Relevant bibliographies by topics / S-37

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Academic literature on the topic 'S-37'

Author: Grafiati
Published: 4 June 2021
Last updated: 16 February 2022

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Journal articles on the topic "S-37"

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Lowry, Sam. "Oregon Clips Measure 37's Wings." Planning & Environmental Law 60, no. 1 (January 2008): 9–10. http://dx.doi.org/10.1080/15480750802203213.

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Dries, D., J. Gramm, H. Lujan, and R. Gamelli. "37; TOXIC EPIDERMAL NECROLYSIS IN THE 90??s." SHOCK 1, Supplement (January 1994): 11. http://dx.doi.org/10.1097/00024382-199401001-00038.

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Kleidman, P. B., and A. J. E. Ryba. "Kostant′s Conjecture Holds for E7: L2(37)." Journal of Algebra 161, no. 2 (November 1993): 535–40. http://dx.doi.org/10.1006/jabr.1993.1234.

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Penna, Ivanna Marina. "Tectonism and erosion as conditioning factors for slope collapses in the Andean Cordillera (37-37°30′S)." Quaternary International 279-280 (November 2012): 374. http://dx.doi.org/10.1016/j.quaint.2012.08.1153.

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Pandorf, T., and R. Preuss. "S-37 In-Vivo like Testing of Ceramic Ball Heads." Journal of Biomechanics 43 (June 2010): S44. http://dx.doi.org/10.1016/s0021-9290(10)70090-7.

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Baltrus, PT, TE Raghunathan, and GA Kaplan. "#37-S race, socioeconomic position and long-term weight gain." Annals of Epidemiology 12, no. 7 (October 2002): 503–4. http://dx.doi.org/10.1016/s1047-2797(02)00325-3.

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Roberts, Rebecca L., Mary C. Wallace, Jill M. Drake, and Lisa K. Stamp. "Identification of a novel thiopurine S-methyltransferase allele (TPMT*37)." Pharmacogenetics and Genomics 24, no. 6 (June 2014): 320–23. http://dx.doi.org/10.1097/fpc.0000000000000049.

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Rehak, Katrin, Manfred R. Strecker, and Helmut P. Echtler. "Morphotectonic segmentation of an active forearc, 37°–41°S, Chile." Geomorphology 94, no. 1-2 (February 2008): 98–116. http://dx.doi.org/10.1016/j.geomorph.2007.05.002.

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Penna, I. M., R. L. Hermanns, S. Niedermann, and A. Folguera. "Multiple slope failures associated with neotectonic activity in the Southern Central Andes (37 -37 30'S), Patagonia, Argentina." Geological Society of America Bulletin 123, no. 9-10 (June 24, 2011): 1880–95. http://dx.doi.org/10.1130/b30399.1.

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Nivière, Bertrand, Grégoire Messager, Sébastien Carretier, and Pierre Lacan. "Geomorphic expression of the southern Central Andes forebulge (37°S, Argentina)." Terra Nova 25, no. 5 (April 27, 2013): 361–67. http://dx.doi.org/10.1111/ter.12044.

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Dissertations / Theses on the topic "S-37"

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Lara, Pulgar Luis Enrique. "NEOTECTONIQUE DE L'ARC VOLCANIQUE QUATERNAIRE DES ANDES DU SUD DU CHILI ENTRE 37° ET 42° S." Phd thesis, Université Paul Sabatier - Toulouse III, 2006. http://tel.archives-ouvertes.fr/tel-00123663.

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Les Andes du Sud au Chili se développent sur la marge active du continent Sud Américain, entre la plaque de Nazca et la plaque de l'Amérique du Sud et sont le résultat global de la convergence oblique durant le Cénozoïque. L'arc volcanique quaternaire, représenté par la Zone Volcanique Sud (ZVS: 33º-46ºS) présente une architecture qui peut être mise en rapport avec la déformation crustale développée dans cette marge convergente. Les provinces méridionales de la ZVS, situées entre 37ºS et le Point Triple du Chili (46ºS), coexistent avec la Zone de Faille Liquiñe-Ofqui (ZFLO), une structure d'intra-arc de longue vie. En particulier, l'arc volcanique dans le segment 37º-42° est formé par une série de chaînes volcaniques transversales et des groupes de cônes monogéniques situés sur la ZFLO dont l'évolution est le résultat de l'interaction entre les processus magmatiques et la néotectonique de l'arc volcanique.
L'étude de la néotectonique entre 37º-42ºS, avec l'analyse des caractéristiques principales du volcanisme dans cette région, permettent d'établir qu'une telle interaction est complexe au-delà de la relation spatiale évidente entre des volcans et des failles. D'abord, elle souligne l'influence de la croûte continentale fracturée qui est sous-jacente à l'arc volcanique. Tant la configuration préalable de l'arc que les anisotropies du substratum exercent un fort contrôle sur l'ascension, la mise en place et l'évolution des magmas quaternaires comme on peut le signaler, par exemple, dans le cas du Complexe Volcanique Puyehue-Cordón Caulle.
Le régime de déformation quaternaire, caractérisé par une transpression générale dextre avec une contrainte horizontale maximale (s1=sHmax) NE-SW, contrôlerait spécialement la distribution et l'évolution des chaînes transversales holocènes ainsi que les cônes de flanc dans les stratovolcans. Ce régime de contraintes régionales, en tout cas, dévie localement en s'adaptant aux structures du substratum. De même, des tenseurs de compression existent dans quelques secteurs et expliqueraient le soulèvement relatif de surfaces qui sont signalées dans la morphologie de la cordillère. Ces mouvements verticaux dans la ZFLO s'associeraient aussi avec des épisodes discrets de volcanisme qui permettent l'ascension de magmas primitifs directement depuis la source asthénosphérique.
Cependant, des tenseurs de transpression comme de compression maintiennent un s1=sHmax constant de direction NE-SW, ce qui justifie l'influence de la tectonique dans le transport de magma à travers la croûte comme étant une caractéristique d'échelle régionale.
De même, bien que moins récurrent, le déclenchement à distance d'éruptions volcaniques en raison de grands séismes dans la zone de subduction est un facteur additionnel qui explique certains épisodes et il est superposé au régime de déformation corticale à l'intérieur de l'arc volcanique.
Finalement, l'étude à l'échelle régionale des régimes de déformation crustale et le volcanisme associé permettent de comprendre comment se forme l'architecture complexe d'un arc volcanique, dont l'évolution spatiale et temporelle est contrôlée par une multiplicité de facteurs mais qui présente d'importantes régularités des transferts de masse à travers la croûte.
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Lara, Pulgar Luis Enrique. "Néotectonique de l’arc volcanique quaternaire des Andes du sud du Chili entre 37° et 42° S." Toulouse 3, 2006. https://tel.archives-ouvertes.fr/tel-00123663.

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Entre 37° et 42°S, la néotectonique et les caractéristiques du volcanisme suggèrent une interaction complexe, due à la proximité entre volcans et failles. L'influence du socle préfracturé est importante. Le champ de contrainte quaternaire, caractérisé par une transpression dextre (σ1=SHmax NE-SW), contrôle la distribution tant des chaînons obliques holocènes que des cônes de flanc des stratovolcans. Des régimes compressifs locaux le long du Système de Faille Liquiñe-Ofqui peuvent partiellement expliquer le soulèvement local qui serait aussi lié à des événements volcaniques discrets. Cependant, la direction de σ1, tant pour les tenseurs transpressifs que compressifs est la même, ce qui confirmerait l'influence régionale de la tectonique crustale sur la montée des magmas et le volcanisme. L'étude régionale des champs de contrainte et des caractéristiques volcaniques permet de comprendre comment l'architecture complexe de l'arc est configurée et comment le transfert de masse se fait à travers la croûte
The Southern Andes in Chile occur along the active margin between Nazca and South American plates and they are a global result of the oblique convergence since the Cenozoic. Quaternary volcanic arc, there represented by the Southern Andean Volcanic Zone (SVZ: 33°-46ºS) shows an architecture that can be related with the crustal deformation along the convergent margin. The southern provinces of the SVZ between 37ºS and the Chile Triple Junction (46ºS), occur next to the Liquiñe-Ofqui Fault Zone (LOFZ), a long-lived intra-arc system. Specifically, the arc segment between 37°-42°S is formed by several oblique volcanic chains and clusters of monogenetic cones located atop of the LOFZ, which are a result of the interaction between magmatic and tectonic processes in the arc. Neotectonic study of the volcanic arc between 37°-42°S, together with the analysis of the main features of volcanism in the region, allow to establish a rather complex interaction, beside the close spatial relationship between volcanoes and faults. First of all, the influence of the prefractured continental crust that underlies the arc should be remarked. The previous arc geometry and the basement anisotropy exert a strong control on the magma ascent, as can be observed on the Puyehue-Cordón Caulle Volcanic Complex case-study. .
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González-Reyes, Álvaro, James McPhee, Duncan A. Christie, Quesne Carlos Le, Paul Szejner, Mariano H. Masiokas, Ricardo Villalba, Ariel A. Muñoz, and Sebastián Crespo. "Spatiotemporal Variations in Hydroclimate across the Mediterranean Andes (30°–37°S) since the Early Twentieth Century." AMER METEOROLOGICAL SOC, 2017. http://hdl.handle.net/10150/625182.

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In the Mediterranean Andes region '(MA; 30 degrees-37 degrees S), the main rivers are largely fed by melting snowpack and provide freshwater to around 10 million people on both sides of the Andes Mountains. Water resources in the MA are under pressure because of the extensive development of industrial agriculture and mining activities. This pressure is increasing as the region faces one of its worst recorded droughts. Previous studies have pointed to El Nioo-Southern Oscillation '(ENSO) as the main climatic force impacting the MA. However, the role of decadal and multidecadal climate variability, their spatial patterns, and the recurrence of long-term droughts remains poorly studied. In an attempt to better understand these factors, spatial and temporal patterns of hydroclimatic variability are analyzed using an extensive database of streamflow, precipitation, and snowpack covering the period between 1910 and 2011. These analyses are based on the combination of correlation, principal components, and kernel estimation techniques. Despite a general common pattern across the MA, the results presented here identify two hydroclimatic subregions, located north and south of 34 degrees S. While the interannual variability associated with ENSO is slightly stronger north of 34 degrees S, the variability associated with the Pacific decadal oscillation '(PDO) and/or the interdecadal Pacific oscillation '(IPO) index shows similar patterns in both regions. However, variations produced by the IPO forcing seem to be greater in the southern subregion since 1975. The estimations presented here on drought recurrence reveal a generalized increase in dry extremes since the 1950s. These findings suggest that the northern MA is more vulnerable to changes in hydrology and climate than the southern MA.
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Ramos, Santiago Daniel Hernandez-Piloto. "A dimensão formativa do cinema e a catarse como categoria psicológica : um diálogo com a psicologia histórico-cultural de Vigotski." Mestrado em Educação, 2015. http://repositorio.ufes.br/handle/10/1535.

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FAPES
A pesquisa trata da relação entre a estética do filme e a dimensão sensível do espectador, e toma como eixo central deste diálogo o conceito de catarse desenvolvido na Psicologia da arte de Vigotski (1999b). O objetivo é compreender como o conceito de catarse pode contribuir para a reflexão, no âmbito da educação dos sentidos (formação estética), bem como se ele pode criar as condições e possibilidades para transformar, qualitativamente, o espectador em contato com o filme/cinema. A metodologia é de cunho eminentemente teórico-reflexivo, realizada a partir do levantamento bibliográfico, análise de trabalhos acadêmicos com foco no conceito-chave. Pressupõe-se que, na sociedade contemporânea, o cinema é uma das principais vias de formação estética, com presença significativa no processo de constituição da individualidade em diversos contextos sociais. A dimensão reflexiva da pesquisa também opera a partir da análise do filme Fresa y Chocolate (1993), do cineasta cubano Tomás Gutierrez Alea. Uma primeira hipótese considera que a dimensão formativa do cinema só chega a sua máxima concretude quando o espectador, na vivência com o filme, é elevado a um nível superior de transformação qualitativa a partir das emoções contrárias suscitadas pela narrativa estética – conflito entre conteúdo x forma. Uma segunda hipótese considera que a perspectiva estética de Gutierrez Alea, em especial no filme Fresa y Chocolate (1993), aproxima-se da concepção de catarse desenvolvida por Vigotski. Desse modo, esse conceito pode contribuir para, no âmbito do campo dos fundamentos da educação, ampliar a reflexão sobre a compreensão da reação estética que o espectador experimenta em contato com o filme, cuja função vai além da representação da realidade, ele pode ser considerado a própria visão social do espectador sobre a realidade. A catarse, como fundamento da reação estética experimentada pelo espectador com a obra, constitui-se em uma complexa transformação sensível e, também, da própria consciência e percepção da realidade objetiva.
The academic research deals with the relationship between the aesthetics of film and the sensitive dimension of the viewer and takes as its central axis of this dialogue the concept of catharsis at the Psychology of Art Vygotsky (1999b). The objective of the research is to understand how the concept of catharsis can contribute with the reflection in the field of education of the senses (aesthetic training) and if he can create the conditions and possibilities to transform qualitatively the viewer in contact with the film / cinema. The methodology is eminently of theoretical-reflective nature. Used the study of the literature, analysis of the scholarly works focusing on catharsis key concept. The research takes as its premise that, in contemporary society, the cinema is one of the main routes of aesthetic, with a significant presence in the process of formation of individuality in different social contexts. The reflective dimension of the survey also operates from the analysis of the film Fresa y Chocolate (1993), by Cuban filmmaker Tomas Gutierrez Alea. A first hypothesis considers that formative dimension of cinema only reaches its maximum concreteness when the viewer, the experience with the film, is elevated to a higher level of qualitative transformation from opposing emotions aroused by the aesthetic narrative - conflict between content and form. A second hypothesis that considers the aesthetics perspective of Gutierrez Alea, in particular Fresa y Chocolate (1993) approaches the concept developed by Vygotsky of catharsis. Thus, this concept can contribute to, in the field of education, broaden reflection on the understanding of the aesthetic response that the viewer experiences in contact with the film, whose function goes beyond the representation of reality, it can be considered the viewer's own vision of social reality. Catharsis, as the foundation of aesthetic response experienced by the viewer with the work, is in a complex transformation sensitive and also of one's consciousness and perception of objective reality.
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Mota, Erika Maria Targino. "Distribuição e abundância do ictioplâncton na plataforma continental (42-37 W, 48-21 S) no Nordeste do Brasil." reponame:Repositório Institucional da UFC, 2013. http://www.repositorio.ufc.br/handle/riufc/11216.

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MOTA, E. M. T. Distribuição e abundância do ictioplâncton na plataforma continental (42-37 W, 48-21 S) no Nordeste do Brasil. 2013. 69 f. Dissertação (mestrado em Ciências Marinhas Tropicais) - Instituto de Ciências do Mar, Universidade Federal do Ceará, Fortaleza, 2013.
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Information about distribution and abundance of ichthyplankton during the larval period is essential for fisheries biology, because the phenomena occurring in this phase are crucial for the recruitment, affecting the stock available for capture. Although research about fish eggs and larvae are common in many regions of the world, but studies for the coast of Ceará are scarce. In 2010, 54 samples were collected, divided into two campaigns. (Campaign 1 (July) and Campaign 2 (October)). The trawls were horizontal subsurface a plankton net of 300 mm in mesh. The collected material was analized and identified, and found 3,829 eggs and fish larvae 3665. In Campaign 2 showed a greater abundance of larvae, in contrast eggs showed the highest abundances in the campaign 1. Engraulidae and Gobiidae were more prominent in the campaigns. The families Gobiidae, Engraulidae and Gerreidae were classified as frequent. The species found on the continental shelf of the states of Ceará and Piauí are important fishery resources for the local population.
Informações sobre a distribuição e abundância do ictioplâncton durante o período larval é essencial para a biologia pesqueira, pois os fenômenos ocorridos nessa fase são determinantes para o recrutamento, afetando o estoque disponível para a captura. Embora pesquisas sobre ovos e larvas de peixes sejam frequente em diversas regiões do mundo, os estudos para o litoral do Ceará são escassos. O objetivo deste trabalho foi estudar a distribuição e a abundância da comunidade de ovos e larvas de peixes na plataforma continental dos estados Ceará e Piauí (Brasil, Nordeste). No ano de 2010, 54 coletas foram realizadas, divididas em duas campanhas. (Campanha 1 – Julho e Campanha 2 – Outubro). Os arrastos foram horizontais subsuperficiais, através de rede de plâncton de 300 μm de malha (acoplados com fluxômetro), com a duração de aproximadamente 5 minutos. O material coletado foi triado e identificado, tendo sido encontrados 3.829 ovos e 3.665 larvas de peixes. Na campanha 2 obteve-se maior abundância de larvas, em contraste os ovos apresentaram as maiores abundâncias absolutas na campanha 1. As famílias Engraulidae e Gobiidae tiveram maior destaque nas campanhas. Em relação à frequência, Gobiidae, Engraulidae e Gerreidae foram classificados como frequentes. As espécies encontradas na plataforma continental dos estados do Ceará e Piauí são importantes recursos pesqueiros para a população ribeirinha. Algumas dessas famílias compõem o grupo das mais importantes encontradas nas zonas costeiras tropicais.
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Schauer, Anja [Verfasser], Hortense [Gutachter] Slevogt, Kerstin [Gutachter] Voigt, and Ulrike [Gutachter] Seifert. "Die Bedeutung von Interleukin-37 (IL-37) bei der durch Streptococcus pneumoniae (S. pneumoniae) induzierten Lungenentzündung sowie der Progression in eine Sepsis / Anja Erika Schauer ; Gutachter: Hortense Slevogt, Kerstin Voigt, Ulrike Seifert." Jena : Friedrich-Schiller-Universität Jena, 2019. http://d-nb.info/117738695X/34.

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Hunt, Brian Peter Vere. "Mesozooplankton community structure in the vicinity of the Prince Edward Islands (Southern Ocean) 37⁰ 50'E, 46⁰ 45'S." Thesis, Rhodes University, 2000. http://eprints.ru.ac.za/11/.

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Kuun, Patrick John. "Morphometrics and preliminary biology of the caridean shrimp Nauticaris marionis Bate, 1888, at the Prince Edward Islands (South Ocean), 37° 50'E, 46° 45'S." Thesis, Rhodes University, 1998. http://hdl.handle.net/10962/d1005419.

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Carapace length, as the best measure of N. marionis body size, is precisely defined. It is shown that N. marionis is a partially protandric hermaphrodite. N. marionis appear to hatch just before April each year, with a little hatching persisting until May. The vast majority of juveniles develop into males. The majority of males transmutate into females in their third year. By April/May the transmutation is probably complete. Reproduction can occur before all male secondary characteristics have been lost. A small minority of individuals develop directly into females without passing through a male phase. At least some of these females can be initially recognized after they have developed mature ovaries by the presence of appendices internae on their first pleopods, a male copulatory structure which all juvenile N. marionis possess. Too few gravid females were recovered to make any statement on whether spawning can occur before this structure is lost. Such females may lose their first pleopod appendices internae in one moult, possibly just before spawning, which may be in late April/early May. Such individuals seem to mature into ovigerous females at a slightly smaller carapace length than do the majority of females which have had a male-phase past. A few females which have passed through a male phase seem to begin developing ovaries at about this small carapace length as well. Once the appendices internae have been lost there appears to be no way of identifying any given female's past life-history. It would seem that during the first year of life N. marionis survive in undetected localities, moult into juveniles, and then settle amongst the benthos from the plankton. Diurnal vertical migration then occurs up to an unknown larger size. It is not known whether the larvae are initially planktonic or not. It is possible that settling of small N. marionis onto the benthos only begins after November. Whether the appendices masculinae of some males only begin growing after they have settled Abstract XIX onto the benthos is unknown, but for the majority at least this begins whilst they are planktonic juveniles. Individuals older than five years are undetectable using samples of the sizes analyzed in this thesis, but they may well persist until quite an advanced age. Niche separation between smaller and larger N. marionis individuals may occur. Diel vertical migration may occur to some extent amongst large N. marionis. Itinerant euphausiids may contribute substantially to the maintenance of top predator populations at the archipelago, either through direct predation by those predators or via predation by N. marionis, which in turn are consumed by those predators. N. marionis itself is an opportunistic feeder, although the majority of its prey seem to be suspension feeders, both benthic and pelagic. In multisample situations, ageing of N. marionis cohorts is made less subjective if one utilizes the phenomenon of synchronized sexual inversion. The von Bertalanffy growth parameters for N. marionis are tentatively identified as k = 0.2353/year, L_ = 12.69mm, to = -0.2828 years and WW_ = 2.03g. The programme FiSAT is discussed, having been found to be extremely useful, but having also been found to have certain faults. Various hypotheses are proposed and are put forward as suggestions for future studies.
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González, Reyes Alvaro Ignacio. "Modelación de la línea de equilibrio altitudinal (ELA) desde el año A.D. 1500, y variaciones climáticas recientes en los Andes Mediterráneos de Chile (30°-37°S)." Tesis, Universidad de Chile, 2019. http://repositorio.uchile.cl/handle/2250/170189.

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Tesis para optar al grado de Doctor en Ciencias, Mención Geología
La variabilidad del clima durante el último milenio (A.D 1000 - 2000), permitió que diversos glaciares de montaña a escala global hayan experimentado su máximo crecimiento en térmi- nos de su masa, respecto a actuales condiciones. Las causas climáticas de este crecimiento glaciar se relacionan con La Pequeña Edad de Hielo (PEH; A.D 1500 - 1850). Este periodo de interés paleoclimático global ha sido bien documentado en el hemisferio Norte, contrario al hemisferio Sur.. Más aún, existe un desconocimiento profundo acerca de cómo, mecanismos climáticos que actualmente afectan el clima de regiones como los Andes Mediterráneos de Chile y Argentina (AM; 30-37 S), como El Niño Oscilación del Sur, hayan afectado el balance de masa glaciar y las variaciones temporales de la línea de equilibrio altitudinal (ELA) duran- te dicho intervalo. La PEH es un antónimo a lo que acontece actualmente con los glaciares de montaña, donde en regiones como los AM diversos estudios han identificado un severo retroceso. El balance de masa glaciar (MB) y su ELA está influenciado por los cambios en la temperatura del aire, elevación de la Isoterma de 0C y las precipitaciones. La presente tesis doctoral consta de dos capítulos y un capítulo introductorio. Un primer capítulo exhibe las tendencias de las variables climáticas que actúan directamente sobre el MB, y mencionadas anteriormente. Un segundo capítulo, presenta una modelación de la ELA durante A.D 1500 - 1848 mediante un modelo forzado por tres modelos climáticos globales (GCMs). Se estudió las relaciones entre las variaciones temporales en la Temperatura Superficial del Mar (SST) del Océano Pacífico y la variabilidad temporal de la ELA. La temperatura media se ha in- crementado significativamente durante enero, febrero, marzo, y desde agosto a noviembre, considerando 1969 - 2016. La temperatura mínima, por su parte, se ha incrementado signifi- cativamente durante enero y mayo, mientras que la temperatura máxima, excepto en mayo, julio y septiembre, se ha incrementado significativamente durante 1969 - 2015. La isoterma de 0oC (ISO0) registró un incremento significativo en enero, marzo y anual durante 1858 - 2015. Tendencias en la ISO0 (años 2000 - 2015) exhiben un incremento significativo durante enero, mayo, junio y agosto. La precipitación (pp) de abril a septiembre registró una ne- gativa y significativa tendencia desde 1876, con reducciones significativas durante los meses de mayo, junio y julio. Entre 1981 - 2015, una significativa reducción ha sido registrada en la pp de abril a agosto. La ELA anual durante la PEH registró una elevación de 3775 m. Una menor elevación de la ELA fue identificada durante A.D 1640 - 1670 y 1800 - 1948. Contrariamente, una mayor elevación de la ELA fue identificada durante A.D 1550 - 1575. Propiedades espectrales de la ELA modelada indican significativas señales de entre 2 - 7 años de periodicidad, y también señales decadales a multi decadales. Significativas señales espec- trales fueron también obtenidas con el primer modo de variabilidad de la SST región Niño 3.4. Además, correlaciones significativas fueron obtenidas entre la ELA anual y la SST en la región Pacífico. Se propone que la variabilidad de la SST del océano Pacífico fue el principal modulador de los cambios temporales de la ELA en los AM durante A.D 1500 - 1848.
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Molina, del Canto Pablo Antonio. "Evidencias e implicación de deformación intracristalina en olivinos de los conos monogenéticos Caburga y La Barda y estratovolcanes Copahue y Callaqui de la zona volcánica Sur (37° -39°S)." Tesis, Universidad de Chile, 2016. http://repositorio.uchile.cl/handle/2250/142081.

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Se seleccionaron los conos monogenéticos de La Barda y Caburga y los estratovolcanes de Callaqui y Copahue para estudiar olivinos deformados en lavas de estos volcanes pertenecientes a la Zona Volcánica Sur. Se determinó que en ambos tipos de volcanes los olivinos deformados son de origen cortical, hay presencia de antecristales, evidencias de mezcla de magma, poblaciones de cristales, zonaciones normales e inversas, la mayoría de los núcleos de olivinos se localizan fuera del equilibrio con su fundido hospedante, presentan prácticamente la misma distribución de tamaños de grano (en núcleos deformados y no deformados), igual distribución de tipo de evidencia óptica de deformación. Difieren en que los conos monogenéticos presentan una mayor proporción de olivinos deformados y una densidad de dislocaciones cualitativamente mayor. Además, las proporciones de tipo de zonación entre núcleos deformados y no deformados son diferentes entre ambos tipos de volcanes. No hay diferencia en tamaño, forma, textura, química que permita distinguir olivinos deformados de no deformados. Solo diferencias ópticas permiten su clasificación. Se propone que la deformación de los olivinos se produciría en reservorios profundos e intermedios y en conductos de ascenso en la corteza. En los reservorios someros (estratovolcanes) y temporales (conos monogenéticos) no se produciría deformación debido a las bajas presiones y temperaturas a las que se verían afectados. En estos reservorios se adquirirían las zonaciones químicas. La mayor proporción de olivinos deformados en conos monogenéticos se explicaría por los procesos de recuperación de dislocaciones, los que disminuirían la densidad de dislocaciones. Estos procesos operarían en ambos tipos de volcanes, pero en los estratovolcanes debido a los mayores tiempos de residencia afectarían a los cristales deformados por más tiempo.
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Books on the topic "S-37"

1

Ilʹin, V. E. S-37, 1.44: Rossiĭskie istrebiteli poslednego pokolenii︠a︡. Moskva: AST, 2002.

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Koralova, Nevena. Razgovori v kadŭr i zad kadŭr: S 37 bŭlgarski muzikanti. Sofii︠a︡: Zvezdan, 2004.

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Koralova, Nevena. Razgovori v kadŭr i zad kadŭr: S 37 bŭlgarski muzikanti. Sofii︠a︡: Zvezdan, 2004.

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Demaría, Laura Beatriz. Argentina-s: Ricardo Piglia dialoga con la generación del 37 en la discontinuidad. Bs. As. [i.e. Buenos Aires]: Corregidor, 1999.

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Sauget, Joseph-Marie. Deux panegyrika melkites pour la seconde partie de l'année liturgique: Jérusalem S. Anne 38 et Ḥarīṣā 37. Città del Vaticano: Biblioteca apostolica vaticana, 1986.

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Sauget, Joseph-Marie. Deux panegyrika melkites pour la seconde partie de l'année liturgique: Jérusalem S. Anne 38 et Harīsā 37. Città del Vaticano: Biblioteca Apostolica Vaticana, 1986.

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United States. Congress. Senate. Committee on Energy and Natural Resources. Subcommittee on Public Lands, Forests, and Mining. Miscellaneous public land bills: Hearing before the Subcommittee on Public Lands, Forests, and Mining of the Committee on Energy and Natural Resources, United States Senate, One Hundred Thirteenth Congress, first session, on S. 37, S. 343, S. 364, S. 404, S. 509, S. 753, S. 1169, S. 1300, S. 1301, S. 1309, H.R. 507, H.R. 862, H.R. 876, H.R. 993, July 30, 2013. Washington: U.S. Government Printing Office, 2013.

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The last king(s) of Judah: Zedekiah and Sedekias in the Hebrew and Old Greek versions of Jeremiah 37(44):1-40(47):6. Tübingen, Germany: Mohr Siebeck, 2017.

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National trails bills: Hearing before the Subcommittee on National Parks of the Committee on Energy and Natural Resources, United States Senate, One Hundred Seventh Congress, second session on S. 213, S. 1069, S. 1946, H.R. 37, H.R 834, H.R. 1384, March 7, 2002. Washington: U.S. G.P.O., 2002.

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Kukharenko, Tatʹi︠a︡na Alekseevna. Kommentariĭ k Federalʹnomu zakonu ot 2 i︠a︡nvari︠a︡ 2000 g. no. 37-FZ O narodnykh zasedateli︠a︡kh federalʹnykh sudov obshcheĭ i︠u︡risdikt︠s︡ii v Rossiĭskoĭ Federat︠s︡ii: Postateĭnyĭ : s uchetom noveĭshikh podzakonnykh aktov. Moskva: ĖlKnigi, 2012.

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Book chapters on the topic "S-37"

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Sukhoruchkin, S. I., and Z. N. Soroko. "Excited Nuclear States for S-37 (Sulfur)." In Nuclei with Z = 1 - 29, 2024–38. Berlin, Heidelberg: Springer Berlin Heidelberg, 2012. http://dx.doi.org/10.1007/978-3-642-22798-1_237.

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Sukhoruchkin, S. I., and Z. N. Soroko. "Excited Nuclear States for S-37 (Sulfur)." In Supplement to I/25 A-E, 675–77. Berlin, Heidelberg: Springer Berlin Heidelberg, 2015. http://dx.doi.org/10.1007/978-3-662-47801-1_136.

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Sukhoruchkin, S. I., and Z. N. Soroko. "Atomic Mass and Nuclear Binding Energy for S-37 (Sulfur)." In Nuclei with Z = 1 - 54, 1008–10. Berlin, Heidelberg: Springer Berlin Heidelberg, 2009. http://dx.doi.org/10.1007/978-3-540-69945-3_466.

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Sagripanti, Lucía, Andrés Folguera, Lucas Fennell, Emilio Agustín Rojas Vera, and Victor A. Ramos. "Progression of the Deformation in the Southern Central Andes (37°S)." In Springer Earth System Sciences, 115–32. Cham: Springer International Publishing, 2015. http://dx.doi.org/10.1007/978-3-319-23060-3_6.

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von Roth, Dominik, and Ulrike Roesler. "Nr. 37 | F. [Franz] Brendel, „Ein dritter Ausflug nach Weimar“, in: NZfM 19 (1852), Bd. 37, Nr. 22 (26. November), S. 225–227; Nr. 23 (3. Dezember), S. 237–240; Nr. 24 (10. Dezember), S. 251–254." In Die Neudeutsche Schule – Phänomen und Geschichte, 362–80. Stuttgart: J.B. Metzler, 2020. http://dx.doi.org/10.1007/978-3-476-04923-0_37.

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Litvak, Vanesa D., Stella Poma, Rosemary E. Jones, Lucía Fernández Paz, Sofía B. Iannelli, Mauro Spagnuolo, Linda A. Kirstein, Andrés Folguera, and Victor A. Ramos. "The Late Paleogene to Neogene Volcanic Arc in the Southern Central Andes (28°–37° S)." In The Evolution of the Chilean-Argentinean Andes, 503–36. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-67774-3_20.

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von Roth, Dominik, and Ulrike Roesler. "Nr. 131 | Oscar Comettant, „Liszt, Wagner, Schumann, and Baron, and the Vital Fluids!“, in: The Musical World 37 (1859), Nr. 37 (10. September), S. 588f." In Die Neudeutsche Schule – Phänomen und Geschichte, 1644–53. Stuttgart: J.B. Metzler, 2020. http://dx.doi.org/10.1007/978-3-476-04923-0_131.

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Reisinger, Peter. "Circular Dichroism Spectra of Native 37 S Hemocyanin from the Spider Eurypelma Californicum and Its Subunits." In Invertebrate Oxygen Carriers, 203–6. Berlin, Heidelberg: Springer Berlin Heidelberg, 1986. http://dx.doi.org/10.1007/978-3-642-71481-8_34.

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Sánchez, Natalia, Martín Turienzo, Isabelle Coutand, Fernando Lebinson, Vanesa Araujo, and Luis Dimieri. "Structural and Thermochronological Constraints on the Exhumation of the Chos Malal Fold and Thrust Belt (~37° S)." In Opening and Closure of the Neuquén Basin in the Southern Andes, 323–40. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-29680-3_13.

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von Roth, Dominik, and Ulrike Roesler. "Nr. 76 | Franz Liszt, „Berlioz und seine Haroldsymphonie“, in: NZfM 22 (1855), Bd. 43, Nr. 3 (13. Juli), S. 25–32; Nr. 4 (20. Juli), S. 37–46; Nr. 5 (27. Juli), S. 49–55; Nr. 8 (17. August), S. 77–84; Nr. 9 (24. August), S. 89–97." In Die Neudeutsche Schule – Phänomen und Geschichte, 873–933. Stuttgart: J.B. Metzler, 2020. http://dx.doi.org/10.1007/978-3-476-04923-0_76.

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Conference papers on the topic "S-37"

1

Da Lio, B., H. Terai, T. Yamashita, J. S. Neergaard-Nielsen, M. Galili, K. Rottwitt, U. L. Andersen, et al. "Co-Existence of 87 Mbit/s Quantum and 10 Gbit/s Classical Communications in 37-Core Fiber." In 2019 Conference on Lasers and Electro-Optics Europe & European Quantum Electronics Conference (CLEO/Europe-EQEC). IEEE, 2019. http://dx.doi.org/10.1109/cleoe-eqec.2019.8871492.

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Kong, D., A. A. Jørgensen, M. R. Henriksen, F. Klejs, Z. Ye, Ò. B. Helgason, H. E. Hansen, et al. "Single Dark-Pulse Kerr Comb Supporting 1.84 Pbit/s Transmission over 37-Core Fiber." In CLEO: Applications and Technology. Washington, D.C.: OSA, 2020. http://dx.doi.org/10.1364/cleo_at.2020.jth4a.7.

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Poirrier, Julien, Suzanne Salaun, Gerard Buxeres, Bruno Raguenes, Frederic Neddam, and Maryse Moignard. "Field demonstration of 10 Gbit/s transmission over a 37 ps PMD cable using electronic mitigation." In 2008 Conference on Optical Fiber Communication - OFC 2008 Collocated National Fiber Optic Engineers. IEEE, 2008. http://dx.doi.org/10.1109/ofc.2008.4528210.

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Vasiliev, S. S. "About the influence of the mechanism of equalization of tariffs of electric energy (power) to industrial enterprises of the Republic of Sakha (Yakutia)." In XX Anniversary All-Russian Scientific and Practical Conference of Young Scientists, Postgraduates and Students. Technical Institute (BRANCH) of NEFU, 2019. http://dx.doi.org/10.18411/s-2019-37.

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Hender, U., T. Lund-Hansen, and D. Winther. "COMPARISON OF THE EFFECT OF FACTOR VII PREPARED FROM HUMAN PLASMA (pVIIa) AND RECOMBINANT Vila (rVIIa) IN VITRO AND IN RABBITS." In XIth International Congress on Thrombosis and Haemostasis. Schattauer GmbH, 1987. http://dx.doi.org/10.1055/s-0038-1643788.

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Purified human FVIIa has been shown to induce haemostasis in pat. with haemoph. A compl. with antibodies against VIII:C (Hedner & Kisiel 1983). The in vitro effect of addition of pVIIa or rVIIa was studied by adding 0, 44, or 180 u pVIIa/rVIIa/ml to haemoph. A or haemoph. B plasma. The APTT shortened from 61 s (mean of 5 determin.) without any Vila added to 38 s after addition of 44 u pVIIa to haemoph. A plasma, and to 33 s after addition of 180 u/ml. In haemoph. B plasma the corresponding APTTs were 64 s, 35 s (44 u pVIIa/ml Vila) and 31 s (180 u pVIIa/ ml). Similar results were obtained when rVIIa was added to the same plasmas. In haemoph. A plasma APTT was shortened from 66 S to 52 s (50 u rVIIa/ml) and to41s(159u rVIIa/ml), and in haemoph. B plasma 71 s,44 s,and 37 s.Also in plasma from pat. with acquired antibodies against VIII:C a shortening of APTT was found both of pVIIa (60 s, 37 s, and 32 s) and rVIIs (65 s, 38 s, and 33 s). In normal plasma the APTT only shortened a few seconds after addition of the same amounts of pVIIa/rVIIa per ml (30 s, 27 s, 25 s). The doses required to normalize the APTT in vitro exceed substantially the doses used in vivo so far. The pVIIa and rVIIa were therefore also given i.v. to rabbits.Plasma samples were drawn before inj., 15 min, 2 hrs,4 hrs, 8 hrs, and 24 hrs after and platelets, APTT, fib.gen, ATIII, α2M, α2AP, ethanol gel. test, FVII,Hb, Hkr were followed. Doses of 500 u/kgb.w.,1000 or 5000 u/kg b.w. were given. No signs of a gen.activ.of the coag. were observed. The FVII level in plasm rose adequately. In conclusion higher doses of Vila than used clin. so far may be needed to achieve full haemost. effect in haemoph. pat. or pat. with acq. antibodies against VIII:C. Such doses also seem to be safe. rVIIa was as active as pVIIa and as safe in rabbits.
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Kull, Lukas, Danny Luu, Christian Menolfi, Thomas Morf, Pier Andrea Francese, Matthias Braendli, Marcel Kossel, Alessandro Cevrero, Ilter Ozkaya, and Thomas Toifl. "A 10-Bit 20–40 GS/S ADC with 37 dB SNDR at 40 GHz Input Using First Order Sampling Bandwidth Calibration." In 2018 IEEE Symposium on VLSI Circuits. IEEE, 2018. http://dx.doi.org/10.1109/vlsic.2018.8502268.

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Cobbold, P. R., E. A. Rossello, and F. O. Marques. "Compressional Growth Strata Of Late Oligocene To Miocene Age In The Loncopué And Catan-Lil Intermontane Basins, Neuquén Province, Argentina (37°- 40° S)." In 9th Simposio Bolivariano - Exploracion Petrolera en las Cuencas Subandinas. European Association of Geoscientists & Engineers, 2006. http://dx.doi.org/10.3997/2214-4609-pdb.111.79.

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McKenna, R., E. R. Cole, A. Yuk, and W. Whisler. "NORMAL APTT IN A PATIENT WITH A PERSISTENT ACQUIRED FACTOR XI INHIBITOR." In XIth International Congress on Thrombosis and Haemostasis. Schattauer GmbH, 1987. http://dx.doi.org/10.1055/s-0038-1643303.

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A 55 year-old white male (MR) with documented normal hemostatic tests at our institution for 14 years, was admitted for a laminectomy. His pre-operative APTT and prothrombin time activity (Q) were again normal. A prolonged APTT of 58 seconds (21-31 N) and Q of 18% (> . 70% N) was noted on the 14th post-operative day; patient had received I unit PRBC during surgery.Mixtures of pooled normal plasma (NPP) incubated with MR’ s plasma (301, 37° C) yielded normal APTTs with as little as 20% NPP in these mixtures, suggesting a plasma factor(s) deficiency. Factor XI level was undetectable with normal values of factors Vlll-C, IX and XII. A factor XI level of 7% was found in incubated mixtures (60’ , 37° C) of equal parts of NPP + MR’ s plasma as compared to 70% in NPP + buffer and < 1% in MR’ s native plasma + buffer, indicating the presence of an inhibitor in MR’ s plasma. Infusion of 1540 ml of FFP (22 ml/kg) to the patient resulted in an APTT of 28 seconds and a Q of 36% with a persistent undetectable XI (expected ∿ 45%). The in-vivo lack of response to FFP was also suggestive of an inhibitor.Additional in-vitro tests showed that the response of MR’ s plasma was no different from that of NPP with the addition of increasing dilutions of human brain thromboplastin, differentiating this inhibitor from the Lupus type anticoagulant. The severely reduced Q was due to severe temporary reductions in factors II (20%), V (34%), Vll/X (2%) and X (20%) without any evidence of hepatocellular dysfunction or vitamin K deficiency. Fibrinogen, thrombin time, FSP, platelet counts and bleeding times remained normal throughout.There was no external evidence of bleeding after the first operation at any site, despite 1M injections and venepunctures. MR was reoperated on day 15 for a cauda equina hematoma; adequate intra and 72 hour post-operative management was with 1 U FFP Q 6 hourly and Amicar; this was associated with a normal PTT, Q %35% and undetectable XI, but without generalized bleeding. Discontinuation of this regimen resulted in onset of bleeding from drainage tubes only, without bleeding from the rest of the incision. Reinstitution of I U FFP Q 12 hourly and Amicar resulted in a prompt cessation of bleeding. Patient had no evidence for an autoimmune disease, dyspro-teinemia or any other illness. The potential role of the 1 unit of PRBC transfused cannot be discounted. Further data on this inhibitor will be presented.
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Hong, Seung-Seo, YoungSeok Kim, Jung-Hee Park, Jangguen Lee, and Jong-Sub Lee. "Temperature Distribution and Frozen Soil Characteristics at Jangbogo Antarctic Research Station." In ASME 2012 31st International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2012. http://dx.doi.org/10.1115/omae2012-83121.

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Temperature monitoring along the depth in construction site of the Jangbogo Antarctic research station (74° 37′S, 164° 12′E) was carried out. The thermal behavior of the frozen ground was investigated. The temperatures were measured during site investigation from February 07, 2011 to February 12, 2011. The temperature profile was analyzed in the frozen ground. The results show that the increase along with the depth. This study demonstrates that the temperature profile obtained at this site could be effective reference for the construction of the research station in the Antarctic.
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Zhang, Chun-Lin, Gui-Cheng Yuan, De-Chang Liu, Han-Ping Chen, Ding-Yu Liu, and Rong Wang. "An Experimental Study of the Gaseous Pollution Emissions in Petroleum-Coke-Fired Fluidized Beds." In 17th International Conference on Fluidized Bed Combustion. ASMEDC, 2003. http://dx.doi.org/10.1115/fbc2003-030.

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Petroleum cokes have high calorific value (about 37 MJkg−1), high sulfur content (2–7% wt.), and high nitrogen content (1∼3% wt.), introducing serious environmental problems when using as fuel. In this paper the effects of operating parameters (bed temperature, Ca/S mole ratio, and excess oxygen) on gaseous pollutant (SO2, NO, and N2O) emissions in a well-controlled bench scale fluidized bed reactor and an 1t/h bubbling fluidized bed for different type of petroleum cokes. Finally, the pollution emission differences between petroleum coke and coal were compared and the reasons were analyzed.
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