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Статті в журналах з теми "Geology Victoria Kanyapella Basin"
Lisker, Frank, and Andreas L. Läufer. "The Mesozoic Victoria Basin: Vanished link between Antarctica and Australia." Geology 41, no. 10 (October 2013): 1043–46. http://dx.doi.org/10.1130/g33409.1.
Повний текст джерелаHoldgate, G. R., T. A. G. Smith, S. J. Gallagher, and M. W. Wallace. "Geology of coal-bearing Palaeogene sediments, onshore Torquay Basin, Victoria." Australian Journal of Earth Sciences 48, no. 5 (October 2001): 657. http://dx.doi.org/10.1046/j.1440-0952.2001.00888.x.
Повний текст джерелаHoldgate, G. R., T. A. G. Smith, S. J. Gallagher, and M. W. Wallace. "Geology of coal-bearing Palaeogene sediments, onshore Torquay Basin, Victoria." Australian Journal of Earth Sciences 48, no. 5 (October 2001): 657–79. http://dx.doi.org/10.1046/j.1440-0952.2001.485888.x.
Повний текст джерелаHoldgate, G. R., S. J. Gallagher, and M. W. Wallace. "Tertiary coal geology and stratigraphy of the Port Phillip Basin, Victoria." Australian Journal of Earth Sciences 49, no. 3 (June 2002): 437–53. http://dx.doi.org/10.1046/j.1440-0952.2002.00930.x.
Повний текст джерелаLanigan, Kerrie-Anne. "Australia’s gas future: how Victoria can stay ahead of the pack." Proceedings of the Royal Society of Victoria 126, no. 2 (2014): 14. http://dx.doi.org/10.1071/rs14014.
Повний текст джерелаRose, Marion, Yi Zeng, and Mark Dransfield. "Applying FALCON® gravity gradiometry to hydrocarbon exploration in the Gippsland Basin, Victoria." Exploration Geophysics 37, no. 2 (June 2006): 180–90. http://dx.doi.org/10.1071/eg06180.
Повний текст джерелаEglington, Col. "Marine Ostracoda (Crustacea) from the Late Oligocene Gellibrand Marl, Otway Basin, Victoria, Australia." Proceedings of the Royal Society of Victoria 131, no. 2 (2019): 53. http://dx.doi.org/10.1071/rs19009.
Повний текст джерелаGunn, P. J., J. Mitchell, T. Mackey, and D. Cathro. "Evolution and Structuring of the Offshore Otway Basin, Victoria as Delineated by Aeromagnetic Data." Exploration Geophysics 26, no. 2-3 (June 1, 1995): 303–8. http://dx.doi.org/10.1071/eg995262.
Повний текст джерелаBESTLAND, E. A. "A Miocene Gilbert-type fan-delta from a volcanically influenced lacustrine basin, Rusinga Island, Lake Victoria, Kenya." Journal of the Geological Society 148, no. 6 (November 1991): 1067–78. http://dx.doi.org/10.1144/gsjgs.148.6.1067.
Повний текст джерелаUnverfärth, Jan, Thomas Mörs, and Benjamin Bomfleur. "Palynological evidence supporting widespread synchronicity of Early Jurassic silicic volcanism throughout the Transantarctic Basin." Antarctic Science 32, no. 5 (July 7, 2020): 396–97. http://dx.doi.org/10.1017/s0954102020000346.
Повний текст джерелаДисертації з теми "Geology Victoria Kanyapella Basin"
Millan, Cristina. "Syntectonic Fluid Flux in a Glaciated Rift Basin: Record from vein arrays in the AND-1B and AND-2A sedimentary rock cores, Victoria Land Basin, Antarctica." The Ohio State University, 2013. http://rave.ohiolink.edu/etdc/view?acc_num=osu1366309725.
Повний текст джерелаIsbell, John L. "Fluvial sedimentology and basin analyses of the Permian Fairchild and Buckley Formations, Beardmore Glacier Region, and the Weller Coal Measures, Southern Victoria Land, Antarctica /." The Ohio State University, 1990. http://rave.ohiolink.edu/etdc/view?acc_num=osu1487684245468595.
Повний текст джерелаBush, Angela L. "Physical and chemical hydrogeology of the Otway Basin, southeast Australia." Connect to thesis, 2009. http://repository.unimelb.edu.au/10187/8523.
Повний текст джерелаNelson, Emma Jane. "Present-day stress in Central and Southeast Australian sedimentary basins." 2007. http://hdl.handle.net/2440/45071.
Повний текст джерелаhttp://proxy.library.adelaide.edu.au/login?url= http://library.adelaide.edu.au/cgi-bin/Pwebrecon.cgi?BBID=1283781
Thesis(Ph.D.) -- Australian School of Petroleum, 2007
Nelson, Emma Jane. "Present-day stress in Central and Southeast Australian sedimentary basins." Thesis, 2007. http://hdl.handle.net/2440/45071.
Повний текст джерелаThesis(Ph.D.) -- Australian School of Petroleum, 2007
Nahm, Gi Young. "The hydrogeology of the Gippsland Basin, and its role in the genesis and accumulation of petroleum." 2002. http://repository.unimelb.edu.au/10187/1565.
Повний текст джерелаLockier, E. R. "Hydroclimate variability during the past millennium: a new record from West Basin Lake, Victoria." Thesis, 2015. http://hdl.handle.net/2440/118187.
Повний текст джерелаOur understanding of the long-term climate variability in Australia is limited by the number of high-resolution climate reconstructions. High-resolution palaeoenvironmental studies in Australia spanning more than a millennium are required to identify regional coherency among records and to recognise the relationships between climate and environmental conditions. This research project aims to investigate the nature of decadal-centennial scale climate and hydroclimate variability in south-eastern Australia. A record of hydrological change is established for the past millennium at West Basin Lake, a maar lake located in western Victoria. Palaeoclimate variability is inferred from sedimentary diatom analysis and is used to reconstruct lake water salinity. These data are interpreted in conjunction with element concentration data. The record indicates that West Basin Lake underwent hydrological variability on a decadal-centennial timescale. The diatom record shows evidence of a more variable climate during 932-550 cal BP and less saline conditions from 500-100 cal BP. The record also identifies a multi-decadal period of increased salinity from 625-575 cal BP. This suggests a more variable climate during the past millennium than observed since European settlement. The record established from this study provides a regionally coherent palaeoclimate reconstruction of the last millennium for western Victoria, Australia.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 2015
Dean, C. E. "Lake carbonate geochemistry as a proxy for paleohydrology: a validation-in-time at West Basin Lake, Victoria." Thesis, 2019. https://hdl.handle.net/2440/136950.
Повний текст джерелаThere is a lack of extensive historical climate data in Australia, meaning high-resolution paleoclimate studies are essential for a more comprehensive understanding of natural climate variability. The majority of paleohydrology records in south-eastern Australia region are low resolution, millennial time-scale reconstructions, resulting in a lack of understanding of climate variability at shorter time-scales relevant to human life spans. Here, we attempt to validate the use of geochemical analysis of lake sediments from West Basin, Victoria, as a way to create a high resolution paleohydrology reconstruction. The isotopic composition of the lake water in West Basin is primarily controlled by the precipitation to evaporation ratio (P:E). Ostracod calcite and bulk inorganic carbonates (BIC) that form within the water column reflect these changes and thus are used as proxies of past changes in P:E. This reconstruction is supported by a 210Pb- and 240/230Pu-based chronology which estimates a sediment accumulation rate of 0.3 to 0.4 cm/year and a maximum age at 40 cm of 118 years. This enables the resulting oxygen and carbon profiles to be validated against instrumental records of annual rainfall and temperature. The oxygen profile exhibits good agreement with this climate record, with peaks in δ18O values often coinciding with periods of low annual rainfall. Based on this, the ostracod record was determined to be capable of recording reliable, high resolution changes in P:E. The BIC record, though less consistent, can produce a detailed profile where ostracods are unavailable. Studies of this kind are vital to improving the accuracy of proxy system models which allow for reconstructions to be extended further in the geological record. Such models would allow for contextual understanding of the severity of drought occurrences and the assessment of the possible impacts of human induced climate change.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 2019
Merrett, H. D. "2D lithospheric imaging of the Delamerian and Lachlan Orogens, southwestern Victoria, Australia from Broadband Magnetotellurics." Thesis, 2016. http://hdl.handle.net/2440/121124.
Повний текст джерелаA geophysical study utilising the method of magnetotellurics (MT) was carried out across southwestern Victoria, Australia, imaging the electrical resistivity structure of the lithosphere beneath the Delamerian and Lachlan Orogens. Broadband MT (0.001-1000 Hz) data were collected along a 160 km west-southwest to east-northeast transect adjacent to crustal seismic profiling. Phase tensor analyses from MT responses reveal a distinct change in electrical resistivity structure and continuation further southwards of the Glenelg and Grampians-Stavely geological zones defined by the Yarramyljup Fault, marking the western limit of exploration interest for the Stavely Copper Porphyries. The Stawell and Bendigo Zones also show change across the Moyston and Avoca faults, respectively. Results of 2D modelling reveal a more conductive lower crust (10-30 Ωm) and upper mantle beneath the Lachlan Orogen compared to the Delamerian Orogen. This significant resistivity gradient coincides with the Mortlake discontinuity and location of the Moyston fault. Broad-scale fluid alteration zones were observed through joint analysis with seismic profiling, leaving behind a signature of low-reflectivity, correlating to higher conductivities of the altered host rocks. Isotopic analysis of xenoliths from western Victoria reveal the lithospheric mantle has undergone discrete episodes of modal metasomatism. This may relate to near-surface Devonian granite intrusions constrained to the Lachlan Orogen where we attribute the mid to lower crustal conductivity anomaly (below the Stawell Zone) as fossil metasomatised ascent paths of these granitic melts. This conductivity enhancement may have served to overprint an already conductive lithosphere, enriched in hydrogen from subduction related processes during the Cambrian. A predominately reflective upper crust exhibits high resistivity owing to turbidite and metasedimentary rock sequences of the Lachlan Orogen, representative of low porosity and permeability. Conductive sediments of the Otway Basin have also been imaged down to 3 km depth southwest of Hamilton.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 2016
Книги з теми "Geology Victoria Kanyapella Basin"
Ozimic, S. Gippsland Basin, Victoria. Canberra: Australian Government Pub. Service, 1987.
Знайти повний текст джерелаЧастини книг з теми "Geology Victoria Kanyapella Basin"
Barrett, P. J., S. A. Henrys, L. R. Bartek, G. Brancolini, M. Busetti, F. J. Davey, M. J. Hannah, and A. R. Pyne. "Geology of the Margin of the Victoria Land Basin off Cape Roberts, Southwest Ross Sea." In Geology and Seismic Stratigraphy of the Antarctic Margin, 183–207. Washington, D. C.: American Geophysical Union, 2013. http://dx.doi.org/10.1029/ar068p0183.
Повний текст джерелаCollen, J. D., and P. J. Barrett. "Petroleum Geology from the CIROS-1 Drill Hole, McMurdo SoundImplications for the Potential of the Victoria Land Basin, Antarctica." In Antarctica as an Exploration Frontier—Hydrocarbon Potential, Geology, and Hazards. American Association of Petroleum Geologists, 1990. http://dx.doi.org/10.1306/st31524c10.
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