Дисертації з теми "Geology, Structural Tasmania, Northern"
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Crook, Stephen R. "Structural Geology of the Northern Part of Elkhorn Mountain, Bannock Range, Idaho." DigitalCommons@USU, 1985. https://digitalcommons.usu.edu/etd/6677.
Повний текст джерелаGreen, George Meredith 1964 Carleton University Dissertation Geology. "Detailed sedimentology of the Bowser Lake group, northern Bowser basin, north-central British Columbia." Ottawa.:, 1992.
Знайти повний текст джерелаSigler, Joshua T. "The metamorphic and structural evolution of the Davis Peak area, northern Park Range, Colorado." Laramie, Wyo. : University of Wyoming, 2008. http://proquest.umi.com/pqdweb?did=1798480831&sid=1&Fmt=2&clientId=18949&RQT=309&VName=PQD.
Повний текст джерелаFitz-Gerald, Dudley Braden. "Evidence for an Archean Himalayan-style orogenic event in the northern Teton Range, Wyoming." Laramie, Wyo. : University of Wyoming, 2008. http://proquest.umi.com/pqdweb?did=1798480821&sid=1&Fmt=2&clientId=18949&RQT=309&VName=PQD.
Повний текст джерелаValentino, David W. "Tectonics of the lower Susquehhanna River region, southeastern Pennsylvania and northern Maryland: late proterozoic rifting to late paleozoic dextral transpression." Diss., Virginia Tech, 1993. http://hdl.handle.net/10919/30108.
Повний текст джерелаHuang, Kuan. "Geological studies of igneous rocks and their relationships along the Kyrenia Range, Northern Cyprus." Click to view the E-thesis via HKUTO, 2008. http://sunzi.lib.hku.hk/hkuto/record/b40204030.
Повний текст джерелаVenn, Jonathan Andrew. "Structural and metamorphic evolution of the northern Margin of the Pelvoux Hassif, Hautes Alpes, France." Thesis, University of Bristol, 1992. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.358090.
Повний текст джерелаNguyen, Phung T. "Structural geology and mineralization of the White Devil Mine, Tennant Creek, Northern Territory /." Title page, table of contents and abstract only, 1987. http://web4.library.adelaide.edu.au/thesis/09SB/09sbN576.pdf.
Повний текст джерелаNeves, Douglas Scott. "Footwall Deformation and Structural Analysis of the Footwall of the Willard Thrust Fault, Northern Wasatch Range, Utah." DigitalCommons@USU, 1989. https://digitalcommons.usu.edu/etd/5784.
Повний текст джерелаZhao, Jian-xin. "The geology, geochemistry and geochronology of the Atnarpa Igneous Complex, SE Arunta Inlier, northern Australia : implications for early to middle proterozoic tectonism and crustal evolution." Title page, contents and abstract only, 1989. http://web4.library.adelaide.edu.au/theses/09SM/09smz63.pdf.
Повний текст джерелаBendall, Betina. "Mid-Palaeozoic shear zones in the Strangways Range : a record of intracratonic tectonism in the Arunta Inlier, Central Australia." Title page, contents and introduction only, 2000. http://web4.library.adelaide.edu.au/theses/09PH/09phb458.pdf.
Повний текст джерелаHarbort, Terrence Anthony. "Structure and tectonic synthesis of the Marlborough block, Northern New England fold belt, Australia /." [St. Lucia, Qld.], 2001. http://www.library.uq.edu.au/pdfserve.php?image=thesisabs/absthe19092.pdf.
Повний текст джерелаHarms, Tekla Ann, and Tekla Ann Harms. "STRUCTURAL AND TECTONIC ANALYSIS OF THE SYLVESTER ALLOCHTHON, NORTHERN BRITISH COLUMBIA: IMPLICATIONS FOR PALEOGEOGRAPHY AND ACCRETION." Diss., The University of Arizona, 1986. http://hdl.handle.net/10150/187539.
Повний текст джерелаYeats, Kenneth James, and Kenneth James Yeats. "Geology and structure of the northern Dome Rock Mountains, La Paz County, Arizona." Thesis, The University of Arizona, 1985. http://hdl.handle.net/10150/558016.
Повний текст джерелаHuang, Kuan, and 黃寬. "Geological studies of igneous rocks and their relationships along the Kyrenia Range, Northern Cyprus." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 2008. http://hub.hku.hk/bib/B40204030.
Повний текст джерелаHines, Frederick Michael. "The sedimentation, tectonics and stratigraphy of the cretaceous/tertiary sequence of northwest Santander, northern Spain." Thesis, University of Oxford, 1986. http://ora.ox.ac.uk/objects/uuid:1d1f8c32-9fd3-44a5-ba6a-d963fa9868c0.
Повний текст джерелаKruse, Stefan. "Structural evolution of the northern Thor–Odin Culmination, Monashee Complex southern Canadian Cordillera." Thesis, University of New Brunswick, 2007. http://hdl.handle.net/1882/941.
Повний текст джерелаShunqukela, Tokozani. "A study of the structural geology of an area between the Neusspruit shear zone and the Brakfontein shear zone near Kakamas, Northern Cape." University of the Western Cape, 2014. http://hdl.handle.net/11394/4359.
Повний текст джерелаThe study area Koekoeb B is a farm that falls under the Kakamas Terrane which in turn falls under the Gordonia Subprovince in the Namaqua-Natal Metamorphic Province, South Africa. This area was chosen due to lack in literature about its lithology. Koekoeb B is comprised of metasedimentary rocks of the Biesje Poort Subgroup and granitoids of the Keimoes Suite. The Kakamas Terrane was deposited in an intracratonic basin between the Kaapvaal Craton and the Namaqua continental mass. The sediments were buried with time and experienced metamorphism due to burial pressures and temperatures. The area experienced folding as a result of the collision of the newly formed Kakamas Terrane and the Bushmanland segment with the Kaapvaal Craton during a Wilson Cycle. During subduction and collision the metasedimentary rocks were intruded by what is known as the Keimoes Suite. The most abundant intrusive rock in Koekoeb B is the Friersdale Charnockite. It is considered the youngest with Rb-Sr ages around 1080-1090 Ma. The Gordonia Subprovince experienced such intense deformation that continuous folds formed and there is even evidence of parasitic folds. Northwest striking shear zones developed as a result of the continued compression of the Namaqua mass with the adjacent north easterly Kaapvaal Craton. The folds and shear zones formed under four major deformational events Two months were spent acquiring orientation data (direction of dip and dip) in the field. A Clar compass was used to measure the dip direction and dip readings of bedding, cleavage, joints and lineations. The orientation data was imported into Move® software to create a geological map. Samples collected from the field were used to produce thin sections for petrography studies using the petrographic microscope. Conclusions were drawn from the analysis of the data. Koekoeb B experienced regional metamorphism and folding when the Kakamas Terrane collided with the Kaapvaal Craton. The area was subdivided into four subareas based on the strike and dip data generated on the geological map. The synoptic β-axis diagram determined that the subareas are of the same generation but the fold axes orientations vary slightly. Because the study area did not include the shear zones no conclusive reason can be given but it can be assumed that the variation is due to movement along the shear zone or as a result of the intrusion of the Keimoes Suite. The area later experienced brittle deformation which is evident from the large number of joints found; the joints cut across the folds and show a different stress regime from the folds. Conjugate joints were observed on the field and plotted on stereonets. The results showed a vertical sigma two which confirmed that Koekoeb had been affected not only by compression tectonics but by the strike-slip movement on the shear zone.
Yuan, Tianson. "Seismic studies of the northern Cascadia accretionary prism, sediment consolidation and gas hydrates." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1996. http://www.collectionscanada.ca/obj/s4/f2/dsk3/ftp04/nq21957.pdf.
Повний текст джерелаLoundagin, Nicholas R. "Geophysical Characterization of the Structural Configuration and Tectonic Evolution along the Northern Margin of the Gulf of Mexico Basin, Northwestern Mississippi." Thesis, University of Louisiana at Lafayette, 2019. http://pqdtopen.proquest.com/#viewpdf?dispub=13422120.
Повний текст джерелаThe tectonic history of the Gulf of Mexico Basin in northwestern Mississippi is poorly understood due to a lack of publicly available data and overlying Mesozoic sediments. Using an extensive set of geophysical data including: well data, potential field data, and 2-D seismic data, we define distinct zones of varying structural styles across the region and provide new insight into the tectonic evolution of the northern margin of the Gulf of Mexico.
The cratonal region is defined by the extent of Precambrian basement across the region and is characterized by an orthogonal set of normal faults related to Precambrian – Cambrian rifting and subsidence along the southern Paleozoic shelf margin. The, now, foreland basin is composed primarily of Cambrian-Devonian shelf carbonates and Carboniferous clastics deposited along the southern continental margin, coinciding with the southern limit of Precambrian cratonal material.
Divisible into two structural domains, the Frontal and Allochthonous Domain, the sub-cropping Ouachita orogenic belt is defined by geophysical data in northwestern Mississippi. The Frontal Domain of the Ouachita zone is restricted to the western study area and is characterized by small, imbricate thrusts branching from a lower detachment within autochthonous sediments and an upper detachment along the base of back thrusted Carboniferous sediments. Large thrust sheets of the Allochthonous Domain are correlatable across the study area and are truncated to the north by large intrusions or basement blocks.
The seismically defined limit of the basinal zone corresponds to a linear gravity minima separating Mesozoic rift-related basins to the south from Precambrian and intrusive bodies to the north. Geophysical data of the basinal zone characterize multiple igneous bodies of varying ages. Syn-rift Triassic graben clastics confined to grabens paralleling the basinal zone limit are interpreted to be related to a Mesozoic rift-related transform across Mississippi separating rift basins of the larger region.
Al, Tarawneh Maha Atallah. "Structural setting of the Jordan Northern Highlands : an integrated study using surface and sub-surface geological data by utilizing GIS Technology." Doctoral thesis, University of Cape Town, 2011. http://hdl.handle.net/11427/10001.
Повний текст джерелаEagan, Keith E. "Paleoenvironmental and Stratigraphic Interpretation of the Middle Cambrian Ute Formation, Northern Utah." DigitalCommons@USU, 1996. https://digitalcommons.usu.edu/etd/6791.
Повний текст джерелаMoore-Nall, Anita Louise. "Structural controls and chemical characterization of brecciation and uranium vanadium mineralization in the Northern Bighorn Basin." Thesis, Montana State University, 2017. http://pqdtopen.proquest.com/#viewpdf?dispub=10251316.
Повний текст джерелаThe goals of this research were to determine if the mode of mineralization and the geology of two abandoned uranium and vanadium mining districts that border the Crow Reservation might be a source for contaminants in the Bighorn River and a source of elevated uranium in home water wells on the Reservation. Surface and spring waters of the Crow Reservation have always been greatly respected by the Crow people, valued as a source of life and health and relied upon for drinking water. Upon learning that the Bighorn River has an EPA 303d impaired water listing due to elevated lead and mercury and that mercury has been detected in the fish from rivers of the Crow Reservation this study was implemented. Watersheds from both mining districts contribute to the Bighorn River that flows through the Crow Reservation.
Initial research used the National Uranium Resource Evaluation database to analyze available geochemistry for the study areas using GIS. The data showed elevated concentrations of lead in drainages related to the mining areas. The data also showed elevated uranium in many of the surface waters and wells that were tested as a part of the study on the Crow Reservation. The author attended meetings and presented results of the National Uranium Resource Evaluation data analyses to the Crow Environmental Health Steering Committee. Thus, both uranium and lead were added to the list of elements that were being tested in home water wells as part of a community based participatory research project addressing many issues of water quality on the Crow Reservation. Results from home wells tested on the reservation did show elevated uranium.
Rock samples were collected in the study areas and geochemically analyzed. The results of the analyses support a Permian Phosphoria Formation oil source of metals in the two mining districts. Structural data support fracturing accompanied by tectonic hydrothermal brecciation as a process that introduced oil and brines from the Bighorn Basin into the deposits where the uranium vanadium deposits later formed.
Robinson, Delores Marie, and Delores Marie Robinson. "Structural and neodymium-isotopic evidence for the tectonic evolution of the Himalayan fold-thrust belt, western Nepal and the northern Tibetan Plateau." Diss., The University of Arizona, 2001. http://hdl.handle.net/10150/289761.
Повний текст джерелаLi, Hongyan. "Seismic calibration of northern Eurasia using regional phases from nuclear explosions and 3-D Moho configuration of accreted terranes in western British Columbia." Laramie, Wyo. : University of Wyoming, 2006. http://proquest.umi.com/pqdweb?did=1188873741&sid=3&Fmt=2&clientId=18949&RQT=309&VName=PQD.
Повний текст джерелаDelwiche, Benjamin M. "Oligocene paleotopography and structural evolution of the Pah Rah Range, western Nevada implications for constraining slip on the right-lateral Warm Springs Valley fault in the northern Walker Lane /." 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:1446438.
Повний текст джерелаWinker, Charles David 1952. "Neogene stratigraphy of the Fish Creek-Vallecito section, southern California : implications for early history of the northern Gulf of California and Colorado Delta." Diss., The University of Arizona, 1987. http://hdl.handle.net/10150/191123.
Повний текст джерелаKaenmee, Kwanjai. "Structural Interpretation and Investigation of the Displacement Gradients of the Normal Fault System beneath the Horda Platform, the northern North Sea." Thesis, Norges teknisk-naturvitenskapelige universitet, Institutt for petroleumsteknologi og anvendt geofysikk, 2012. http://urn.kb.se/resolve?urn=urn:nbn:no:ntnu:diva-19211.
Повний текст джерелаAmbrose, Tyler. "Structure, metamorphism, and tectonics of the northern Oman-UAE ophiolite and underlying metamorphic sole." Thesis, University of Oxford, 2017. http://ora.ox.ac.uk/objects/uuid:e9520624-0f91-4c9d-a9b9-e9e2fc5d5517.
Повний текст джерелаYakovlev, Petr V. "Transitions in Structural Styles and Trends within the Northern Appalachian Hudson Valley Fold-Thrust Belt Near Catskill, New York." Thesis, Boston College, 2010. http://hdl.handle.net/2345/1191.
Повний текст джерелаThe Hudson Valley fold-thrust belt (HVB) is a narrow belt of deformed Upper Ordovician to Middle Devonian clastic and carbonate strata exposed in the western Hudson Valley of New York State. Geologic mapping at a scale of 1:10,000 was carried out near the town of Catskill. The southern portion of the map area includes a large doubly-plunging structure which features a fault-dominated southern portion plunging towards 017° and a northern fold-dominated, 206° trending, southerly plunging segment. A relay structure between two major faults or fault systems is interpreted as existing between the two domains. Farther north, the HVB narrows and folds plunge shallowly towards 212°, and then widens with folds plunging shallowly towards 017°. The changes can be explained by a localized increase in slip on the Austin Glen Detachment in the center of the map area, and subsequent loss of slip towards the north
Thesis (BA) — Boston College, 2010
Submitted to: Boston College. College of Arts and Sciences
Discipline: College Honors Program
Discipline: Geology and Geophysics
Whiting, Thomas H. "A study of the lithology and structure of the eastern Arunta Inlier based on aeromagnetic interpretation : a lithological subdivision and structural history of the eastern Arunta Inlier, with particular emphasis on the relationship between magnetic mineral petrogenesis, rock magnetism and aeromagnetic signature /." Title page, contents and abstract only, 1987. http://web4.library.adelaide.edu.au/theses/09PH/09phw6125.pdf.
Повний текст джерелаBoelema, Robert. "The metallogeny of the Upington and Kenhardt area, northern Cape." Thesis, Rhodes University, 1995. http://hdl.handle.net/10962/d1005587.
Повний текст джерелаWu, Kam-kuen, and 胡淦權. "Metamorphism of the Northern Liaoning Complex: implications for the tectonic evolution of the latearchean basement of the eastern block, North China Craton." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 2011. http://hub.hku.hk/bib/B46935605.
Повний текст джерелаNukman, Mochamad [Verfasser], Wilhelm [Akademischer Betreuer] Dominik, and Inga [Akademischer Betreuer] Moeck. "Geothermal exploration involving structural geology and hydrochemistry in the Tarutung Basin, Northern Central Sumatra (Indonesia) / Mochamad Nukman. Gutachter: Inga Moeck. Betreuer: Wilhelm Dominik." Berlin : Technische Universität Berlin, 2014. http://d-nb.info/1065669704/34.
Повний текст джерелаHoffmann, Markus [Verfasser], and Anke M. [Akademischer Betreuer] Friedrich. "Young tectonic evolution of the Northern Alpine Foreland Basin, southern Germany, based on linking geomorphology and structural geology / Markus Hoffmann ; Betreuer: Anke Friedrich." München : Universitätsbibliothek der Ludwig-Maximilians-Universität, 2017. http://d-nb.info/1139977849/34.
Повний текст джерелаHoffmann, Markus Verfasser], and Anke M. [Akademischer Betreuer] [Friedrich. "Young tectonic evolution of the Northern Alpine Foreland Basin, southern Germany, based on linking geomorphology and structural geology / Markus Hoffmann ; Betreuer: Anke Friedrich." München : Universitätsbibliothek der Ludwig-Maximilians-Universität, 2017. http://d-nb.info/1139977849/34.
Повний текст джерелаHansen, Christel Dorothee. "The characterisation of an openwork block deposit, northern buttress, Vesleskarvet, Dronning Maud Land, Antarctica." Thesis, Rhodes University, 2014. http://hdl.handle.net/10962/d1013138.
Повний текст джерелаMorrison, William F. "Vertical and Lateral Hydraulic Connectivity of the Wilcox Formation for Tiber Field and the Outbound Structural Province of Keathley Canyon and Walker Ridge, Northern Gulf of Mexico." ScholarWorks@UNO, 2018. https://scholarworks.uno.edu/td/2569.
Повний текст джерелаRohrer, Lucas P. "BEDROCK GEOLOGIC MAPPING AND STRUCTURAL ANALYSIS OF THE WESTERN HALF OF THE PETERSHAM QUADRANGLE, CENTRAL MASSACHUSETTS: FURTHER TESTS OF THE MODEL FOR MIDDLE TO LATE PALEOZOIC DUCTILE TRANSPRESSION, VERTICAL EXTRUSION, AND LATERAL ESCAPE IN THE NORTHERN APPALACHIANS." UKnowledge, 2015. http://uknowledge.uky.edu/ees_etds/32.
Повний текст джерелаSonwa, Cyrille Stephane Tsakou. "Analysis of the structural geology of the high-grade metamorphic rocks in part of the Kakamas terrane of an area adjacent to the Neusspruit shear zone South of the orange river, Northern Cape, South Africa." University of the Western Cape, 2021. http://hdl.handle.net/11394/8257.
Повний текст джерелаThe Proterozoic Namaqua-Natal Province comprises highly deformed rocks of medium to high grade metamorphism and is bordering the Archean Kaapvaal Craton to the west, south and east in South Africa. The sector to the west of the Craton, namely the Namaqua Sector, is structurally complex and subdivided from west to east into the Bushmanland Subprovince, the Kakamas and Areachap terranes of the Gordonia Subprovince and the Kheis Subprovince. The prominent Neusberg Mountain Range, with exposures to the north and south of the Orange River in the Kakamas Terrane constitutes evidence of crustal shortening as a result of continental collision of the Namaqua Sector block with the Kaapvaal Craton during the Namaquan Orogeny. The Mesoproterozoic Korannaland Group in the Kakamas Terrane is affected by faulting, folding and shearing.
Pogue, Kevin R. "Stratigraphic and structural framework of Himalayan foothills, northern Pakistan." Thesis, 1993. http://hdl.handle.net/1957/35578.
Повний текст джерелаGraduation date: 1994
Chernicoff, Carlos Jorge. "Synthesis of the structural geology of the Northern Transvaal." Thesis, 2014. http://hdl.handle.net/10210/10229.
Повний текст джерелаThe study area is subdivided into seven tectonic domains, viz. Bandelierkop, Southern Beit Bridge Complex, Alldays, Hestern Transvaal, Soutpansberg, Waterberg and Lebombo domains. The Bandelierkop domain comprises the Southern Marginal Zone of the Limpopo Belt (Bdl) and the northern portion of the Kaapvaal craton (Bd2). Bdl is characterized by the presence of highly disrupted xenoliths of pelitic and mafic supracrustal rocks distributed in a "s ea " of granitic ·material. This contrasts with the much bigger supracrustal xenoliths in Bd2, i.e. the greenstone belt relicts. The granulite facies rocks of Bdl may have been upthrust roughly from south to north along one or more south-dipping thrust faults soling into a gently-dipping to flatlying basal shear zone. Since this model reveals the existence of the Kaapvaal craton partly on edge, the progressively higher grade of regional metamorphism (from greenschist to granulite facies) encountered in the Bandelierkop domain, from south (Bd2) to north (Bdl), could express the transition from upper crust to lower crust as exposed on the present land surface. The structural trends found in Bdl and Bd2 are not strictly confined to either area, and some overlapping exists. The most distinct structural trend in Bdl is a west-northwest fold trend, a northeast fold trend also being recognized in the eastern portion of Bdl. Bd2 exhibits f~ld trends varying from west-northwest to northeast in orientation; in this area there is ample evidence for the later nature of the northwest- to west-northwest oriented folding event. The east-northeast- to northeast folding is con~ dered to represent an event independent of the effect of deformation of the Kudus River shear zone to which this folding was previously thought to be related.The portion of the Central Zone of the Limpopo Belt falling within South African territory comprises the Alldays and Southern Beit Br_idge Compl ex (SBBCd) doma tn s., There exists a marked contrast between the roughly north trending fold trends of the Alldays domain and the east-northeast fold structure of the southernmost part of the Central Zone, the SBBCd. The relatively gentle plunges of the fold structure of the Alldays domain may have accentuated the size of the regional folds in this region. The SBBCd occupies a narrow east-northeast oriented strip extending immediately south of the Alldays domain, where tightly folded gneisses and metasedim~nts are exposed. all strata are strongly aligned in the regionally extensive eastnortheast direction. A contrasting difference between the SBBCd and the surrounding Precambrian terranes is clear, as the former domain conveys a relatively higher strain; this evidence of heterogeneous strain suggests that the SBBCd represents a shear zone. The shearing movement may have been of thrust type, consistent with the thrust model referred to above, and the SBBCd may be regarded as the thrust plane. In'iiew of the steeply-dipping, south-southwest oriented fold axes known to exist along part of the SBBCd (area south of Messina), it would appear that, at least in that area, the thrust movement would have been towards the north-northeast. A late, involved history of deformation followed in the SBBCd, during which one or more episodes of wrench-type movement may have taken place. The Soutpansberg domain is a relatively narrow and long fault zone of Proterozoic to Phanerozoic age that separates 'mobile belt' environment to the north, from 'cratonic' environment to the south. A linked fault system characterized by south-dipping, normal listric faults soling into ? gently-dipping major detachment surface may account for the structural pattern of this domain. The thrust system referred to above, which developed earlier in the geological history of the region along the Limpopo Belt - Kaapvaal craton boundary, may have controlled the late extensional displacement in the Soutpansberg domain. The overall structure of the Waterberg domain would seem to be controlled by the superimposition of northeastand northwest oriented gentle folds and, with the exception of locally intense deformation in the early Waterberg basin, would appear to have developed on a relatively stable portion of crust. The structure of the Lebombo domain is characterized by a north-south striking monocline with gentle east dip. Most of the lineaments inferred from the aeromagnetic survey of the study area originate from dyke intrusions. Faulting, fracturing and shearing are less clearly manifested in the pattern of the aeromagnetic contour maps, instead they are better correlated with the lineaments inferre~ from LANDSAT imagery and from the drainage patterns of the region.
Van, Heeswijck Aldo. "The structure, sedimentology, sequence stratigraphy and tectonics of the northern Drummond and Galilee Basins, Central Queensland, Australia." Thesis, 2006. https://researchonline.jcu.edu.au/1557/1/01front.pdf.
Повний текст джерелаVan, Heeswijck Aldo. "The structure, sedimentology, sequence stratigraphy and tectonics of the northern Drummond and Galilee Basins, Central Queensland, Australia." 2006. http://eprints.jcu.edu.au/1557/1/01front.pdf.
Повний текст джерелаDavies, Richard Charles Idris. "Tectonic, magmatic and metallogenic evolution of the Cajamarca mining district, Northern Peru." Thesis, 2002. https://researchonline.jcu.edu.au/10/1/01front.pdf.
Повний текст джерелаDavies, Richard Charles Idris. "Tectonic, magmatic and metallogenic evolution of the Cajamarca mining district, Northern Peru /." 2002. http://eprints.jcu.edu.au/10.
Повний текст джерелаJones, James V. Connelly James N. "Proterozoic tectonic evolution of southern Laurentia new constraints from field studies and geochronology in southern Colorado and northern New Mexico, U.S.A. /." 2005. http://repositories.lib.utexas.edu/bitstream/handle/2152/1945/jonesiiij96843.pdf.
Повний текст джерелаRogers, Robert Douglas Mann Paul. "Jurassic-recent tectonic and stratigraphic history of the Chortis block of Honduras and Nicaragua (northern Central America)." 2003. http://wwwlib.umi.com/cr/utexas/fullcit?p3122784.
Повний текст джерелаSchneider, Craig L. "Pre-pliocene structural geology and structural evolution of the northern Los Angeles Basin, southern California." Thesis, 1994. http://hdl.handle.net/1957/35965.
Повний текст джерелаGraduation date: 1994
Rogers, Robert Douglas. "Jurassic-recent tectonic and stratigraphic history of the Chortis block of Honduras and Nicaragua (northern Central America)." Thesis, 2003. http://wwwlib.umi.com/cr/utexas/fullcit?p3122784.
Повний текст джерела