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Tesis sobre el tema "Tectonic processes"

Autor: Grafiati

Publicado: 4 de junio de 2021

Última modificación: 26 de julio de 2025

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1

McAllister, Edward. "Tectonic processes on the mid-Atlantic ridge." Thesis, University of Leeds, 1995. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.429571.

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2

Ghail, Richard Charles. "An investigation of regional tectonic processes on Venus." Thesis, Lancaster University, 1996. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.337568.

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3

Parke, Jeffrey Robert. "Active tectonic and sedimentary processes in Western Turkey." Thesis, University of Cambridge, 2001. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.621363.

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4

Hoppa, Gregory Vincent 1972. "Europa: Effects of rotation and tides on tectonic processes." Diss., The University of Arizona, 1998. http://hdl.handle.net/10150/282763.

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Tides due to orbital eccentricity may have a substantial effect on the rotation and tectonics observed on Jupiter's moon, Europa. A direct measurement of Europa's rotation rate has been made by measuring the positions of surface features relative to the terminator in both Voyager and Galileo images. From these measurements I have found that the rotation of Europa relative to the direction of Jupiter is <0.5° over a 17 year period, i.e. one rotation with respect to Jupiter would require at least 12,000 years. Non-synchronous rotation is also a significant source of global stress which, combined

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5

Thiede, Rasmus Christoph. "Tectonic and climatic controls on orogenic processes the Northwest Himalaya, India /." Phd thesis, [S.l.] : [s.n.], 2005. http://deposit.ddb.de/cgi-bin/dokserv?idn=974306037.

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6

Jolley, Stephen J. "Mid crustal thrust tectonic processes : examples from the Dalradian of N.W. Donegal." Thesis, Durham University, 1994. http://etheses.dur.ac.uk/5884/.

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A D2 ductile thrust imbricate stack has been identified within the mid greenschist facies (Appin Group) metasediments of the Breaghy Head area of Co. Donegal. Major stratigraphy parallel tectonic slides detach arrays of subsidiary ductile thrust imbricates, which display patterns of intensifying strain and minor structures generally regarded as being diagnostic of the much broader thrust sense shear zones (tectonic slides) which typify deformation within metamorphic "parts of mountain belts. This commonality of structural associations implies that the. Breaghy Head imbricates and their broader

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7

Keller, William R. Heaton Thomas H. "Cenozoic plate tectonic reconstructions and plate boundary processes in the Southwest Pacific /." Diss., Pasadena, Calif. : California Institute of Technology, 2004. http://resolver.caltech.edu/CaltechETD:etd-01102005-223039.

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8

Lloyd, Ryan. "InSAR observations of active magmatic and tectonic processes in the East African Rift." Thesis, University of Bristol, 2018. http://hdl.handle.net/1983/cd90b7ee-5e84-46f9-8b14-2335913438bb.

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Continental rifting is achieved through a combination of magmatic and amagmatic processes. However, these processes can be influenced by heterogeneities at a range of scales, which act as regions of relative strength and weakness in the crust. The subaerial East African Rift, the longest continental rift on Earth, demonstrates the transition between incipient amagmatic and mature magmatic rifting. The rift interacts with geology that spans 3.8 Ga, and thus represents the ideal place to investigate crustal heterogeneities and rifting. Interferometric Synthetic Aperture Radar (InSAR) has been us

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9

Hall, Jennifer Lynn. "Processes leading to the formation of tectonic features on the Moon and Mars." Thesis, Massachusetts Institute of Technology, 1985. http://hdl.handle.net/1721.1/54305.

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Thesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences, 1985.<br>Microfiche copy available in Archives and Science.<br>Vita.<br>Bibliography: leaves 283-306.<br>by Jennifer Lynn Hall.<br>Ph.D.

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10

Matzel, Jennifer E. Piontek 1973. "Rates of tectonic and magmatic processes in the North Cascades continental magmatic arc." Thesis, Massachusetts Institute of Technology, 2004. http://hdl.handle.net/1721.1/30292.

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Thesis (Ph. D.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences, 2004.<br>Includes bibliographical references.<br>Continental magmatic arcs are among the most dynamic. geologic systems, and documentation of the magmatic, thermal, and tectonic evolution of arcs is essential for understanding the processes of magma generation, ascent and crustal growth. The primary goal of this research is to determine rates of tectonic and magmatic processes in the mid to deep crustal levels of the crystalline core of the Cretaceous North Cascades arc. This region was

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11

Sacek, Victor. "Modelagem numérica conjunta de processos sedimentares e tectônicos em bacias sedimentares." Universidade de São Paulo, 2011. http://www.teses.usp.br/teses/disponiveis/14/14132/tde-21062013-151844/.

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O principal objetivo deste trabalho é prever a evolução de margens divergentes desde o início da extensão litosférica, levando-se em consideração a interação entre processos superficiais e tectônicos. Para isto, foi desenvolvido um modelo numérico que acopla isostasia flexural, efeitos térmicos, estiramento litosférico e processos superficiais. A isostasia flexural é simulada através de uma placa elástica fina sobre um fluido invíscido, representando o comportamento flexural da litosfera flutuando sobre a astenosfera. Durante a simulação, a estrutura térmica da litosfera evolui como um resulta

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12

Bicudo, Tacio Cordeiro. "Estudo da formação da bacia hidrográfica do rio Amazonas através da modelagem numérica de processos tectônicos e sedimentares." Universidade de São Paulo, 2017. http://www.teses.usp.br/teses/disponiveis/14/14132/tde-04062018-143103/.

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A bacia hidrográfica do rio Amazonas abrange uma área de 6 × 106 km2 da região norte da América do Sul. O seu canal mais longo, com quase 7.000 km tem origem nos Andes peruanos e cruza todo o continente até chegar na foz, no Atlântico Equatorial. Apesar dos diversos esforços científicos, os processos que guiaram a evolução da paisagem na Amazônia ainda são discutidos, assim como a data do estabelecimento dessa grande bacia hidrográfica que culminou com a forma¸cao do rio Amazonas como um rio transcontinental. O presente trabalho teve como objetivo estudar como se deu a evolução da paisagem na

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13

Kumerics, Christine Maria. "Contribution of tectonic processes to the exhumation of the Cycladic blueschist unit, Greece and Turkey." [S.l.] : [s.n.], 2005. http://deposit.ddb.de/cgi-bin/dokserv?idn=975910949.

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14

Rehak, Katrin. "Pliocene-Pleistocene landscape evolution in south-central Chile : interactions between tectonic, geomorphic, and climatic processes." Phd thesis, Universität Potsdam, 2008. http://opus.kobv.de/ubp/volltexte/2008/1979/.

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Landscapes evolve in a complex interplay between climate and tectonics. Thus, the geomorphic characteristics of a landscape can only be understood if both, climatic and tectonic signals of past and ongoing processes can be identified. In order to evaluate the impact of both forcing factors it is crucial to quantify the evolution of geomorphic markers in natural environments. The Cenozoic Andes are an ideal setting to evaluate tectonic and climatic aspects of landscape evolution at different time and length scales in different natural compartments. The Andean Cordillera constitutes the type su

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15

Maksymowicz, Jeria Andrei. "Physical characterization of the processes of accretion and tectonic erosion at the chilean continental wedge." Tesis, Universidad de Chile, 2014. http://repositorio.uchile.cl/handle/2250/131092.

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Doctor en Ciencias, Mención Geología<br>El presente trabajo de tesis aborda la caracterización cuantitativa de parámetros físicos relacionados a la tectónica de la cuña continental Chilena, con objeto de estudiar las variaciones del estado dinámico del margen en función de las inhomogeneidades presentes tanto en la placa oceánica como en la cuña continental. En una primera etapa, se estudia el impacto de la subducción del centro de expansión de la Dorsal de Chile al sur del punto tripla Nazca-Antártica-Sudamérica (CTJ). En base a un modelo de inversión 2-D obtenido a lo largo de un perfil sísm

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16

Richardson, Stephen Edwin Jonathan. "Tectonic, climatic, and sedimentary processes recorded by Pleistocene fold growth strata, the South Caspian Basin, Azerbaijan." Thesis, Durham University, 2012. http://etheses.dur.ac.uk/5905/.

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The Pleistocene – Present-day sedimentary succession of the South Caspian Basin was deposited syntectonically alongside growing anticlines in an under-filled, rapidly subsiding basin. The combination of ample sediment supply from surrounding mountain belts, fast sedimentation rates (variously estimated at between 0.4 and 1.7 m/kyr) and high accommodation space has resulted in an exceptionally thick succession (up to 3000 m) which documents structural growth and regional tectonics at a high temporal resolution. The succession additionally records the palaeo-water level history of the Caspian Se

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17

Ballato, Paolo. "Tectonic and climatic forcing in orogenic processes : the foreland basin point of view, Alborz mountains, N Iran." Phd thesis, Universität Potsdam, 2009. http://opus.kobv.de/ubp/volltexte/2010/4106/.

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Systeme von Vorlandbecken repräsentieren bedeutende geologische Archive und dienen dem Verständnis von Rückkopplungen zwischen oberflächennahen und tektonischen Prozessen. Außerdem dokumentieren sie die Entwicklung unmittelbar angrenzender Bergketten. Die sedimentären Abfolgen in Vorlandbecken reflektieren das Gleichgewicht zwischen tektonischer Subsidenz, der Bildung langzeitlichen Akkommodationsraumes und des Sedimenteintrages, welcher wiederum die Wirksamkeit von Erosions- und Massenneuverteilungsprozessen wiederspiegelt. Um die Effekte von Klima und Tektonik in einem solchen System zu erfo

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18

Williams, Clare Margaret. "Oceanic lithosphere magnetization marine magnetic investigations of crustal accretion and tectonic processes in mid-ocean ridge environments /." Thesis, Massachusetts Institute of Technology, 2007. http://hdl.handle.net/1912/2031.

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Thesis (Ph. D.)--Massachusetts Institute of Technology and Woods Hole Oceanographic Institution, 2007.<br>"Joint Program in Oceanography/Applied Ocean Science and Engineering"--Cover. Title from Web page (viewed on Mar. 24, 2008). "September 2007". Includes bibliographical references.

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19

Partin, Camille Ann. "On the evolution of atmosphere-ocean oxygenation and plate tectonic processes as recorded in Paleoproterozoic sedimentary basins." Elsevier, 2013. http://hdl.handle.net/1993/22727.

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Important geochemical and tectonic events in the Paleoproterozoic Era lay the foundation for the status and operation of the modern Earth, including the initial rise of atmospheric oxygen paving the path for animal evolution, and the emergence of modern plate tectonic processes leading to the amalgamation of the Canadian Shield (Laurentia). Rudimentary geological and geochronological documentation of Paleoproterozoic sedimentary basins is the foundation from which we can ask larger questions about geochemical changes or plate tectonic events on the evolving Earth, since those questions are lar

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20

Allen, Rosemary. "Relationship of thermal evolution to tectonic processes in a proterozoic fold belt : Halls Creek Mobile Zone, East Kimberley, West Australia /." Title page, contents and introduction only, 1986. http://web4.library.adelaide.edu.au/theses/09PH/09pha4288.pdf.

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21

Booth, Matthew Graham. "Field-based evidence of sedimentary and tectonic processes related to continental collision : the Early Cenozoic basins of Central Eastern Turkey." Thesis, University of Edinburgh, 2013. http://hdl.handle.net/1842/7603.

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Turkey is widely accepted to have formed from a collage of microcontinents that rifted from the northern margin of Gondwana and assembled from the Mesozoic to Mid Cenozoic in response to the closure, collision and suturing of numerous oceanic strands in the Eastern Mediterranean. Sedimentary-tectonic basins, which formed during ocean basin closure, can yield important information about the evolution, timing and processes related to the closure of these oceanic strands. The Darende Basin and the adjacent Hekimhan Basin are two sedimentary-tectonic basins which developed during the collision and

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22

Wilks, Matthew. "A seismological investigation into tectonic, magmatic and hydrothermal processes at Aluto and Corbetti, two restless volcanoes in the Main Ethiopian Rift." Thesis, University of Bristol, 2016. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.702874.

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23

Kurfeß, Daniel. "Crustal uplift and subsidence due to the interaction between tectonic and surface processes an integrated 3D numerical approach for spatial quantification /." [S.l. : s.n.], 2008. http://digbib.ubka.uni-karlsruhe.de/volltexte/1000009996.

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24

Ozacar, Atilla Arda. "Complex Rupture Processes Of Large Strike-Slip Earthquakes And Receiver Function Analysis Of Crust And Upper Mantle In Active Tectonic Settings." Diss., The University of Arizona, 2007. http://hdl.handle.net/10150/194258.

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This dissertation explores the uses for data collected at broadband seismic stations to investigate source process of large strike-slip earthquakes and crust and upper mantle structure within active continental tectonic settings. First, we analyzed rupture mechanism of the 2002 Denali earthquake (M = 7.9) and the 2001 Kunlun earthquake (M = 7.8) using teleseismic P waveforms. According to our results, the Denali earthquake began with initial thrusting and later ruptured a 300-km-long segment with a right-lateral strike-slip mechanism. In contrast, the Kunlun earthquake nucleated along an exten

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25

Wilkinson, Maxwell. "The use of Terrestrial Laser Scanning in characterizing active tectonic processes from postseismic slip to the long term growth of normal faults." Thesis, Durham University, 2012. http://etheses.dur.ac.uk/5573/.

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This thesis investigates two main hypotheses regarding uncertainty in the measurement of paleoseismic offsets used to estimate fault activity and paleoearthquake magnitudes on normal faults: (1) That variations in fault geometry have a significant effect on throw-rates and fault offsets; and (2) that postseismic deformation can be a significant component of the total fault slip for moderate magnitude earthquakes. These hypotheses are tested using high resolution terrestrial laser scan datasets of normal fault topographic offsets and surface ruptures. The first hypothesis is addressed by studyi

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26

Jefferies, Sharon P. "Microstructural and geochemical processes in long-lived reactivated crustal-scale fault zones : a case study from the Median Tectonic Line, SW Japan." Thesis, Durham University, 2006. http://etheses.dur.ac.uk/2582/.

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The Median Tectonic Line (MTL) is a major, crustal-scale fault in Japan that separates the low-P/high-T Ryoke metamorphic belt of mainly subduction related granitoids from the high-P/low-T Sambagawa Belt of accretionary complex metasedimentary rocks. Like many large, crustal-scale faults, the MTL has a long history of movement having been active predominantly as a strike-slip fault since the mid-Cretaceous. Fault rock exposures in the core of the MTL preserve a history of deformation at a range of mid- to shallow-crustal depths. Ryoke mylonites 1-5 km north of the main contact record deeper le

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27

Weiß, Benedikt Johannes [Verfasser], and Christian [Akademischer Betreuer] Hübscher. "The tectonic evolution of the southeastern Terceira Rift/São Miguel region (Azores) and associated submarine volcanic & sedimentary processes / Benedikt Johannes Weiß. Betreuer: Christian Hübscher." Hamburg : Staats- und Universitätsbibliothek Hamburg, 2016. http://d-nb.info/1084213176/34.

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28

Weiß, Benedikt Johannes Verfasser], and Christian [Akademischer Betreuer] [Hübscher. "The tectonic evolution of the southeastern Terceira Rift/São Miguel region (Azores) and associated submarine volcanic & sedimentary processes / Benedikt Johannes Weiß. Betreuer: Christian Hübscher." Hamburg : Staats- und Universitätsbibliothek Hamburg, 2016. http://nbn-resolving.de/urn:nbn:de:gbv:18-77509.

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29

Hogan, John Patrick. "Mineralogical, chemical and isotopic diversity in plutonic rock suites from the Coastal Maine Magmatic Province:the role of source region heterogeneity, tectonic setting and magmatic processes." Diss., Virginia Tech, 1990. http://hdl.handle.net/10919/39074.

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This dissertation represents an investigation of the mid-Paleozoic tectono-thermal and kinematic evolution of the crust in eastern coastal Maine as recorded by the plutonic rocks of this region. The first chapter describes the plutonic rocks of the Coastal Maine Magmatic Province. A tectonic model is developed in which late Ordovician-Silurian bimodal magmatism is interpreted to reflect crustal melting as a result of intraplating of mantle melts at high crustal levels during a period of tension. Large scale melting of lower crustal source regions, represented by voluminous intrusion of Devoni

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30

Morter, Bethany Kathleen. "Understanding the history of a volcanic arc: linking geochemistry of Cenozoic volcanic cobbles from the Wrangell arc, Alaska, to upper plate and subducting slab tectonic processes." Thesis, Kansas State University, 2017. http://hdl.handle.net/2097/38164.

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Master of Science<br>Department of Geology<br>Matthew E. Brueseke<br>The Wrangell arc (WA) is a ~29 Ma magmatic belt, extending from south-central Alaska into the Yukon Territory, that lies above the edges and leading front of the Yakutat microplate, a buoyant oceanic plateau that is causing shallow subduction (11-16º) in the region. The WA occurs in a transition zone between “normal” Aleutian subduction to the west and dextral strike-slip tectonics to the east, accomplished by the Totschunda, Denali, and Duke River faults. This geologic setting offers a chance to study the interrelations betw

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31

Hogan, John Patrick. "Mineralogical, chemical and isotopic diversity in plutonic rock suites from the Coastal Maine Magmatic Province : the role of source region heterogeneity, tectonic setting and magmatic processes /." This resource online, 1990. http://scholar.lib.vt.edu/theses/available/etd-08082007-114045/.

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32

Baese, Rauno [Verfasser]. "Fluid-rock interaction processes during subduction and exhumation of oceanic crust: Constraints from jadeitites in serpentinites, eclogite veins in blueschists and tectonic breccias formed during uplift / Rauno Baese." Kiel : Universitätsbibliothek Kiel, 2013. http://d-nb.info/1030604762/34.

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33

Dannowski, Anke [Verfasser]. "Processes of magmatic and tectonic accretion of oceanic lithosphere at mid-ocean ridges : constraints from a seismic refraction study at the Mid-Atlantic Ridge near 21.5° N / Anke Dannowski." Kiel : Universitätsbibliothek Kiel, 2009. http://d-nb.info/1019867175/34.

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34

Kühn, Rebecca [Verfasser], Bernd [Akademischer Betreuer] Leiss, Jonas [Gutachter] Kley, and Michael [Gutachter] Stipp. "Advanced synchrotron texture analysis of phyllosilicate-rich rocks from different tectonic settings – Understanding texture-forming processes and anisotropic physical properties / Rebecca Kühn ; Gutachter: Jonas Kley, Michael Stipp ; Betreuer: Bernd Leiss." Göttingen : Niedersächsische Staats- und Universitätsbibliothek Göttingen, 2019. http://d-nb.info/1200209133/34.

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35

Steinmann, Lena Verfasser], Volkhard [Akademischer Betreuer] [Gutachter] Spiess, and Sebastian [Gutachter] [Krastel. "Reconstruction of volcano-tectonic processes in interplay with sedimentary deposition in the Gulf of Naples (Italy) using a seismoacoustic dataset / Lena Steinmann ; Gutachter: Volkhard Spiess, Sebastian Krastel ; Betreuer: Volkhard Spiess." Bremen : Staats- und Universitätsbibliothek Bremen, 2016. http://d-nb.info/1116600129/34.

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36

Le, Saout Morgane. "Interaction dorsale-point chaud : relations entre les processus tectoniques et magmatiques à l'axe de la dorsale Est Pacifique, 16°N." Thesis, Brest, 2015. http://www.theses.fr/2015BRES0019/document.

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Le segment 16°N de la dorsale Est-Pacifique (EPR) est le plus large et le moins profond de cette dorsale rapide. Cette morphologie atypique est liée à un apport magmatique accru sous la dorsale dû à la proximité du point chaud des Mathématiciens. Ce travail présente une étude morphostructurale et de chronologie relative détaillée de la zone axiale de ce segment, réalisée à partir de l’analyse de données bathymétriques à 40 m, 10 m et 1 m de résolution, combinée à l’analyse de photos et vidéos de plongées Nautile acquises lors de la campagne PARISUB (PAnache Ridge SUBmersible.). Cette étude per

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37

Ni, Xinghua. "Late Paleozoic - Early Mesozoic tectonic evolution of the southwestern Central Asian Orogenic Belt : structural, metamorphic and magmatic evidence from the eastern Tianshan." Electronic Thesis or Diss., Orléans, 2024. http://www.theses.fr/2024ORLE1043.

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Les orogènes d'accrétion formées le long de marges convergentes se caractérisent par une longue évolution et sont les principaux sites de croissance continentale sur la Terre. Les phénomènes de convergence dans les orogènes d'accrétion impliquent des processus tectoniques complexes, tels que la subduction et le retrait de slabs, l'accrétion arc-arc/continent, et l'extension post-collisionnelle. Cependant, les processus orogéniques des anciennes orogènes sont plus compliqués en raison de l'importante érosion, nécessitant de connaissances approfondies sur la déformation, le métamorphisme et le m

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38

Palamenghi, Luisa [Verfasser], Volkhard [Akademischer Betreuer] Spiess, and Till [Akademischer Betreuer] Hanebuth. "Tectonic and Sea Level Control on the Transport and Depositional Processes in a Siliciclastic Sedimentary Basin. Insights from the Ganges-Brahmaputra Delta, Bengal Basin, Bangladesh / Luisa Palamenghi. Gutachter: Volkhard Spiess ; Till Hanebuth. Betreuer: Volkhard Spiess." Bremen : Staats- und Universitätsbibliothek Bremen, 2012. http://d-nb.info/1072046326/34.

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39

Becker, Katharina [Verfasser], Charlotte M. [Akademischer Betreuer] Krawczyk, Dieter [Akademischer Betreuer] Franke, Charlotte M. [Gutachter] Krawczyk, Frank [Gutachter] Börner, and Dieter [Gutachter] Franke. "The crustal structure and evolution of the South Atlantic : a marine geophysical study with focus on tectonic and magmatic processes / Katharina Becker ; Gutachter: Charlotte, M. Krawczyk; Frank Börner; Dieter Franke ; Charlotte, M. Krawczyk; Dieter Franke." Berlin : Technische Universität Berlin, 2016. http://d-nb.info/1156333997/34.

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40

Blacic, Tanya Marie. "Magma supply and storage in volcanic systems : shallow crustal emplacement processes and causes of the large axial high along the western Galápagos Spreading Center, and relation of earthquakes to tectonic and magmatic features near Lassen Peak, northern California /." For electronic version search Digital dissertations database. Restricted to UC campuses. Access is free to UC campus dissertations, 2005. http://uclibs.org/PID/11984.

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41

Tuckwell, George William. "Models of structural processes at oceanic plate boundaries." Thesis, University of Southampton, 1997. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.243170.

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42

LLUCH, DIDIER. "Les unites a materiel sedimentaire supra-"schistes lustres" de saint florent et de macinaggio (corse du nord)." Toulouse 3, 1989. http://www.theses.fr/1989TOU30029.

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Les unites tectoniques a materiel sedimentaire exempt de metamorphisme alpin de la corse du nord sont considerees, soit d'origine interne par rapport au domaine ophiolitique ligure, soit d'origine interne. Les leves cartographiques ont permis de mettre en evidence differentes sous-unites dont le materiel est issu d'autant de zones paleogeographiques distinctes. Les donnees structurales permettent de distinguer trois phases de deformation: ante-eocene distensive, eocene ou oligocene cisaillante, post-nappes

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43

Гоптарьова, Н. В. "Геолого-фізичні чинники деформаційних процесів породних масивів і експлуатаційних колон свердловин нафтогазових родовищ внутрішньої зони Передкарпатського прогину". Thesis, Івано-Франківський національний технічний університет нафти і газу, 2003. http://elar.nung.edu.ua/handle/123456789/3980.

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Дисертація присвячена вивченню геолого-фізичних чинників, що впливають на деформаційні процеси породних масивів та на технічний стан експлуатаційних колон свердловин нафтогазових родовищ Внутрішньої зони Передкарпатського прогину. За результатами геолого-промислового матеріалу побудовано карти-схеми геотехногенної порушеності родовищ і визначено зони активізації деформаційних процесів, які відрізняються інтенсивністю проявів тектонічних рухів та деформацій осадових товщ. Побудовано графічні та встановлено аналітичні залежності зміни пористості гірських порід від зміни пластового тиску. Встанов

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44

Landes, Bruno. "Les unités briançonnaises de la bordure orientale du massif de la Vanoise méridionale (Savoie) : évolution sédimentaire et structurale." Grenoble 1, 1988. http://www.theses.fr/1988GRE10031.

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L'etude stratigraphique et structurale a permis de distinguer 5 unites superposees depuis le socle jusqu'a la nappe des schistes lustres et 3 phases de deformations synschisteuses suivies d'une phase de bombement et de fracturation du massif

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45

MacManus, Sean Christopher. "Architectural Tectonics: A Shift Between the Cultural Tradition of Making to Contemporary Building Processes." Thesis, Virginia Tech, 2014. http://hdl.handle.net/10919/25235.

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Modern architecture has lost its sense of place by the adoption of practices like standardization and universal modularity, over the focus and influence of unique local building practices. However, looking outside of the cultural main stream works of architecture, there exists some built structures with such purity around how they were constructed and a form of honesty deeply embedded within their material usage. Having been idealized in such a locally specific manner, these attributes become the essence of belonging that ties the building to its particular place. In this thesis, I have cons

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46

Charbonnier, Guillaume. "Reconstitution paléoclimatique et paléoenvironnementale au Valanginien (~135 Ma, Crétacé inférieur) : vers une meilleure compréhension des processus locaux versus globaux." Phd thesis, Université Paris Sud - Paris XI, 2013. http://tel.archives-ouvertes.fr/tel-00956584.

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L'étage Valanginien est caractérisé dans le registre sédimentaire par une excursion positive des isotopes du carbone (amplitude 1,5-2‰), appelée " Episode Weissert ". Cet événement coïncide avec des changements paléoenvironnementaux et paléoclimatiques majeurs. La formation de la province volcanique ignée du Paraná-Etendeka a été proposée comme principal facteur forçant contrôlant ces changements. Cependant, de récentes études démontrent que l'Episode Weissert précède systématiquement l'activité volcanique. Ainsi, les facteurs déclenchant qui contrôlent ces changements sont encore source de dé

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47

Engelder, Todd. "Investigating the Coupling Between Tectonics, Climate and Sedimentary Basin Development." Diss., The University of Arizona, 2012. http://hdl.handle.net/10150/217092.

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Sedimentary deposits have been broadly used to constrain past climate change and tectonic histories within mountain belts. This dissertation summarizes three studies that evaluate the effects of climate change and tectonics on sedimentary basin development. (1) The paleoslope estimation method, a method for calculating the threshold slope of a fluvial deposit, does not account for the stochastic variations in water depth in alluvial channels caused by climatic and autogenic processes. Therefore, we test the robustness of applying the paleoslope estimation method in a tectonic context. Based on

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48

Kim, Sangmyung David. "Spreading-rate Dependent Mid-ocean Ridge Processes Expressed in Western Atlantic Lithosphere." Diss., Georgia Institute of Technology, 2006. http://hdl.handle.net/1853/11472.

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The Far-Offset Active-Source Imaging of Mantle (FAIM) experiment was conducted along an 800-km-long transect in the Western Atlantic to study the evolution of 108-157 m.y. lithosphere. The main transect (Line 1) crosses a transition from slow (13-14 mm/yr in half rate) to ultra-slow (~8 mm/yr) paleo spreading rates, and thus represents an ideal setting to study spreading-rate dependent processes as expressed in preserved lithospheric structure. This thesis presents results of four analysis efforts along this transect. We present a crustal model based on seismic refraction and wide-angle tra

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49

Moore, Nicole E. DeBari Susan M. "Origin and geochemical evolution of mafic magmas from Mount Baker in the northern Cascade arc, Washington : probes into mantle and crustal processes /." Online version, 2010. http://content.wwu.edu/cdm4/item_viewer.php?CISOROOT=/theses&CISOPTR=345&CISOBOX=1&REC=14.

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Stanionis, Arminas. "Žemės plutos horizantaliųjų judesių Ignalinos atominės elektrinės rajone tyrimas geodeziniais metodais." Doctoral thesis, Lithuanian Academic Libraries Network (LABT), 2006. http://vddb.library.lt/obj/LT-eLABa-0001:E.02~2005~D_20060117_125618-84276.

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A method prepared and created algorithm for computations and evaluation of relation between Earth’s crust horizontal deformations and variations of tectonic stresses. Hooke’s law was used for relation description. Method of evaluation of Earth’s crust horizontal deformations was improved as well as modelling method based on observation data. Elements of deformation tensors were evaluated by applying finite element method. New data of Earth’s crust horizontal movements and their geodynamic interpretation at the Ignalina Nuclear Power Plant region were obtained.

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