En XXXII Congresso Brasileiro de Neurocirurgia. Thieme Revinter Publicações Ltda, 2018. http://dx.doi.org/10.1055/s-0038-1672521.

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Jaramillo, Valeria, Thomas A. Johnson, John M. Cottle, Kyle P. Larson y Andrew R. C. Kylander-Clark. "INSIGHTS INTO THE EMPLACEMENT OF THE KATHMANDU KLIPPE FROM QUARTZ MICROSTRUCTURES AND TITANITE PETROCHRONOLOGY". En GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-335783.

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Bosu, Somiddho, Delores Robinson y Gourab Bhattacharya. "KINEMATIC ANALYSIS OF THE ALMORA KLIPPE: TESTING TECTONIC MODELS OF THE HIMALAYAN THRUST BELT". En 50th Annual GSA South-Central Section Meeting. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016sc-274015.

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Informes sobre el tema "Klippes"

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Lee, Byung Boong y Fausto Passariello. Klippel-Trenaunay Syndrome. Fondazione Vasculab, mayo de 2016. http://dx.doi.org/10.24019/2016.ktrenaunay.

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Stacey, J. R. y D. R. M. Pattison. Stratigraphy, structure, and petrology of a representative klippe of the Bravo Lake Formation, Piling Group, central Baffin Island, Nunavut. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2003. http://dx.doi.org/10.4095/214195.

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Isard, S. J., J. A. Gilotti, W. C. McClelland, M. B. Petrie y C. R. van Staal. Geology and U-Pb geochronology of low-grade mafic rocks from the St. Cyr klippe and a marble from the footwall, Canadian Cordillera, Yukon. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2016. http://dx.doi.org/10.4095/297474.

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Solie, D. N. Killik River Quadrangle, northcentral Brooks Range. Preliminary report on Kikiktat Mountain: a klippe of basalts, cherts, and calcareous arkosic sediments in the northern Brooks Range, Alaska. Alaska Division of Geological & Geophysical Surveys, 1986. http://dx.doi.org/10.14509/1207.

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