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Dissertations / Theses on the topic 'Structural Geology Geology'

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Published: 4 June 2021

Last updated: 1 February 2022

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1

McClay, K. R. "Structural geology and tectonics /." Title page, contents and abstract only, 2000. http://web4.library.adelaide.edu.au/theses/09SD/09sdm126.pdf.

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2

Kiani, Tayebeh. "Modeling for geospatial database : application to structural geology data : application to structural geology data." Paris 6, 2010. http://www.theses.fr/2010PA066057.

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L’objectif de cette étude est de créer un modèle de base de données dans un système d’information géographique afin d’archiver, analyser, présenter et de diffuser des données observées lors des analyses de géologie structurale. Le modèle de données est conçu pour atteindre quatre objectifs: établir un vocabulaire partagé par les spécialistes, modéliser les concepts de géologie structurale, produire des cartes dérivées des cartes géologiques d’Iran et fonctionner avec un logiciel de système d’information géographique. Un ensemble de classes conceptuelles est alors identifié pour représenter les

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3

Lisle, Richard John. "Techniques of quantitative structural geology." Thesis, University of Birmingham, 2007. https://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.446367.

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4

Metzger, Nicolai. "Structural controls on the shear zone hosted, IOCG-style Kiskamavaara Cu-Co-Au mineralization." Thesis, Luleå tekniska universitet, Institutionen för samhällsbyggnad och naturresurser, 2019. http://urn.kb.se/resolve?urn=urn:nbn:se:ltu:diva-74068.

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Sweden is the largest producer of iron ore in the European Union, as well as amongst the top producers for base and precious metals. Much of its mineral wealth derives from northern Norrbotten, type locality of the Kiruna-type-magnetite-apatite ores. Besides the massive iron ore bodies, the region is further recognized as important iron-oxide-copper-gold (IOCG) province, with the world class, Aitik Cu-Au-Ag-(Mo) deposit as its most prominent example (1061 Mt with 0,22% Cu; 0,15ppm Au; 1.3ppm Ag), (Wanhainen et al. 2012, Boliden 2017). The close spatial relation between Aitik, further IOCG styl

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5

Bauer, Tobias. "Structural and sedimentological reconstruction of the inverted Vargfors basin : a base for 4D-modelling." Licentiate thesis, Luleå tekniska universitet, Geovetenskap och miljöteknik, 2010. http://urn.kb.se/resolve?urn=urn:nbn:se:ltu:diva-17596.

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The Palaeoproterozoic Skellefte mining district in northern Sweden covers an area of 120 by 30 km and is one of the most important mining districts in Europe, producing mainly Zn, Cu, Pb, As and Au from volcanogenic massive sulfide (VMS) and orogenic gold deposits.Detailed mapping of structures and stratigraphy within the sedimentary Vargfors Group combined with a structural analysis revealed a syn-extensional fault pattern of NW-SE-trending normal faults and associated NE-SW-trending transfer faults, creating the segmented sedimentary Vargfors basin. It comprises distinct fault-bound compartm

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6

Andersson, Joel. "Structural evolution of two ore-bearing Palaeoproterozoic metasupracrustal belts in the Kiruna area, Northwestern Fennoscandian Shield." Licentiate thesis, Luleå tekniska universitet, Geovetenskap och miljöteknik, 2019. http://urn.kb.se/resolve?urn=urn:nbn:se:ltu:diva-72034.

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In this project, two key study areas in the northwestern Fennoscandian Shield are under investigation. The “Western supracrustal belt” and “Central Kiruna area” are both located along lithotectonically comparable Rhyacian-Orosirian metasupracrustal belts and both areas are characterized by iron oxide-apatite (IOA) and iron oxide-copper-gold (IOCG)-style mineralizations and related hydrothermal alterations. The area is in general well studied but the structural evolution remains unresolved. In order to build a structural framework for the Kiruna area, the number of deformation events, kinematic

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7

Jonsson, Linus. "Seismic tomography as an instrument for structural evaluation in the Printzsköld and Alliansen ore bodies, Malmberget." Thesis, Luleå tekniska universitet, Institutionen för samhällsbyggnad och naturresurser, 2017. http://urn.kb.se/resolve?urn=urn:nbn:se:ltu:diva-64918.

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The Malmberget deposit is one of the major apatite iron ores in Europe, located in northern Norrbotten. As the mining in Malmberget proceeds deeper more challenges with the stability have been faced. When the stress distribution of a rock mass exceeds the rock strength energy in form of seismic waves is released. In Malmberget, a monitoring system consisting of 200 geophones is installed which detects all seismic waves in the area. Based on data received from the monitoring system, LKAB has achieved to generate a seismic tomography model over the velocity variations of the seismic waves as the

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8

Miller, John Frederick. "Structural geology of the Ohio Shale." Connect to resource, 1996. http://rave.ohiolink.edu/etdc/view?acc%5Fnum=osu1163610177.

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9

Kampmann, Tobias Christoph. "3D structural framework and constraints on the timing of hydrothermal alteration and ore formation at the Falun Zn-Pb-Cu-(Au-Ag) sulphide deposit, Bergslagen, Sweden." Licentiate thesis, Luleå tekniska universitet, Geovetenskap och miljöteknik, 2015. http://urn.kb.se/resolve?urn=urn:nbn:se:ltu:diva-26483.

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The Falun pyritic Zn-Pb-Cu-(Au-Ag) sulphide deposit, situated in the Palaeoproterozoic (1.9–1.8 Ga) Bergslagen lithotectonic unit in the south-western part of the Fennoscandian Shield, is one of the major base and minor precious metal sulphide deposits in Sweden. Host rocks to the deposit as well as the ores and altered rocks were metamorphosed and affected by heterogeneous ductile strain during the Svecokarelian orogeny the total duration of which was 2.0–1.8 Ga. These processes both reworked the mineral assemblages of the original hydrothermal alteration system and reshaped the structural ge

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10

Ferreira, Samuel Nunes [UNESP]. "Geologia estrutural aplicada às rochas ornamentais na Pedreira Knawa, Cláudio (MG)." Universidade Estadual Paulista (UNESP), 2004. http://hdl.handle.net/11449/92887.

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11

Silva, Carlos Humberto da [UNESP]. "Evolução geológica da faixa Brasília na região de Tapira, Sudoeste de Minas Gerais." Universidade Estadual Paulista (UNESP), 2006. http://hdl.handle.net/11449/103025.

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Made available in DSpace on 2014-06-11T19:32:21Z (GMT). No. of bitstreams: 0 Previous issue date: 2006-10-14Bitstream added on 2014-06-13T19:42:56Z : No. of bitstreams: 1 silva_ch_dr_rcla.pdf: 785091 bytes, checksum: 6e1bc5d4c82f715e1777e80217b4a4b6 (MD5)<br>Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)<br>O presente trabalho apresenta uma proposta de evolução geológica Neoproterozóica de um segmento da Faixa Brasília Meridional, na região de Tapira (SW de Minas Gerais). A partir de mapeamento geológico detalhado é da caracterização estrutural e metamórfica. As rochas desta r

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12

Massucatto, Armando José [UNESP]. "Caracterização estrutural do embasamento do Grupo Araí, na zona externa da faixa Brasília (GO)." Universidade Estadual Paulista (UNESP), 2003. http://hdl.handle.net/11449/103016.

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Made available in DSpace on 2014-06-11T19:32:21Z (GMT). No. of bitstreams: 0 Previous issue date: 2003-02-25Bitstream added on 2014-06-13T20:43:23Z : No. of bitstreams: 1 massucatto_aj_dr_rcla.pdf: 7707531 bytes, checksum: 674b102878234ea9505b57b68ec0de3e (MD5)<br>Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)<br>A área de estudo, objeto desta tese de doutoramento, situa-se na porção nordeste do estado de Goiás, na região de Cavalcante. Nesta região são encontradas rochas do embasamento da Faixa de Dobramentos Brasília, composto por rochas do Complexo Granítico-gnáissico, mega

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13

Zahid, Khandaker Uddin Ashraf. "Provenance and basin tectonics of Oligocene-Miocene sequences of the Bengal Basin, Bangladesh." Auburn, Ala., 2005. http://repo.lib.auburn.edu/2005%20Fall/Thesis/ZAHID_KHANDAKER_14.pdf.

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14

Tang, Lai-kwan Denise. "Geology of Tuen Mun Area, NW Hong Kong an updated model /." Click to view the E-thesis via HKUTO, 2007. http://sunzi.lib.hku.hk/hkuto/record/B3829283X.

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15

Copfer, Torrey J. "Geology of the Deseret Peak East 7.5' Quadrangle, Tooele County, Utah, and Impacts for Hydrology of the Region." DigitalCommons@USU, 2003. https://digitalcommons.usu.edu/etd/6723.

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Detailed geologic mapping of the Deseret Peak East 7.5' Quadrangle yields new interpretations regarding the stratigraphy of the Oquirrh Basin, fault and fold geometry, and structural evolution of the region. The Stansbury Range consists of the north-southtrending Deseret anticline. Basal Mississippian units rest unconformably on Cambrian beds in the central part of the range. Paleozoic uplift, Mesozoic contraction, and Cenozoic extension have created a series of broad folds, large thrust faults, and several normal faults. The area is dominated by bedrock springs, with the presence of abundant

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16

White, Thomas West Steltenpohl Mark G. "Geology of the 1:24,000 Tallassee, Alabama, Quadrangle, and its implications for southern Appalachian tectonics." Auburn, Ala, 2008. http://repo.lib.auburn.edu/EtdRoot/2008/SPRING/Geology_and_Geography/Thesis/White_Thomas_41.pdf.

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17

Tozer, Craig Hampton. "The influence of inherited structures on the Cenozoic orogeny of the Kyrgyz Tien Shan /." view abstract or download file of text, 2004. http://wwwlib.umi.com/cr/uoregon/fullcit?p3147837.

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Thesis (Ph. D.)--University of Oregon, 2004.<br>Typescript. Includes vita and abstract. Includes bibliographical references (leaves 171-180). Also available for download via the World Wide Web; free to University of Oregon users.

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18

Al-Kotbah, Ahmed Mohammed Abdullah. "Structural geology of South Hadhramaut area Yemen Republic." Thesis, University of Glasgow, 1996. http://theses.gla.ac.uk/1460/.

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The northern margin of the Gulf of Aden has a long history of extension from the Cambrian to the present. The dominant structures are related to Oligo-Miocene rifting in the early stages of development of the Gulf of Aden and they overprint Palaeozoic and Mesozoic structures. An area of 170 km by 50 km was mapped at scale of 1:50,000. Landsat images of the whole area, at 1:50,000 and 1:100,000 and air photographs of part of the area were used as base maps. The resulting maps are the first detailed geological maps to be made for this area and are a major outcome of this research. Precambrian ba

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19

Kazadi, Banza Samuel-Barry. "Structural geology of the Kinsevere Copper Deposit, DRC." Diss., University of Pretoria, 2012. http://hdl.handle.net/2263/24753.

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The Kinsevere mine is a copper deposit located in the Democratic Republic of Congo (DRC), within the Central African Copperbelt. This area is situated in the Katangan basin within the SE portion of the Lufilian Arc, which is a large, arcuate structure that extends from SE Angola, across the DRC, and into NW Zambia. The purpose of this study is to characterise the brittle deformation observed around the Kinsevere copper deposit to lead to an understanding of the deformation history of the area. This is accomplished by analysing fault-slip and fold data to help understand the relationship betwee

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20

Gleason, James Donald. "Paleozoic tectonics and sediment sources of the Ouachita fold belt, Arkansas-Oklahoma and West Texas: An isotopic and trace element geochemical study." Diss., The University of Arizona, 1994. http://hdl.handle.net/10150/186844.

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Ordovician through Pennsylvanian strata of the Ouachita and Marathon sedimentary sequences show correlated Nd-Sr isotopic relations, Th/Sc ratios and REE patterns typical of evolved upper crustal sources, indicating that the 2000 km long Ouachita-Marathon fold belt consists primarily of recycled crustal materials. wi thin this sequence, Nd isotopes distinguish three distinct provenance groups: 1) Lower to Middle Ordovician hemipelagites and quartzose turbidites with ε(Nd)(t) = -13 to -16 (T(DM) = 1.8 to 2.1 Ga); 2) Upper Ordovician through Pennsylvanian hemipelagites and quartzolithic turbidit

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21

Henry, Heather Marie. "Investigation of a triangle zone structure between Augusta and Bowman's Corners, Lewis and Clark County, Montana." CONNECT TO THIS TITLE ONLINE, 2007. http://etd.lib.umt.edu/theses/available/etd-05212007-104742/.

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22

Elliot, Henry K. "Fractures in the region of the Rocky Hill anticline, Rocky Hill, Connecticut : a structural geological study /." View abstract, 2001. http://library.ccsu.edu/ccsu%5Ftheses/showit.php3?id=1644.

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Thesis (M.S.)--Central Connecticut State University, 2001.<br>Thesis advisor: Charles W. Dimmick. " ... in partial fulfillment of the requirements for the degree of Master of Science in Physics and Earth Sciences." Includes bibliographical references (leaves 60-64). Also available via the World Wide Web.

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23

Bradway, Michael David. "Stratigraphy and structural geometry at the leading edge of the Montana Thrust Belt, east of Sun River Canyon, Lewis and Clark and Teton Counties, Montana." CONNECT TO THIS TITLE ONLINE, 2007. http://etd.lib.umt.edu/theses/available/etd-05072007-163806/.

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24

Andrade, Frederico Guilherme Guaraldo de [UNESP]. "Lineações minerais em porfiroblastos." Universidade Estadual Paulista (UNESP), 2006. http://hdl.handle.net/11449/92881.

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Made available in DSpace on 2014-06-11T19:26:13Z (GMT). No. of bitstreams: 0 Previous issue date: 2006-12-14Bitstream added on 2014-06-13T20:14:56Z : No. of bitstreams: 1 andrade_fgg_me_rcla.pdf: 1229975 bytes, checksum: 09b1fccb568d0ad941d82c61d3c81d9f (MD5)<br>Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)<br>O estudo de lineações minerais tem fundamental importância na compreensão da evolução tectônica de cinturões orogênicos. Entretanto, em áreas polideformadas, enquanto as orientações das lineações mais novas podem ser resgatadas, as lineações antigas tendem a ser

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25

Nogueira, Johnson Fernandes [UNESP]. "Estrutura, geocronologia e alojamento dos batólitos de Quixadá, Quixeramobim e Senandor Pompeu - Ceará central." Universidade Estadual Paulista (UNESP), 2004. http://hdl.handle.net/11449/103013.

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Made available in DSpace on 2014-06-11T19:32:21Z (GMT). No. of bitstreams: 0 Previous issue date: 2004-05-21Bitstream added on 2014-06-13T19:42:55Z : No. of bitstreams: 1 nogueira_jf_dr_rcla_prot.pdf: 5154714 bytes, checksum: 9c2ffc2d884cd3adbed2a96a48ec0737 (MD5)<br>Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)<br>O Ceará Central caracteriza-se pela ocorrência de uma rede de zonas de cisalhamento preferencialmente orientada na direção NE-SW e/ou NNE-SSW. Associados espacialmente a estas zonas de cisalhamento ocorrem rochas intrusivas de dimensões variadas. Entre estas

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26

Silva, Carlos Humberto da. "Evolução geológica da faixa Brasília na região de Tapira, Sudoeste de Minas Gerais /." Rio Claro : [s.n.], 2003. http://hdl.handle.net/11449/103025.

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Orientador: Luiz Sérgio Amarante Simões<br>Banca: Rudolph Allard Johannes Trouw<br>Banca: Cláudio de Morrisson Valeriano<br>Banca: Hildor José Seer<br>Banca: Hans Dirk Ebert<br>Resumo: O presente trabalho apresenta uma proposta de evolução geológica Neoproterozóica de um segmento da Faixa Brasília Meridional, na região de Tapira (SW de Minas Gerais). A partir de mapeamento geológico detalhado é da caracterização estrutural e metamórfica. As rochas desta região apresentam uma complexa evolução estrutural, onde a principal estrutura reconhecida é uma foliação em baixo ângulo (S4) orientada em mé

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27

Andrade, Frederico Guilherme Guaraldo de. "Lineações minerais em porfiroblastos /." Rio Claro : [s.n.], 2006. http://hdl.handle.net/11449/92881.

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Orientador: Luiz Sérgio Amarante Simões<br>Banca: Rudolph Allard Johannes Trouw<br>Banca: Antenor Zanardo<br>Resumo: O estudo de lineações minerais tem fundamental importância na compreensão da evolução tectônica de cinturões orogênicos. Entretanto, em áreas polideformadas, enquanto as orientações das lineações mais novas podem ser resgatadas, as lineações antigas tendem a ser obliteradas pela superposição dos eventos deformacionais mais novos. Esta dissertação lança uma nova metodologia para o resgate da orientação de lineações minerais inclusas em porfiroblastos, utilizando a Platina Univers

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28

Ferreira, Samuel Nunes. "Geologia estrutural aplicada às rochas ornamentais na Pedreira Knawa, Cláudio (MG) /." Rio Claro : [s.n.], 2004. http://hdl.handle.net/11449/92887.

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Resumo: Este trabalho apresenta os resultados de mapeamento geológico-estrutural de detalhe numa área piloto (Pedreira Knawa, Cláudio Estado de Minas Gerais) em escala de 1:200 e dos estudos de reconhecimento geológico em suas áreas adjacentes, e da aplicação do método de GPR na identificação de estruturas geológicas na Pedreira Knawa. Onde seu objetivo principal é proporcionar um direcionamento dos trabalhos geológico-estruturais na pedreira, visando otimizar a extração da rocha. As rochas que compõem esta região abrangem tanto rochas do complexo gnáissico-migmatítico de médio a alto grau den

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29

Massucatto, Armando José. "Caracterização estrutural do embasamento do Grupo Araí, na zona externa da faixa Brasília (GO) /." Rio Claro : [s.n.], 2003. http://hdl.handle.net/11449/103016.

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Orientador: Luiz Sergio Amarante Simões<br>Banca: Nilson Francisquini Botelho<br>Banca: Marco Antonio Fonseca<br>Banca: Norberto Morales<br>Banca: Hans Dirk Ebert<br>Resumo: A área de estudo, objeto desta tese de doutoramento, situa-se na porção nordeste do estado de Goiás, na região de Cavalcante. Nesta região são encontradas rochas do embasamento da Faixa de Dobramentos Brasília, composto por rochas do Complexo Granítico-gnáissico, mega veios de quartzo e Formação Ticunzal. Recobrindo estas rochas são visíveis os metassedimentos do Grupo Araí. As rochas do embasamento da Faixa de Dobramentos

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30

Thompson, Stephen C. "Active tectonics in the central Tien Shan, Kyrgyz Republic /." Thesis, Connect to this title online; UW restricted, 2001. http://hdl.handle.net/1773/6744.

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Burgette, Reed Joel. "Uplift in response to tectonic convergence : the Kyrgyz Tien Shan and Cascadia subduction zone /." Connect to title online (ProQuest), 2008. http://proquest.umi.com/pqdweb?did=1616709721&sid=1&Fmt=2&clientId=11238&RQT=309&VName=PQD.

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Thesis (Ph. D.)--University of Oregon, 2008.<br>Typescript. Includes vita and abstract. Includes bibliographical references (leaves 225-242). Also available online in ProQuest, free to University of Oregon users.

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Rodriguez-Roa, Fernando Antonio. "Thrust belt architecture of the central and southern Western Foothills of Taiwan." Thesis, [College Station, Tex. : Texas A&M University, 2007. http://hdl.handle.net/1969.1/ETD-TAMU-1523.

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Kronsell, Ida. "Structural control on the Peña del Seo tungsten-greisen vein deposit, northwest Spain." Thesis, Luleå tekniska universitet, Institutionen för samhällsbyggnad och naturresurser, 2019. http://urn.kb.se/resolve?urn=urn:nbn:se:ltu:diva-76402.

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Tungsten is listed on the European Commission list of critical raw materials that are crucial to Europe’s economy. By raising awareness of tungsten as a critical raw material the EU can prioritise to enhance exploration, mining and recycling of tungsten. In this thesis the structural relationship between wall rock and veins, in a greisen-tungsten vein deposit, were analysed with the intention to interpret how tectonic deformation events control the emplacement of tungsten-bearing veins. The objective of this thesis is to investigate if and how structures controlled hydrothermal fluid flow and

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34

Armstrong, Thomas Robert. "Structural and Petrologic Evolution of Acadian Dome Structures in Southern Vermont." Diss., Virginia Tech, 1995. http://hdl.handle.net/10919/37857.

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Petrologic and thermobarometric studies, coupled with geologic mapping and structural analysis, provide critical evaluation of several different models for Acadian (Late Silurian to Middle Devonian) dome evolution in southern Vermont. Previous models considered diapiric uprise and composite nappe-stage crustal thickening and subsequent diapirism as likely causes of dome formation. Both of these previous models result in symmetrical distribution of P-T values about the dome structures with corresponding coreward increases in temperature, and typically, coreward decrease in associated pressures.

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Drover, David Howard. "Regional and detailed structural geology of the Quirk Creek structure, S.W. Alberta." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 2000. http://www.collectionscanada.ca/obj/s4/f2/dsk1/tape4/PQDD_0017/MQ55203.pdf.

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Crowley, James L. Carleton University Dissertation Earth Sciences. "U-Pb geochronology in Frenchman Cap dome of the Monashee complex, southern Canadian Cordillera; early Tertiary tectonic overprint of a Proterozoic history." Ottawa, 1997.

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Hansman, Reuben. "Constraining the Uplift History of the Al Hajar Mountains, Oman." Licentiate thesis, Stockholms universitet, Institutionen för geologiska vetenskaper, 2016. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-133409.

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Mountain building is the result of large compressional forces in the Earth’s crust where two tectonic plates collide. This is why mountains only form at plate boundaries, of which the Al Hajar Mountains in Oman and the United Arab Emirates is thought to be an example of. These mountains have formed near the Arabian–Eurasian convergent plate boundary where continental collision began by 30 Ma at the earliest. However, the time at which the Al Hajar Mountains developed is less well constrained. Therefore, the timing of both the growth of the mountains, and the Arabian–Eurasian collision, needs t

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Nushart, Nathan. "Modeling Intrusive Geometries of a Shallow Crustal Intrusion: New Evidence From Mount Ellsworth, Utah." Scholar Commons, 2015. http://scholarcommons.usf.edu/etd/5753.

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Surface displacements resulting from upper-crustal intrusion of melt are a paramount concern for communities and facilities located in or near active volcanic areas (e.g. Campi Flegrei, Yucca Mtn.). Study of active intrusions such as Campi Flegrei, Italy west of Mt. Vesuvius, is limited to remote observations through geophysical/geodetic procedures. While the surface displacement due to melt emplacement at depth can easily be determined, the geometries and depth of intrusions are often based on simplified assumptions (e.g. spheres and prolate or oblate ellipsoids). These models benefit from d

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Seiler, Christina. "Structural and thermal evolution of the Gulf Extensional Province in Baja California, Mexico : implications for Neogene rifting and opening of the Gulf of California /." Connect to thesis, 2009. http://repository.unimelb.edu.au/10187/4212.

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Feinstein, Michael Nicholas. "Contributions to the geology of the Cuenca de Oro." To access this resource online via ProQuest Dissertations and Theses @ UTEP, 2007. http://0-proquest.umi.com.lib.utep.edu/login?COPT=REJTPTU0YmImSU5UPTAmVkVSPTI=&clientId=2515.

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41

Lee, Cho-min. "The tectonic framework of Hong Kong and vicinity and its relationship to regional seismicity /." [Hong Kong] : University of Hong Kong, 1990. http://sunzi.lib.hku.hk/hkuto/record.jsp?B13122368.

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42

Green, George Meredith 1964 Carleton University Dissertation Geology. "Detailed sedimentology of the Bowser Lake group, northern Bowser basin, north-central British Columbia." Ottawa.:, 1992.

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43

Neves, Mirna Aparecida [UNESP]. "Evolução cenozóica da região de Jundiaí (SP)." Universidade Estadual Paulista (UNESP), 1999. http://hdl.handle.net/11449/92935.

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Made available in DSpace on 2014-06-11T19:26:15Z (GMT). No. of bitstreams: 0 Previous issue date: 1999-06-18Bitstream added on 2014-06-13T19:13:17Z : No. of bitstreams: 1 neves_ma_me_rcla.pdf: 8679642 bytes, checksum: 5c01ef629bc53f21298ec0cf2a7dc4a5 (MD5)<br>Neste trabalho é apresentado um estudo das relações existentes entre a ocorrência de depósitos sedimentares nos arredores de Jundiaí (SP) e o papel das falhas e fraturas na sua formação, deformação e preservação, objetivando a investigação de alguns eventos sucedidos na evolução cenozóica da região. Os métodos utilizados envolvem a extr

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44

Johnson, Shannon D. "Structural geology of the Usakos Dome in the Damara Belt, Namibia." Thesis, Stellenbosch : Stellenbosch University, 2005. http://hdl.handle.net/10019.1/50457.

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Thesis (MSc)--Stellenbosch University, 2005.<br>ENGLISH ABSTRACT: The northeast-trending south Central Zone (sCZ) of the Pan-African Damara belt in central Namibia is structurally characterized by kilometer-scale, northeast-trending dome structures developed in Neoproterozoic rocks of the Damara Sequence. A number of different structural models have been proposed for the formation of these domes in the literature. This study describes the structural geology of the Usakos dome. The study discusses the structural evolution of the dome within the regional framework of the cSZ that represen

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45

Hayman, Nicholas W. "Structure and petrology of gouge and breccia bearing shallow crustal shear zones of detachment faults in Death Valley, California /." Thesis, Connect to this title online; UW restricted, 2005. http://hdl.handle.net/1773/6699.

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46

Dunham, Rachel E. Crider Juliet G. "Kink band development in the Darrington Phyllite on Samish Island, northwestern Washington /." Online version, 2010. http://content.wwu.edu/cdm4/item_viewer.php?CISOROOT=/theses&CISOPTR=367&CISOBOX=1&REC=14.

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47

Hill, Joseph Christopher. "Structural geology and tectonics of the paleoproterozoic rocks of the Mount Rushmore Quadangle, Black Hills, Souh Dakota." Diss., Columbia, Mo. : University of Missouri-Columbia, 2006. http://hdl.handle.net/10355/4456.

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Thesis (Ph.D.)--University of Missouri-Columbia, 2006.<br>The entire dissertation/thesis text is included in the research.pdf file; the official abstract appears in the short.pdf file (which also appears in the research.pdf); a non-technical general description, or public abstract, appears in the public.pdf file. Title from title screen of research.pdf file viewed on (April 26, 2007) Vita. Includes bibliographical references.

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48

Bayliss, Brian G. Cronin Vincent S. "Test of a method for recognizing unmapped seismogenic faults." Waco, Tex. : Baylor University, 2007. http://hdl.handle.net/2104/5035.

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49

Luo, Hongjun. "Tectonostratigraphy of foreland basins the Upper Cretaceous in southwestern Wyoming /." Laramie, Wyo. : University of Wyoming, 2005. http://proquest.umi.com/pqdweb?did=990280521&sid=1&Fmt=2&clientId=18949&RQT=309&VName=PQD.

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50

Douds, Ashley S. B. "Fractal analysis of topography and structure across the Appalachian foreland of West Virginia." Morgantown, W. Va. : [West Virginia University Libraries], 1998. http://etd.wvu.edu/templates/showETD.cfm?recnum=146.

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Thesis (M.S.)--West Virginia University, 1998.<br>Title from document title page. Document formatted into pages; contains ix, 120, 102, 48, 2, 381, 377 p. : ill., maps (some col.). Includes abstract. Includes bibliographical references (p. 104-106).

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