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Dissertations / Theses on the topic 'Basin (Geology)'

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Published: 4 June 2021

Last updated: 1 February 2022

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1

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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2

Aspler, Lawrence B. (Lawrence Bernard) Carleton University Dissertation Geology. "Geology of Nonacho Basin (early Proterozoic) N.W.T." Ottawa, 1985.

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3

Hawkes, Martin. "Surficial geology of the Boston basin, Ma." Thesis, Massachusetts Institute of Technology, 1987. http://hdl.handle.net/1721.1/14816.

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4

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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5

Mohamed, Abdalla Yagoub. "Basin analysis and hydrocarbon maturation, Unity and Kaikang area, Muglad Basin, Sudan." Thesis, University of Aberdeen, 1996. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.390934.

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Basin analysis study has been conducted along a cross section in the Unity-Kaikang area, Muglad Basin, Sudan. The research is based essentially on geological, seismic investigations and basin model approach. The basin model approach included two dimensional gravity modelling, and one dimensional thermal history, maturation and hydrocarbon generation modelling. In addition an investigation of the hydrocarbon migration processes, routes to the known and probable accumulation targets is studied. The basin models were calibrated against data obtained from wells drilled in the area. The seismic inv

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6

Cloke, Ian Richard. "Structural controls on basin evolution in the Kutai Basin and Mekassar Straits." Thesis, Royal Holloway, University of London, 1997. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.285157.

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The Kutai basin is an inverted extensional basin located onshore Borneo, to the west of the Makassar Straits. Basin initiation had occurred by the middle Eocene and was contemporaneous with oblique oceanic spreading in the Makassar Straits. Field studies, geophysical data and computer modelling elucidate the structural evolution of the rift basin. Vein sets, C-S fabrics and chevron folds were studied in the lurassicCretaceous basement and NW-SE and NE-SW trending fractures were reactivated during the Tertiary controlling the basin architecture. Seismic profiles across both the northern and sou

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7

Huson, Sarah Ann. "Structural study of the southwest part of Elk Basin Anticline, Bighorn Basin, Wyoming." Virtual Press, 2002. http://liblink.bsu.edu/uhtbin/catkey/1236575.

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A subsurface and surface structural study was completed in the southwest part of the Elk Basin Anticline, Wyoming. The goals of this study were to better improve preexisting geologic surface maps of the area and to better understand subsurface structural relationships. A normal fault with a splay to the north was recorded through sections 25, 26. and 35 of T58N, RI00W. Using well logs to create across section, this fault was traced in the subsurface. Strike and dip measurements in undisturbed areas of the anticline averaged 332° (azimuth) or N28W (quadrant). In an area of anomalous strike (sec

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8

Mohapatra, Gopal Krishna 1968. "Faulting and basin geometry beneath the Great Salt Lake: implications for basin evolution and cenozoic extension." Diss., The University of Arizona, 1996. http://hdl.handle.net/10150/565551.

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9

Hamlin, Herbert Scott. "Syn-orogenic slope and basin depositional systems, Ozona sandstone, Val Verde Basin, southwest Texas /." Digital version accessible at:, 1999. http://wwwlib.umi.com/cr/utexas/main.

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10

Fothergill, Patrick Allen. "Late Tertiary and Quaternary intermontane basin evolution in north-east Tibet : the Guide Basin." Thesis, Royal Holloway, University of London, 1998. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.299105.

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11

Ward, Emily M. Geraghty. "Development of the Rocky Mountain foreland basin combined structural, mineralogical, and geochemical analysis of basin evolution, Rocky Mountain thrust front, northwest Montana /." CONNECT TO THIS TITLE ONLINE, 2007. http://etd.lib.umt.edu/theses/available/etd-09262007-094800/.

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12

Tsiftsis, E. V. "Geology and hydrogeology of the Megalopolis Basin, Peloponnese, Greece." Thesis, University of Bristol, 1987. http://hdl.handle.net/1983/df43eab5-19cd-42e5-a740-e850188d2474.

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13

Smith, Stuart A. "The phanerozoic basin-fill history of the Roebuck Basin /." Title page, abstract and contents only, 1999. http://web4.library.adelaide.edu.au/theses/09PH/09phs6615.pdf.

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14

Cooper, Jennifer Rebecca. "Igneous intrusions and thermal evolution in the Raton Basin, CO-NM contact metamorphism and coal-bed methane generation /." Diss., Columbia, Mo. : University of Missouri-Columbia, 2006. http://hdl.handle.net/10355/4606.

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Thesis (M.S.)--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 (February 6, 2007) Includes bibliographical references.

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15

Collier, Richard E. Ll. "Sedimentary facies evolution in Continental fault-bounded basins formed by crustal extension : the Corinth Basin, Greece." Thesis, University of Leeds, 1988. http://etheses.whiterose.ac.uk/2616/.

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Characteristic half-graben and graben geometries are generated by extensional tectonics. The sedimentary infill to such basins reflects their structural evolution. The actively extending basins of central Greece have provided an opportunity to study the mechanisms that control sediment distribution and the resultant facies patterns and geometries produced in such environments. The modern and precedent Neogene to Quaternary sediments studied, and their controlling processes, provide predictive templates for the analysis of controls acting upon ancient extensional basin fills. On a basinwide sca

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16

Marquez, C. Xiomara M. (Marquez Ceballos). "Reservoir geology of upper Devonian Leduc buildups, deep Alberta basin." Thesis, McGill University, 1994. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=28487.

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Upper Devonian (Frasnian) stromatoporoid and coral buildups in the Alberta Basin are among the most important hydrocarbon reservoirs in Western Canada. In the deep basin ($>$4000 m), Strachan, Ricinus West and adjacent buildups have similar depositional facies, but have experienced different diagenetic processes that affected their reservoir characteristics. The most important diagenetic alteration is dolomitization that partially to completely replaced the original limestone buildups. Replacement dolomitization occurred at shallow depths near 500 m, indicated by petrographic and geologic rela

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17

Smith, Claire Juliet. "The Upper Lias of the Hebrides Basin." Thesis, University of Oxford, 1996. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.362086.

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18

Traynor, John-Joe. "Arenig sedimentation and basin evolution in Wales." Thesis, University of Cambridge, 1988. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.306613.

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19

Cowan, M. T. "Integrated geological, geophysical and remotely sensed data in the basin analysis of the Rathlin Basin, the north of Ireland." Thesis, Queen's University Belfast, 2002. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.246449.

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20

Guthrie, Kristin M. "Structural controls on extensional-basin development triassic Ischigualasto Formation, NW Argentina." Connect to this document online, 2005. http://rave.ohiolink.edu/etdc/view?acc%5Fnum=miami1123266742.

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Thesis (M.S.)--Miami University, Dept. of Geology, 2005.<br>Title from first page of PDF document. Document formatted into pages; contains [1], iv, 38 p. : ill. Includes bibliographical references (p. 35-38).

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21

Ward, Emily Geraghty. "DEVELOPMENT OF THE ROCKY MOUNTAIN FORELAND BASIN: COMBINED STRUCTURAL, MINERALOGICAL, AND GEOCHEMICAL ANALYSIS OF BASIN EVOLUTION, ROCKY MOUNTAIN THRUST FRONT, NORTHWEST MONTANA." The University of Montana, 2007. http://etd.lib.umt.edu/theses/available/etd-09262007-094800/.

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The sub-Middle Jurassic unconformity exhumed at Swift Reservoir, in the Rocky Mountain thrust belt of Montana, exposes structures that call for a re-evaluation of the deformation history at this locale. The unconformity separates Late Mississippian Madison Group carbonate (~340 Ma) from the transgressive basal sandstone of the Middle Jurassic (Bajocian-Bathonian) Sawtooth Formation (~170 Ma). Fieldwork established that northwest-trending, karst-widened fractures (grikes) are filled with cherty, phosphatic sandstone and conglomerate of the Sawtooth Formation and penetrate the Madison Group for

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22

Muehlberg, Jessica M. "Geology of the Tahoe City sub-basin, Lake Tahoe, California-Nevada." abstract and full text PDF (free order & download UNR users only), 2007. http://0-gateway.proquest.com.innopac.library.unr.edu/openurl?url_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:dissertation&res_dat=xri:pqdiss&rft_dat=xri:pqdiss:1442871.

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23

Ko, Jaehong. "Illitesmectite diagenesis in the Beaufort-Mackenzie Basin, Arctic Canada." Thesis, McGill University, 1992. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=39337.

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Illitization in the Beaufort-Mackenzie Basin is characterized by random, a mixture of random and ordered, R1-ordered, and R $>$ 1-ordered illite/smectite (I/S). Proportions of I-layers increase with depth, while the dominant I/S type changes in that order. Illitization in offshore wells is generally more advanced than onshore because of higher geothermal gradients. Illitization in geopressure zones and sandy intervals appears to be faster than under normally pressured conditions and in shales, respectively, due to higher water/particle ratios. Hydrocarbons generally occur above and in the inte

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24

McCullagh, Timothy. "Investigating the controls on production from a basin-centered gas accumulation: lower cretaceous cadotte member, Deep Basin Alberta." Thesis, McGill University, 2008. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=18668.

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This thesis examines the controls on gas production from a Cretaceous sandstone deposit located within the Deep Basin of Alberta, Canada. By integrating core, wireline log, 3-D seismic, petrophysical, pressure and production data, we show that the best production comes from permeable chert-rich shoreface and beachface sandstones separated laterally and cyclically by tighter quartzose sandstones. The physical properties of the two lithologies are sufficiently different that they can be distinguished seismically; a map of seismic amplitudes for the Cadotte shows curvilinear high-amplitude anom

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25

May, Geoffrey. "Oligocene to recent evolution of the Calama Basin, northern Chile." Thesis, University of Aberdeen, 1997. http://digitool.abdn.ac.uk:80/webclient/DeliveryManager?pid=191900.

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The Calama and eastern Pampa del Tamarugal Basins are located between 22°S and 23°S within the forearc of northern Chile. They are filled by sediments deposited in alluvial braidplain, fluvial, playa sandflat, lacustrine and volcaniclastic environments under a semi-arid to hyper-arid climate. The nature of the alluvial braidplain depositional environment is unusual in that it combines elements of both alluvial fan and fluvial depositional systems, in contradiction to recently published models of alluvial fan sedimentation. Detailed sedimentary logging, magnetostratigraphy and dating of 14 volc

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26

Pak, Ŭn-ju. "Cenozoic geohistory of the southwestern margin of the Ulleung basin, East Sea." [S.l. : s.n.], 1986. http://catalog.hathitrust.org/api/volumes/oclc/53229626.html.

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27

Johnson, David Alan. "Comparative studies of iron-oxide mineralization: Great Basin." Diss., The University of Arizona, 2000. http://hdl.handle.net/10150/289188.

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The study of iron-oxide-rich mineralization in the Great Basin demonstrates that these occurrences are widespread and are associated with a wide range of host rocks and associated igneous suites. Two well-exposed areas containing similar types of iron-oxide±(Cu-Co-REE) mineralization and voluminous sodium-rich hydrothermal alteration are hosted by contrasting coeval, mid-Jurassic igneous suites and demonstrate a complex, but similar hydrothermal system evolution. One area is hosted by mafic plutonic and volcanic rocks of the Humboldt mafic complex in west-central Nevada. The second area is hos

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28

Pirrie, D. "Sedimentology of the Marambio Group, Larsen Basin, Antarctica." Thesis, Open University, 1989. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.327776.

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29

Tricker, Paul Michael. "Organic maturation in the Lower Palaeozoic Welsh Basin." Thesis, University of Southampton, 1991. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.358811.

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30

Lake, S. D. "The structure and evolution of the Wessex Basin." Thesis, Durham University, 1985. http://etheses.dur.ac.uk/1215/.

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The subsidence form of many sedimentary basins consist of two discrete phases of basin development: a rapid subsidence phase related to riftinq of the crust and thinninq of the sub-crustal lithosphere followed by a thermal or flexural subsidence phase. In marked contrast to this simple models prediction, some basins exhibit a complicated subsidence history consisting of one or more phases of extension and thermal recovery (construction phase). These phases may in turn be followed by phases of destruction (inversion) which could introduce an additional drivinq subsidence. The Wessex Basin is su

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31

Denley, Martyn R. "Carbonate platform to basin transitions." Thesis, University of East Anglia, 1988. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.235490.

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32

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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33

Currie, Brian Scott 1966. "Jurassic-Cretaceous evolution of the central Cordilleran foreland-basin system." Diss., The University of Arizona, 1998. http://hdl.handle.net/10150/282582.

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During Jurassic and Cretaceous time deposition in the western interior basin was controlled by a combination of subduction-related dynamic subsidence and thrust-generated flexural subsidence. Changes in the angle of oceanic plate subduction along the western margin of North America and thrust deformation in the Cordillera governed the spatial and temporal influences of these mechanisms throughout basin history. Dynamic subsidence was the primary control on basin deposition during Early-Middle Jurassic and Late Cretaceous time. During these periods, shallow-angle oceanic plate subduction beneat

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34

Terrinha, Pedro Antonio Gancedo. "Structural geology and tectonic evolution of the Algarve Basin, South Portugal." Thesis, Imperial College London, 1998. http://hdl.handle.net/10044/1/7544.

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35

Gigandet, Katherine M. "Processing and Interpretation of Illinois Basin Seismic Reflection Data." Wright State University / OhioLINK, 2014. http://rave.ohiolink.edu/etdc/view?acc_num=wright1401309913.

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36

Mriheel, Ibrahim Youssef. "Basin modelling of the Gabes-Tripoli basin and geology of the Farwah Group reservoirs, Western Offshore, Libya." Thesis, University of Manchester, 2000. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.496686.

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The Gabes-Tripoli Basin (G-T Basin) is a Mesozoic-Cenozoic basin which was initiated as a result of widespread, late Triassic-Middle Jurassic extensional movements that developed over a broad zone of strain between the African and European plates. The basin formation is probably related to strike slip movement between the western Libyan Coastal Fault System and the north margin of the basin. The basin rifting phase of lithospheric extension lasted as much as 40my. The dominant driving mechanism of subsidence seems clearly to have been subsidence due to cooling following lithospheric thinning a

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37

Walker, David T. "Cyclic sedimentation in the Pliensbachian of the Wessex Basin." Thesis, University of Reading, 1991. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.306041.

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38

Apps, Gillian Margaret. "The evolution of the Gres d'Annot Basin, S.W. Alps." Thesis, University of Liverpool, 1987. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.316126.

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39

Newall, Mark John. "Forward and reverse modelling of extensional sedimentary basin formation." Thesis, University of Liverpool, 1991. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.317249.

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40

Glover, Brian William. "The sedimentology and basin evolution of the Grampian Group." Thesis, Keele University, 1989. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.279007.

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41

Reyes, Maria Ines Jacome. "The formation of the Monagas Foreland Basin : Eastern Venezuela." Thesis, University of Liverpool, 2001. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.367521.

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42

McCune, Julian Glenn. "Cenozoic sedimentary evolution of the Helmville Basin, west-central Montana." CONNECT TO THIS TITLE ONLINE, 2008. http://etd.lib.umt.edu/theses/available/etd-05282008-101831/.

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43

Elrick, Maya. "Development of cyclic ramp-to-basin carbonate deposits, lower Mississippian, Wyoming and Montana." Diss., This resource online, 1990. http://scholar.lib.vt.edu/theses/available/etd-09092008-063649/.

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44

Cannon, Michael P. "Cenozoic kinematics of the Little Pine fault, Santa Maria Basin, California." Thesis, California State University, Long Beach, 2014. http://pqdtopen.proquest.com/#viewpdf?dispub=1527534.

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<p> The Little Pine fault (LPF) delineates the northeast margin of the Santa Maria Basin. The basin is inverting due to north-northeast, south-southwest shortening, associated with vertical-axis rotation of the western Transverse Ranges to the south. Slip data collected along the Little Pine fault yielded principle compressive stress directions that are indicative of reverse slip, with minor lateral components that vary along strike of the fault. Slip data collected to the northwest along the Foxen Canyon fault is indicative of right lateral strike-slip. Mapped offsets near Coralles, Happy, an

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45

Savard, Martine. "Calcite cements in carbonates of the Sverdrup Basin, Canadian Arctic Archipelago." Thesis, University of Ottawa (Canada), 1991. http://hdl.handle.net/10393/7459.

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Calcite cements from the Upper Paleozoic sequences 2, 3 and 4 of the Sverdrup Basin (Canadian Arctic Archipelago) are the subject of this study. On a micro-scale, petrography with light microscopy, cathodoluminescence (CL), scanning electron microscopy (SEM) and staining helped to identify two main textural groups of cements, neomorphic and primary. Both are, in turn, subdivided into two categories: calcitized aragonite and recrystallized high-magnesium calcite for the former, and meteoric calcite and burial (late) calcite, for the latter. In neomorphic cements, eleven micro-scale CL eleven pa

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46

Craigie, Neil William. "Chemostratigraphy of Middle Devonian lacustrine sediments in the Orcadian Basin, north-east Scotland." Thesis, University of Aberdeen, 1998. http://digitool.abdn.ac.uk:80/webclient/DeliveryManager?pid=88106.

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During Middle Devonian times, lacustrine deposition dominated much of NE Scotland including Caithness, Orkney, Shetland and the Inner Moray Firth. Donovan classified such deposits into five distinct facies associations:- the deep water facies association A and the progressively shallower water facies associations B, C, D and sandstones. Such facies associations occur in climatically induced cycles. Facies A sediments (known as "fish beds") are organic rich, comprising triplets of carbonate, clastic and organic laminae (each triplet is c. 1.5mm thick). In the present study the fish beds have be

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47

Othman, Rushdy School of Biological Earth &amp Environmental Sciences UNSW. "Petroleum geology of the Gunnedah-Bowen-Surat Basins, Northern New South Wales : stratigraphy, organic petrology and organic geochemistry." Awarded by:University of New South Wales. School of Biological, Earth and Environmental Sciences, 2003. http://handle.unsw.edu.au/1959.4/20537.

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The three-dimensional thermal maturity pattern has been investigated and the hydrocarbon generation potential assessed for the Permian and Triassic sequences of the southern Bowen and northern Gunnedah Basins and the lower part of the overlying Jurassic Cretaceous Surat Basin sequence in northern New South Wales. An oil-source rock correlation also has been investigated in the Gunnedah Basin. Vitrinite reflectance measurements were conducted on 256 samples from 28 boreholes. A total of 50 of these samples were subjected to Rock-Eval pyrolysis analysis, and 28 samples extracted for additional o

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48

Elswick, Virginia L. "Seismic interpretation and structural evaluation of the Hope Basin, Alaska." Morgantown, W. Va. : [West Virginia University Libraries], 2003. http://etd.wvu.edu/templates/showETD.cfm?recnum=3014.

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Thesis (M.S.)--West Virginia University, 2003.<br>Title from document title page. Document formatted into pages; contains vi, 21, [24] p. : ill. (some col.), maps (some col.). Includes abstract. Includes bibliographical references (p. 20-21).

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49

Davisson, Cole M. "Stratigraphic and structural evolution of the early Diligencia Basin, Orocopia Mountains, Southeastern California." Thesis, This resource online, 1993. http://scholar.lib.vt.edu/theses/available/etd-04072010-020140/.

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50

Jones, David John. "Triassic basin sedimentation in the United Kingdom and North Sea." Thesis, Royal Holloway, University of London, 1991. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.243529.

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