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Structural geology and tectonics /McClay, K. R. January 2000 (has links) (PDF)
Thesis (D.Sc.)--University of Adelaide, Dept. of Geology and Geophysics, 2000. / Includes bibliographical references.
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Surficial mapping and kinematic modeling of the St. Clair thrust fault, Monroe County, West VirginiaSturms, Jason M. January 2008 (has links)
Thesis (M.S.)--West Virginia University, 2008. / Title from document title page. Document formatted into pages; contains vii, 84 p. : ill. (some col.), maps (some col.). Includes abstract. Includes bibliographical references (p. 75-78).
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Structural geology and tectonics / by Kenneth Ronald McClay.McClay, K. R. (Kenneth R.) January 2000 (has links)
Includes bibliographical references. / 1 v. (various pagings) : / Title page, contents and abstract only. The complete thesis in print form is available from the University Library. / Consists of 75 published papers on structural geology and tectonics grouped into 5 broad themes -- and ore deposits; analogue modelling; extensional tectonics; thrust tectonics; and, tectonics, all presented in chronological order within the group. / Thesis (D.Sc.)--University of Adelaide, Dept. of Geology and Geophysics, 2000
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Structural geology and dislocation modeling of the East Coyote anticline, eastern Los Angles basin /Myers, Daniel J. January 1900 (has links)
Thesis (M.S.)--Oregon State University, 2002. / Typescript (photocopy). Includes bibliographical references (leaves 42-44). Also available via the World Wide Web.
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Structure and crustal balance of the Herald Arch and Hope Basin in the Chukchi Sea, AlaskaPatthoff, D. Alex. January 2008 (has links)
Thesis (M.S.)--West Virginia University, 2008. / Title from document title page. Document formatted into pages; contains vii, 106 p. : ill. (some col.), col. maps. Includes abstract. Includes bibliographical references (p. 100-103).
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The Appalachian fold and thrust belt, northwestern Newfoundland /Grenier, Robert, January 1990 (has links)
Thesis (M.Sc.) -- Memorial University of Newfoundland. / Typescript. Bibliography: leaves 137-147. Also available online.
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Development of a dilatant damage zone along a thrust relay in a low-porosity quartz areniteCook, Jennie E., January 2005 (has links) (PDF)
Thesis (M.S.) -- University of Tennessee, Knoxville, 2005. / Title from title page screen (viewed on Feb. 6, 2006). Thesis advisor: William M. Dunne. Vita. Includes bibliographical references.
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Can growth strata identify individual paleoearthquakes and characterize fold kinematics? : a case study from the La Laja fault system, Sierra de Villicum, Argentina /Schultz, Emily S. January 1900 (has links)
Thesis (M.S.)--Oregon State University, 2007. / Printout. Includes bibliographical references (leaves 67-71). Also available on the World Wide Web.
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Characterising and predicting fracture patterns in a sandstone fold-and-thrust beltWatkins, Hannah E. January 2015 (has links)
Fracture distribution in a fold and thrust belt is commonly thought to vary depending on structural position, strain, lithology and mechanical stratigraphy. The distribution, geometry, orientation, intensity, connectivity and fill of fractures in a reservoir are all important influences on fractured reservoir quality. The presence of fractures is particularly beneficial in reservoirs that contain little matrix porosity or permeability, for example tight sandstones. In these examples fractures provide essential secondary porosity and permeability that enhance reservoir production. To predict how reservoir quality may fluctuate spatially, it is important to understand how fracture attributes may vary, and what controls them. This research aims to investigate the influence of structural position on fracture attribute variations. Detailed fracture data collection is undertaken on folded sandstone outcrops. 2D forward modelling and 3D model restorations are used to predict strain distribution in the fold-and-thrust belt. Relationships between fracture attributes and predicted strain are determined. Discrete Fracture Network (DFN) modelling is then undertaken to predict fracture attribute variations. DFN modelling results are compared with field fracture data to determine how well fractured reservoir quality can be predicted. Field data suggests strain is a major controlling factor on fracture formation. Fractures become more organised and predictable as strain increases. For example in high strain forelimb regions, fracture intensity and connectivity are high, and fracture orientations are consistent. In lower strain regions, fracture attributes are much more variable and unpredictable. Fracture variations often do not correspond to strain fluctuations, and correlations can be seen between fracture intensity and lithology. Reservoir quality is likely to be much more variable in low strain regions than high strain regions. DFN modelling is also challenging because fracture attribute variations in low strain regions do not correspond to strain, and therefore cannot be predicted.
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Structures and metamorphism of Ptarmigan Creek area, Selwyn Range, B.C.Forest, Richard C. January 1985 (has links)
No description available.
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