Дисертації з теми "Geology Western Australia Carnarvon Basin"
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Van, Ruth Peter John. "Overpressure in the Cooper and Carnarvon Basins, Australia /." Title page, abstract and table of contents only, 2003. http://web4.library.adelaide.edu.au/theses/09PH/09phv275.pdf.
Повний текст джерелаMcHarg, Sam. "Tectonostratigraphic evolution of the Dampier Sub-basin, Northern Carnarvon Basin, Western Australia." Thesis, Curtin University, 2018. http://hdl.handle.net/20.500.11937/70560.
Повний текст джерелаCouzens, Mark Anthony. "Early cretaceous sequence stratigraphic architecture, Enderby Terrace, Carnarvon Basin, Western Australia /." Title page, abstract and contents only, 2003. http://web4.library.adelaide.edu.au/theses/09SB/09sbc872.pdf.
Повний текст джерелаMarlow, Alison. "Facies distribution within the M. australis section on the Enderby Terrace, Carnarvon Basin, Western Australia." Adelaide : [s.n.], 1995. http://web4.library.adelaide.edu.au/theses/09SB/09sbm347.pdf.
Повний текст джерелаMack, Daniel Aaron. "Seismic and stratigraphic interpretation of the Candace Terrace and Preston Shelf, Northern Carnarvon Basin, Western Australia /." Title page, contents and abstract only, 1993. http://web4.library.adelaide.edu.au/theses/09SM/09smm153.pdf.
Повний текст джерелаDraper, Paul Christopher. "Secondary migration fairways and hydrocarbon potential of the Southern Enderby Terrace, Northern Carnarvon Basin, Western Australia /." Title page, contents and abstract only, 1995. http://web4.library.adelaide.edu.au/theses/09SB/09sbd766.pdf.
Повний текст джерелаTwo folded maps in pocket inside back cover. Includes bibliographical references (leaves 130-135).
Quinn, Matthew J. "Glaucony as an environmental indicator, with examples from the Cretaceous of the Northern Carnarvon Basin, Western Australia /." Title page, contents and abstract only, 1997. http://web4.library.adelaide.edu.au/theses/09S.B/09s.bq72.pdf.
Повний текст джерелаEleven enclosures in six pockets inserted through text. Includes bibliographical references (leaves 52-54).
Quintavalle, Marco. "Lower to Middle Ordovician palynomorphs of the Canning Basin, Western Australia /." [St. Lucia, Qld.], 2004. http://www.library.uq.edu.au/pdfserve.php?image=thesisabs/absthe18370.pdf.
Повний текст джерелаSuwarna, Nana. "Petrology of Jurassic coal, Hill River area, Perth Basin, Western Australia." Thesis, Curtin University, 1993. http://hdl.handle.net/20.500.11937/675.
Повний текст джерелаIasky, Vickie Clare. "Seismic sequence stratigraphy and facies characterisation of the G and H units within the Goodwyn Field Northern Carnarvon Basin Western Australia /." Title page, abstract and table of contents only, 2004. http://web4.library.adelaide.edu.au/theses/09SB/09sbi118.pdf.
Повний текст джерелаSuwarna, Nana. "Petrology of Jurassic coal, Hill River area, Perth Basin, Western Australia." Curtin University of Technology, Department of Applied Geology, 1993. http://espace.library.curtin.edu.au:80/R/?func=dbin-jump-full&object_id=15765.
Повний текст джерелаto the metalignitous type of the Pareek classification. On the basis of carbon and hydrogen content, the coal is categorised as per-hydrous meta- to ortho-lignitous type. The trace elements As, B, Be, Cd, Co, Cr, Cu, Ga, Mn, Mo, Ni, Pb, Sr, Th, U, V, Y, Zn, and Zr, are spectrographically analysed in the coal ash. The B content in the coal supports the presence of marine influence during peat deposition in the basin.On the basis of lithotype, maceral, microlithotype, trace element distribution, pyrite and total sulphur in the coal, the depositional environment for coal and the coal measures, is interpreted as an upper to lower delta type within a regressive phase of marine transgression.
Hull, Jonathan N. F. "Sequence stratigraphic evolution of the Albian to recent section of the Dampier Sub-basin, North West Shelf, Australia." Title page, contents and abstract only, 1999. http://web4.library.adelaide.edu.au/theses/09PH/09phh9128.pdf.
Повний текст джерелаRedfern, Jonathan. "The sedimentology and stratigraphy of the Permo-Carboniferous Grant Group, Barbwire Terrace, Canning Basin, Western Australia." Thesis, University of Bristol, 1990. http://hdl.handle.net/1983/79d4d3ba-71cb-4e52-8f26-d4acd7fa27f0.
Повний текст джерелаBailey, Brett B. "Geological and geophysical evaluation of the Thebe field, Block XX, offshore Western Australia." University of the Western Cape, 2013. http://hdl.handle.net/11394/4028.
Повний текст джерелаThe North West Shelf of Australia is a prolific gas province. The Thebe Gas Field is situated within the northern central Exmouth Plateau in the Northern Carnarvon Basin. The Exmouth Plateau is a submerged continental block whose culmination lies at about 800m below sea level. The seismic data used for this study is the HEX07B survey which was conducted in 2007. The objective of this study was to interpret all available seismic data, of which six horizons were picked, generating two-way-time structure maps and an average velocity map, performing depth conversion and generating various depth maps. The horizons picked were the economic basement, Triassic Mungaroo, Murat Siltstone, Muderong Shale, Gearle Siltstone and the Sea Bed. The horizon of interest was the Triassic Mungaroo Formation and therefore it was the only horizon with an average velocity map. The seismic sections were used in conjunction with the structure maps generated to identify possible locations for appraisal wells to be drilled. Prospect X was identified on the basis of amplitude and structure present within the Triassic Mungaroo Formation. The final task was to calculate the volumes present and a Monte-Carlo Simulation was used for this. The results obtained showed that Prospect X has a good petroleum system in place. The Mungaroo Formation is identified as being the possible source and reservoir rock, the Muderong Shale is the seal, structural traps are provided by large fault block and faults provided the migration pathways from the source in to the reservoir. The volumes were calculated using three areas identified on the structure maps by three closing contours. These areas are the P90, P50, P10 and the volumes for the gas in place were as follows, P90 = 893 Bcf (0.9Tcf), P50 = 1128 Bcf (1.1 Tcf), P10 = 1367 Bcf (1.4Tcf). Using the various parameters the probability of success for Prospect X was calculated to be 20%.
Rutherford, Jasmine Lee. "The role of geology, geomorphology, climate and vegetation, in controlling spatial and temporal changes in groundwater discharge from weathered crystalline basement aquifers in southwestern Australia." University of Western Australia. School of Earth and Geographical Sciences, 2006. http://theses.library.uwa.edu.au/adt-WU2006.0006.
Повний текст джерелаWinhusen, Eric. "PRECAMBRIAN SEAWATER TEMPERATURE ANALYSIS USING OXYGEN ISOTOPES FROM HAMERSLEY CARBONATES, WESTERN AUSTRALIA." University of Cincinnati / OhioLINK, 2001. http://rave.ohiolink.edu/etdc/view?acc_num=ucin992268720.
Повний текст джерелаHamp, Lonn P. "Petrology of the Late Proterozoic(?)-Early Cambrian Arumbera Sandstone, Western MacDonnell Ranges, North-Central Amadeus Basin, Central Australia." DigitalCommons@USU, 1985. https://digitalcommons.usu.edu/etd/6679.
Повний текст джерелаVan, Ruth Peter John. "Overpressure in the Cooper and Carnarvon Basins, Australia / Peter John van Ruth." Thesis, 2003. http://hdl.handle.net/2440/22125.
Повний текст джерелаPhD (by publication).
Includes bibliographical references.
vii, 21, [49] leaves : ill. (some col.), maps, photos (some col.) ; 30 cm.
Title page, contents and abstract only. The complete thesis in print form is available from the University Library.
Thesis (Ph.D.)--University of Adelaide, Australian School of Petroleum (ASP), 2004
Cathro, Donna Louise. "Three-dimensional stratal development of a carbonate-siliciclastic sedimentary regime, Northern Carnarvon Basin, Northwest Australia." Thesis, 2002. http://wwwlib.umi.com/cr/utexas/fullcit?p3108481.
Повний текст джерелаSmith, Stuart A. (Stuart Andrew). "The phanerozoic basin-fill history of the Roebuck Basin." 1999. http://web4.library.adelaide.edu.au/theses/09PH/09phs6615.pdf.
Повний текст джерелаWang, Chin-An, and 王金安. "Permian Paleoenvironment inferred from Oxygen and Carbon Isotope Records of Brachiopod Shells from Canning Basin and Carnarvon Basin, Western Australia." Thesis, 2011. http://ndltd.ncl.edu.tw/handle/38685695821274426233.
Повний текст джерела國立臺灣師範大學
地球科學系
100
To construct the middle paleolatitude environment in the Permian. One hundred and twelve brachiopod shells from two Western Australian basins (Carnarvon and Canning Basins) have been analyzed for oxygen and carbon isotopes to study. All samples were thin sectioned and examined under the petrographic and cathodoluminescence microscopes for evaluating shell preservation. A total of 249 isotopic analyses from well preserved portion (non-luminescent; NL) were found useful for inferring the paleoenvironment. Average δ13C values of NL shells were 4.4 ± 0.5‰ (N = 28) for the Callytharra Formation (late Sakmarian-early Artinskian), 4.5 ± 0.8‰ (N = 4) for the Jimba Jimba Calcarenite (early Artinskian), 4.7± 0.8‰ (N = 10) for the Coyrie/Madeline Formations (both late Artinskian-early Kungurian), 4.9 ±0.6‰ (N =5) for the Quinnanie Shale and Cundlego Formation (both Kungurian), 4.2 ± 0.7‰ (N = 9) for the Wandagee Formation (late Kungurian), 5.1 ± 1.1‰ (N = 6) for the Noonkanbah Formation (Artinskian- Kungurian), 5.4 ± 0.2‰ (N =2) for the Lightjack Formation(Roadian-Capitanian), and 4.8± 0.3‰ (N = 3) for the Hardman Formation (Wuchiapingian). Within the uncertainty of the stratigraphical correlation, the carbon isotope values spanning Late Sakmarian to Kungurian are comparable to those of low latitude Urals. Average δ18O values of NL shells were about 0‰ (-0.2 to 0.2‰) for Callytharra Formation(-0.1±0.5‰), Jimba Jimba Calcarenite(-0.1±0.5), Coyrie/Madeline Formations(-0.2±0.4‰), Quinnanie Shale and Cundlego Formation(-0.1±0.4‰), Noonkanbah Formation(0.1±0.5‰), and Hardman Formation(-0.0±0.3‰); and were -0.5 ± 0.7‰ and -0.6± 0.9‰ for Wandagee Formation and Lightjack Formation, respectively. These oxygen isotope values are overall greater than the coeval values reported for low latitude regions and for eastern Australia. These relatively more positive oxygen isotope values are here interpreted to indicate a possible high evaporation condition for the two studied basins in Western Australia during the Permian.
Frost, Edmund Locke 1974. "Facies heterogeneity, platform architecture and fracture patterns of the Devonian reef complexes, Canning Basin, Western Australia." Thesis, 2007. http://hdl.handle.net/2152/3578.
Повний текст джерелаWaclawik, Victor G. "Landscape evolution of the Umbum Creek Catchment, Western Lake Eyre, Central Australia." 2006. http://hdl.handle.net/2440/42833.
Повний текст джерелаhttp://proxy.library.adelaide.edu.au/login?url= http://library.adelaide.edu.au/cgi-bin/Pwebrecon.cgi?BBID=1260856
Thesis (Ph.D.) -- School of Earth and Environmental Sciences, 2006
Waclawik, Victor G. "Landscape evolution of the Umbum Creek Catchment, Western Lake Eyre, Central Australia." Thesis, 2006. http://hdl.handle.net/2440/42833.
Повний текст джерелаThesis (Ph.D.) -- School of Earth and Environmental Sciences, 2006
McManus, Andrew. "Burial diagenesis and Mississippi Valley-type mineralization in the upper Devonian reef complexes of the Lennard Shelf, Canning Basin, Western Australia." Thesis, 1991. http://hdl.handle.net/2440/112775.
Повний текст джерелаThesis (M.Sc.) -- University of Adelaide, National Centre for Petroleum Geology and Geophysics, 1992
Fujii, Tetsuya. "Using 2D and 3D basin modelling and seismic seepage indicators to investigate controls on hydrocarbon migration and accumulation in the Vulcan Sub-basin, Timor Sea, North-western Australia." 2007. http://hdl.handle.net/2440/40062.
Повний текст джерелаhttp://proxy.library.adelaide.edu.au/login?url= http://library.adelaide.edu.au/cgi-bin/Pwebrecon.cgi?BBID=1277632
Thesis(M.Sc.)-- Australian School of Petroleum, 2007.
Fujii, Tetsuya. "Using 2D and 3D basin modelling and seismic seepage indicators to investigate controls on hydrocarbon migration and accumulation in the Vulcan Sub-basin, Timor Sea, North-western Australia." Thesis, 2007. http://hdl.handle.net/2440/40062.
Повний текст джерелаThesis (M.Sc.) -- Australian School of Petroleum, 2007.
Watson, Simon Timothy. "Conodonts from a core of the Nita and Goldwyer Formations (Lower Middle Ordovician) of the Canning Basin, Western Australia /." 1986. http://collections.mun.ca/u?/theses,119083.
Повний текст джерелаThomas, M. C. "Erskine Sandstone Formation: a provenance and geochronological study within the Fitzroy Trough, Western Australia." Thesis, 2012. http://hdl.handle.net/2440/95492.
Повний текст джерелаThe Erskine Sandstone Formation is located in the Fitzroy Trough, within the northern Canning Basin, Western Australia. The provenance evolution of the onshore Triassic sandstone of the Erskine Sandstone Formation has not previously been researched. Field work was conducted predominantly at two areas, the Erskine Range, the type section of the Sandstone, and the May River outcrops which include the Pinnacle Rock outcrop. Field work in the area showed a transitional boundary between the underlying Blina Shale and the Erskine Sandstone Formation making identification of the boundary zones difficult. Through the use of U-Pb zircon analysis on samples taken from the Erskine Range and the May River, this study suggests the two outcrops have differing sources. Samples taken from the Erskine Range contain Permian aged sediments which are not present in the May River samples. The significant presence of Mesoproterozoic sediments in the May River samples which are not reflected in the Erskine Range samples further suggests different sources. The large presence of Palaeoproterozoic sediments in both the Erskine Range and the May River outcrops suggests the uranium rich King Leopold Ranges is a possible source. These sediments, combined with the presence of reductants in the Erskine Sandstone Formation suggest the possibility of sandstone-hosted uranium mineralisation within the Fitzroy Trough. Other possible sediment sources include the Musgrave Block and Arunta Inlier, located to the south, and suggest a complex detrital history of the Fitzroy Trough.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Earth and Environmental Sciences, 2012