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Статті в журналах з теми "Honours; Geology"
Walkden, Gordon. "A Field-Based “Oil Business Game” for Honours Geology Students." Planet 1, no. 1 (January 2001): 8–12. http://dx.doi.org/10.11120/plan.2001.00010008.
Повний текст джерелаJohnson, G. A. L. "Sir Kingsley Charles Dunham. 2 January 1910 – 5 April 2001 Elected FRS 1955." Biographical Memoirs of Fellows of the Royal Society 49 (January 2003): 147–62. http://dx.doi.org/10.1098/rsbm.2003.0009.
Повний текст джерелаTirdad, Shiva, Erwan Gloaguen, Abderezzak Bouchedda, and J. Christian Dupuis. "Three-dimensional stochastic assimilation of gravity data in Lalor volcanogenic massive sulphide, Manitoba, Canada." Canadian Journal of Earth Sciences 56, no. 5 (May 2019): 556–68. http://dx.doi.org/10.1139/cjes-2018-0166.
Повний текст джерелаSimmons, Michael D., Peter R. Sharland, David M. Casey, Roger B. Davies, and Owen E. Sutcliffe. "Arabian Plate sequence stratigraphy: Potential implications for global chronostratigraphy." GeoArabia 12, no. 4 (October 1, 2007): 101–30. http://dx.doi.org/10.2113/geoarabia1204101.
Повний текст джерелаLord, Alan R., and John E. Whittaker. "On the award of TMS Honorary Membership, 17 November 2004 Professor Robin Whatley – an appreciation." Journal of Micropalaeontology 24, no. 1 (May 1, 2005): 95–96. http://dx.doi.org/10.1144/jm.24.1.95.
Повний текст джерелаPaar, Rinaldo. "Carl Ritter von Ghega – 2018 Surveyor of the Year." Kartografija i geoinformacije 18, no. 32 (December 15, 2019): 64–78. http://dx.doi.org/10.32909/kg.18.32.5.
Повний текст джерелаWong, Theo E., Salomon B. Kroonenberg, and Tom J. A. Reijers. "Editorial." Netherlands Journal of Geosciences - Geologie en Mijnbouw 95, no. 4 (November 21, 2016): 373–74. http://dx.doi.org/10.1017/njg.2016.41.
Повний текст джерелаGraversen, Ole, and Jens Morten Hansen. "Danmarks Geologipris -Denmark's Geology Prize." Bulletin of the Geological Society of Denmark 41 (November 30, 1994): 126–27. http://dx.doi.org/10.37570/bgsd-1995-41-22.
Повний текст джерелаJenkyns, Hugh. "Geology Honors Exceptional Reviewers." Geology 35, no. 2 (2007): 192. http://dx.doi.org/10.1130/0091-7613(2007)35[192:gher]2.0.co;2.
Повний текст джерелаDewey, John Frederick, and Bernard Elgey Leake. "Robert Millner Shackleton. 30 December 1909 – 3 May 2001." Biographical Memoirs of Fellows of the Royal Society 50 (January 2004): 285–97. http://dx.doi.org/10.1098/rsbm.2004.0018.
Повний текст джерелаДисертації з теми "Honours; Geology"
Cave, B. J. "Copper - Gold exploration in the Middleback Ranges; source(s) of fluids and metals." Thesis, 2010. http://hdl.handle.net/2440/98295.
Повний текст джерелаThe Moola Prospect of the Middleback Ranges, South Australia is an epigenetic, hypothermal copper-gold prospect that displays several clear genetic affinities with IOCG deposits/prospects in the Gawler Craton, although from this study alone classification of the mineralisation is imprudent. A broad study on the mineral paragenesis and geochemistry of the deposit was carried out on a single drill core provided by OneSteel, the holder of the tenement encompassing the Moola Prospect. The mineralisation, characterised by pyrite + chalcopyrite, hematite and magnetite, is hosted by the Palaeoproterozoic metavolcanic / volcaniclastic, Myola Volcanics and an unnamed, undated fine-grained microgranite that intrudes the Myola Volcanics. This unnamed, undated microgranite, displays geochemical and petrological similarities with the Myola Volcanics from which it‘s thought to be partial derived from its anatexis; likely being a Wertigo Granite equivalent. Four alteration assemblages were observed in the Moola Prospect drill core and placed into the following paragenic sequence; Na (Ca-Fe) characterised by the formation of albite; sericite replacing K-feldspar and plagioclase and alteration increasing towards sericite veining; chlorite with alteration increasing towards chlorite-mica±epidote veins; late stage quartz, quartz-carbonate, carbonate flooding, that hosts mineralisation. Ore mineral paragenesis occurs in an overlapping sequence; the first mineral precipitated was magnetite that was later extensively martitised, with hematite followed by pyrite and minor heamatite + pyrite, pyrite + chalcopyrite, then chalcopyrite. Later supergene alteration altered the chalcopyrite to native copper and malachite. Sphalerite precipitation couldn‘t be constrained from petrological evidence alone. Iron oxide and sulphide chemistry, and sulphur isotopes from the sulphides support this paragenesis, and constrains precipitation of sphalerite between the pyrite only and chalcopyrite only phases. Iron oxide chemistry also revealed the presence of illmentite in the core, however could only constrain illmentite precipitation as, coeval to after haematite precipitation. Sulphur isotopes revealed evidence for an additional late stage pyrite precipitation, after the chalcopyrite only phase. Bulk rock composition was quite variable with some altered samples showing strong enrichments of Fe2O3, SiO2, CaO, K2O, Na2O SO3, MnO, P2O5 and MgO. Strong enrichment of CaO and/or SiO2 in some of the altered samples, but not others, suggests that the quartz-carbonate alteration represented by this geochemical signature is sporadic in nature. Depletion in SiO2 in some of the altered samples could also represent the consumption of silica during the Na-Ca-Fe alteration event. Enrichment of SO3 in the altered samples likely directly represents alteration related to the precipitation of sulphide ore minerals. Trace element and rare earth element compositional changes from alteration shows enrichments of Cu, U, Pb, Li, B, Mn and V likely relating to alteration associated with mineralisation. εNd (1590Ma) values of the Moola Prospect together with εNd (1590Ma) versus whole rock Cu concentration and Co: Ni ratios of pyrite, indicates a crustal derived, with minor mantle input for the sources of metals. Sulphur isotopes and trace element whole rock geochemistry indicates a primitive/ magmatic fluid source is responsible for alteration and/ or mineralisation.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Earth and Environmental Sciences, 2010
Jones, R. S. W. "Cu mineralisation in the Middleback Ranges: conditions of mineralisation." Thesis, 2010. http://hdl.handle.net/2440/101671.
Повний текст джерелаThe Moola Prospect situated within the Middleback Ranges on the northern Eyre Peninsula, South Australia, is comprised of potential IOCG-style, Cu mineralisation which appears to share some geological and mineralogical affinities with other IOCG deposits throughout the Gawler Craton. This recently identified mineralisation represents a new exploration region within the southern extent of the Olympic Cu-Au province which has proven to be highly lucrative with the recent discovery of the Hillside deposit in the neighbouring Yorke Peninsula. A broad investigation into host rock lithology, alteration and mineralisation paragenesis, as well as paleotemperature-pressure conditions of the deposit was carried out on drill core from OneSteel’s inaugural exploratory diamond drill hole. The mineralisation is hosted within the Paleoproterozoic Myola Volcanics, a package of rhyolites, rhyodacites and felsic gneisses which are intruded by amphibolite sills and granitic intrusives, assumed to be the neighbouring Wertigo granite. Prominently vein hosted, the mineralisation is localised around a north-northeast trending shear zone inferred to be an expression of the Kimban aged, Kalinjala shear zone which is located ~60 Km west of the Middleback Ranges. The alteration mineralogy present is divisible into two main assemblages, an early albite-epidote assemblage which has experienced extensive overprinting by the main mineralising phase associated with a quartz-carbonate-sericite± hematite-sulphide assemblage. Ore mineral paragenesis occurs as a transition of overlapping minerals that record coprecipiation. The first mineral to form was magnetite which was later extensively martitised during the transition to hematite precipitation which is preceded by a transition to pyrite, then finally chalcopyrite. A later phase of native copper mineralisation is recorded within the transecting shear zone which represents a supergene enrichment interpreted to have occurred as meteoric water gained access to depth via the structural weakness of the shear zone and remobilised any sulphides present, which were redeposited as native copper. The temperature of mineralisation was established by TitaniQ thermometry which provided a precise temperature range between 415-530 °C with the peak at ~475 °C, which represents the conditions at which the paragenically linked quartz and mineralisation formed. Chlorite thermometry was also performed to obtain a temperature of mineralisation, with a few samples corresponding with the conditions established by the TitaniQ thermometer; however a majority of the data overestimates the temperature range by an unacceptable amount. Pressure conditions were reconstructed using the much more reliable TitaniQ temperature range inconjuntion with fluid inclusion data to establish the pressure conditions of mineralisation which ranged between ~5-7 kbar, and indicated mineralisation occurred at a deep crustal setting. Fluid and mineralisation characteristics indicate a moderate salinity inferred from the fluid inclusions study, with NaCl ranging between 27.5-7.5 equiv wt%, along with a sulphur isotopic signature corresponding with magmatically derived fluids with the δ34S ranging between -10.5 and -1.2 ‰. Which corresponds with other IOCG style mineralisation present throughout the Craton, with the Moola Prospect also being spatially associated to the interpreted source of these fluids within the Galwer Craton, the Hiltaba Suite granitoids? Even though the Moola Prospect shares affinities with IOCG style mineralisation this study cannot definitively identify its model of genesis as it also comprises characteristics that contradict this model, indicating that further study is required to better understand the extent and nature of this mineralising system.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 2010
Barker, A. R. "The thermal properties, temperature structure and thermal evolution of the Eastern Ghats, India." Thesis, 2010. http://hdl.handle.net/2440/98285.
Повний текст джерелаThe role of the portable gamma ray spectrometer has become a fundamental addition for gathering heat production data to constrain stochastic thermal modelling of the crust. Numerous sensitivity and calibration analyses have been undertaken to verify the validity of the output, and to aid in more efficient and effective use for future users. When applied to a heat flow study of the Eastern Ghats, it was established that the predominantly granulite-facies rocks such as khondalites, Kfeldspar megacrystic granites and quartzo-feldspathic gneisses have high average heat production values of 3.76 ± 0.53μWm-3, 2.79 ± 0.53μWm-3 and 5.49 ± 0.69μWm-3 respectively, whereas the UHT granulites have a low heat production of 0.69 ±0.23 μWm-3. The contribution of uranium to the total heat production was considered low when compared to the input from thorium, which was almost four times higher. The average concentrations of thorium were also approximately fifteen times more than the concentrations of uranium. In this research, thermal conductivity testing was conducted to better constrain parameters for stochastic thermal modelling. Coupled with previous seismic studies, four crustal sections were analysed by one-dimensional steady-state finite difference models using the results of this project. Conclusions drawn from this study indicate that there is a possibility the Eastern Ghats is currently a UHT region, whereas burial of these high heat-producing rocks during orogenesis could have readily heated the crust to produce UHT granulite-facies metamorphism.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Earth and Environmental Sciences, 2010
Grguric, B. "The petrology, geochemistry, and fluid history of calc-silicate rocks and associated primary Cu-Co mineralization in the Ethiudna Mines area, Olary Province, South Australia." Thesis, 1992. http://hdl.handle.net/2440/113058.
Повний текст джерелаTextures in calc-silicate rocks of the Lower Proterozoic Bimba Suite in the Ethiudna mines area, Olary Province, South Australia, record multiple fluid infiltrational episodes associated with both prograde, amphibolite-facies, and retrograde, greenschist-facies metamorphism. Pervasive infiltration of H2O-rich fluids (XCO2<0.18) during prograde metamorphism, was associated with the large-scale development of wollastonite-rich lithologies within the Bimba Suite. Stable oxygen isotope evidence suggests these fluids were equilibrated with siliciclastic sequence(s) prior to infiltrating the Bimba Suite. A second, retrograde metamorphic (temperatures -300oC) infiltrational episode was associated with the development of a grossular-quartz assemblage. Fluid flow was channelized during this episode, the H2O-rich fluids being focussed along structurally-induced zones of high permeability. Large variations in fluid/rock ratios are recorded in the calc-silicates as large variations in the progress of the grossular-quartz producing reaction. The formation of cross-cutting quartz, calcite, and rare laumontite veins postdates both these infiltrational episodes. Fluid inclusion evidence suggests these veins were deposited by fluids at temperatures of less than 250°C. Fluid inclusion data and scapolite compositional data indicate fluids associated with all three episodes were highly saline, consistent with conclusions made by earlier workers that the Bimba Suite represents a meta-evaporite sequence. The microcline-rich rocks of the. Quartzofeldspathic Suite, which underlies the Bimba Suite, host stratiform and disseminated Cu-Co sulphide mineralization. Geochemical and petrological evidence suggests this mineralization is of the genetic type known as a red-bed-associated Cu deposit. The distribution, geochemistry, and textural characteristics of sulphides in the Bimba Suite, suggest this mineralization represents a metasomatic remobilization of pre-metamorphic Quartzofeldspathic Suite mineralization. The sulphide-silicate-carbonate textural relationship in the Bimba Suite suggests this remobilization took place during the high temperature, wollastonite-producing infiltrational episode, and that precipitation of ore metals was effected by a pH rise.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 1992
Guerin, R. J. "Petrography, mineralogy and trace element chemistry of Cu-Au-Mo mineralisation from Central Diorite, Boddington, W.A." Thesis, 2011. http://hdl.handle.net/2440/88640.
Повний текст джерелаThe world-class Boddington Cu-Au-Mo deposit has a complex genetic history. The relative importance of different ore-forming processes during the period 3.0 – 2.6 Ga is debated, particularly with respect to the role played by the 2611±3 Ma Wourahming granite. LA-ICP- MS analysis of trace element concentration in molybdenite represents a valuable new metallogenetic tool to track mineralising events in deposits with protracted geologic histories. The Re content and trace-element signatures in molybdenite from diorite and granite show three distinct populations, attributed to porphyry-style (hundreds of ppm) orogenic- and granite-related systems (<1 to a few ppm, respectively). Rhenium concentrations in molybdenite are highly variable on the deposit-scale. Economic concentrations of Re occur only at shallower levels in both Central Diorite and ABreccia. The Au content correlates with high-concentrations of chalcophile elements (CE). This is seen in the association of Au- minerals and Bi-(Pb)-tellurides present as inclusions in the molybdenite from diorite and is inferred from an LA-ICP-MS element map for molybdenite in granite. The FIB-SEM and TEM study show that visible telluride inclusions extend down to the nanoscale as coherent intergrowths with host molybdenite. Nanoporosity is accompanied by a whole range of structural defects and twinning. The telluride species identified include unnamed Bi4Pb7Te4S9. Analysis of stacking sequences show co-precipitation of Bi-tellurides and molybdenite under equilibrium conditions. In corroboration with EPMA data, this is the first confirmation that minerals from the aleksite series are characteristic components of the ore at Boddington. Molybdenite with high-concentration of chalcophile elements is present as the 2H polytype only, contrary to previous hypothesis that incorporation of trace elements is assisted by 3R structural modification. Instead, a new mechanism is presented in which coherent lattice-scale intergrowths between molybdenite and tellurides are reasons for the measured high CE concentrations. Knowing that Bi-(Pb)-tellurides are Au-carriers, this may also explain the observed, unusual Au-enrichment in molybdenite from Boddington. Nucleation of Au fine particles is inferred from element map correlations but further work is necessary to prove if Au nanoparticles are also present. Petrographic, mineralogical and geochemical evidence support a three-stage model for Boddington. An early porphyry event can account for the bulk of the Cu mineralisation, as well as some of the Au and Mo. A subsequent orogenic-Au event led to shearing and remobilisation of ore components. New constraints on metamorphic conditions are offered by chlorite and stannite-sphalerite geothermometry (200-420 °C) and the occurrence of two co- existing pyrrhotite species. The granite introduced some Au, Mo and other „granitic‟ elements, notably Bi leading to substantial upgrading of Au grades by Bi-melt scavenging. The study concludes however that hydrothermal activity associated with granite was not the most important concentrator of ore minerals.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Earth and Environmental Sciences, 2011
Macintosh, J. N. "Age and basin evolution of the Cuddapah Supergroup, India." Thesis, 2010. http://hdl.handle.net/2440/103376.
Повний текст джерелаU-Pb zircon geochronology indicates deposition of the Cuddapah Supergroup, Cuddapah Basin, India occurred for at least 986 million years. Deposition started after 2502±17 Ma with the deposition of the Gulcheru Formation and ended after 913±11 Ma with the deposition of the Cumbum Formation. Maximum depositional ages have been found for individual formations within the Cuddapah Supergroup; the Pulivendla Formation has a maximum deposition of 1899±19 Ma and the Bairenkonda Formation has a maximum depositional age of 1660±22 Ma. Thermal events during the Palaeoproterozoic present a possible cause of basin formation. At this early stage of the Cuddapah Basin’s evolution the provenance of sediments was the Dharwar Craton, which currently underlies the basin and borders it on the north, south and west sides. The uplift of the Eastern Ghats on the eastern margin affected the evolution of the Cuddapah Basin, changing the shape and the sediments of the basin. Uplift and deformation events in the Eastern Ghats folded the eastern side of the Cuddapah Basin and are responsible for its present crescent shape. The formation of the Eastern Ghats caused increased subsidence to the east, creating an asymmetry in the depth of the basin. The provenance of the sediments of the Cuddapah Supergroup changed to the Eastern Ghats for the deposition of the youngest stratigraphic group, the Nallamalai Group.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 2010
Saunders, P. J. "The structural evolution of the Bull Creek area, southern Adelaide fold belt, South Australia; through the integration of geological mapping and geophysical interpretation." Thesis, 1993. http://hdl.handle.net/2440/87598.
Повний текст джерелаIntegration of a high resolution aeromagnetic survey with detailed structural field data has been achieved in the Bull Creek area of the southern Adelaide Fold Belt, resulting in a comprehensive model for the structural evolution of this area. Aeromagnetic data has placed constraints upon structures mapped at the surface and has also revealed information concerning the nature of structures at depth. The successful interpretation of data is due to the good lithomagnetic marker horizons within the area. These horizons include the magnetic Barossa Complex basement and lithomagnetic units of the Adelaide Supergroup and Kanmantoo Group metasediments. The Brachina Formation, an important magnetic marker horizon of the Adelaide Supergroup, lies at depth (due to thrust related tear-faulting) beneath a magnetic cover of Backstairs Passage Formation of the Kanmantoo Group sediments. Geophysical images and contour maps reveal the location and intensity of important magnetic and radiometric anomalies which constrain the interpretation of mapped structures. Modelling of individual magnetic profiles places constraints on the depth to the top, the width, dip and susceptibility of magnetic bodies. Vertical gradient filtering enhances the edges of two dimensional sources and Automated Gains Control filtering amplifies the effects of small anomalies. A model suggesting multiple sequential thrusting has been devised for the Bull Creek area. This model incorporates a basal decollement located within the basement (4-5 km beneath the present erosion level) which has transported a sliver of basement complex to the surface where it forms a hanging wall anticline. An upper detachment has formed near the basement - cover contact within the basal unit of the Adelaidean sequence. High angle histric thrusts of an imbricate fan (or sigmoidal faults of a duplex system?) stem from this detachment fault.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Earth and Environmental Sciences, 1993
Errock, C. H. "Hydrocarbon migration and mixing in four recently discovered oil fields of the southwestern Eromanga Basin." Thesis, 2005. http://hdl.handle.net/2440/93338.
Повний текст джерелаThe Cooper and Eromanga Basin is located in northeastern South Australia and southwestern Queensland. Nine samples from four fields within the SA sector of the Cooper-Eromanga Province along the southwestern Patchawarra Trough (Sellicks and Christies) and western Wooloo Trough (Worrior and Arwon) were analysed. The aromatic source and maturity cross plot of 1-MP/9-MP versus 2-MP/1-MP was used to determine the ratio of mixing between Permian- and Jurassic/Cretaceous-sourced hydrocarbon in oils. These oils from the Patchawarra Formation within the Sellicks Field has ~0.9% Rc and is a Family 2 Permian end-member, which has migrated a minimum distance of 23-24 km. This same oil contributes 60-70% of the input to the Birkhead and Hutton reservoirs in the Christies Field. The Jurassic input (~0.6% Rc) came from a Birkhead source located 15-30 km to the east. The Worrior and Arwon Fields contain mixed oils within Jurassic and Cretaceous reservoirs. Here the Permian input decreases up section (Hutton 70%, Birkhead 65%, McKinlay 60%) with the Permian Toolachee Formation and Jurassic Birkhead Formation being the likely source rocks. The minimum migration distance for the oil sourced within the Birkhead Formation is 4-5 km from the west and ~24 km from the east.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Earth and Environmental Sciences, 2005
Ryan, S. J. "The geology and genesis of the polymetallic Wagga Tank prospect, Mount Hope, N.S.W." Thesis, 1987. http://hdl.handle.net/2440/105306.
Повний текст джерелаThe Wagga Tank Prospect is located in Central Western N.S. W, 125 km south of Cobar. The prospect is hosted by the Lower Devonian Mount Hope Group, a complex succession of sedimentary, felsic volcanic and comagmatic intrusive rocks representing the oldest division of the Cobar Supergroup in the Mount Hope area. The prospect is primarily a Pb and Zn deposit with minor Cu, Ag and significant Au. Gold values are highest within steeply dipping gossan shoots in the oxidised zone, while Pb and Zn values are highest in subvertical shoots of massive sulphide within the primary zone. Cu is concentrated as chalcocite, digenite and malachite at a zone of supergene enrichment. The primary mineralization occurs within a zone of intense tectonic brecciation and argillic alteration at a pronounced flexure along the steeply dipping contact between the volcaniclastic sequence and a siltstone - slate sequence. The mineralization can be divided into two categories on the basis of textural relationships, i.e. fine grained, crudely banded massive type sulphides and coarser grained vein type sulphides. The vein type sulphides are represented by varying proportions of pyrite, chalcopyrite, sphalerite and galena with rare inclusions of cubanite and pyrrhotite. The massive type sulphides show mineral abundances of pyrite>sphalerite>galena>>chalcopyri te. Fluid inclusion and chlorite data indicate that the mineralizing fluid reached temperatures of about 325°C. Sulphur isotope compositions of the sulphide minerals (delta 34S = 10 per mil) suggest that the sulphur originated from seawater SO4-2. Reduction of seawater SO4-2 to H2S was primarily by an inorganic process at elevated temperatures in a heated rock pile. Thermodynamic calculations suggest possible log f02 - pH constraints of about log f02 = -29. 5 to -31. 7 and pH = 3 to 4. 5 for the mineralizing fluid. The mineralization is considered to be of epigenetic hydrothermal origin. The hydrothermal fluid was probably derived from dewatering of the rock pile during metamorphism accompanying the major deformation. Sulphide precipitation occurred along a plane of high permeability produced by folding of adjacent beds with a contrasting competency. The prospect bears many similarities to the principal deposits in the Cobar area. Those deposits are typically narrow steeply plunging elongate bodies occurring along sheared or brecciated contacts between cleaved turbiditic siltstones and coarser clastic beds or felsic volcanics.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Physical Sciences, 1987
Jagodzinski, E. "The geology of the Gawler Range Volcanics in the Toondulya Bluff area and U-Pb dating of the Yardea Dacite at Lake Acraman." Thesis, 1985. http://hdl.handle.net/2440/86564.
Повний текст джерелаAt Toondulya Bluff a sequence of 'older' Gawler Range Volcanics dip in an easterly direction beneath the overlying Yardea Dacite, and are intruded by the comagmatic Hiltaba Granite. The volcanics occur as a series of tuffs and lava flows. Geochemical evidence suggests these volcanics are related to each other by fractional crystallisation, with plagioclase, clinopyroxene, K-feldspar and titan-magnetite, and accessory zircon and apatite controlling differentiation trends. The Si-rich Hiltaba Granite and Yardea Dacite formed from the final, highly fractionated melts. Geothermometry suggests the volcanic and granite crystallised at temperatures within the range 680deg-850degC. The initial magma from which the lithologies were derived, was formed by partial melting of a lower crustal source probably of granulitic composition. Lake Acraman is believed to have been a site of meteoritic impact in the late Proterozoic (~600 Ma ago). Fragments of dacitic ejecta have been identified within the Bunyeroo Formation, Flinders Ranges and dating of these fragments gives an age of c.1575 Ma using single zircon ion probe dating techniques (Gostin et al in prep.). U/Pb dating of the Yardea Dacite at Lake Acraman reveals it to be of comparable age to these fragments (1603-1631 Ma). The lower intercept of the discordia line reveals there has been no resetting of the U/Pb system in response to the postulated meteoritic impact.
Thesis (B.Sc.(Hons)) -- University of Adelaide, School of Earth and Environmental Sciences, 1985
Книги з теми "Honours; Geology"
London, Geological Society of, ed. Geology of the earthquake source: A volume in honour of Rick Sibson. London: Geological Society, 2011.
Знайти повний текст джерела1934-, Verma V. K., Arun Kumar, Kushwaha R. S, and Thakur Baleshwar, eds. Earth system sciences: Felicitation volumes in honour of Professor V.K. Verma. New Delhi: Concept Pub. Co., 2009.
Знайти повний текст джерелаGermany) International Hanns Bruno Geinitz Symposium (2000 Dresden. International Hanns Bruno Geinitz Symposium: Proceedings of the symposium in honour of Hanns Bruno Geinitz, Dresden, Saxony, January 28-30, 2000. Edited by Geinitz Hanns Bruno 1814-1900 and Lange Jan-Michael. Dresden: Staatliche Naturhistorische Sammlungen, Museum für Mineralogie und Geologie, 2000.
Знайти повний текст джерелаH, Osborne Robert, ed. From shoreline to abyss: Contributions in marine geology in honor of Francis Parker Shepard. Tulsa, Okla: SEPM (Society for Sedimentary Geology), 1991.
Знайти повний текст джерела1902-, Chakravarti D. K., and Bhattacharya A. K. 1928-, eds. Proceedings of Indian Geological IVth Session Congress, Varanasi, 1982: A volume in honour of Prof. D.K. Chakravarti. New Delhi: Today & Tomorrow's Printers and Publishers, 1985.
Знайти повний текст джерелаJ, Aumann Robert, and Wooders Myrna Holtz, eds. Topics in mathematical economics and game theory: Essays in honor of Robert J. Aumann. Providence, RI: American Mathematical Society, 1999.
Знайти повний текст джерелаSEPM (Society for Sedimentary Geology) and SEPM (Society for Sedimentary Geology). North American Micropaleontology Section, eds. Geologic problem solving with microfossils: A volume in honor of Garry D. Jones. Tulsa , Okla: SEPM (Society for Sedimentary Geology), 2009.
Знайти повний текст джерелаSassi, F. P. The abundance of 55 elements and petrovolumetric models of the crust in 9 type areas from the crystalline basements of Italy with some geophysical and petrophisycal data: In honor of Bruno Zanettin on the occasion of his 80th birthday. Edited by Zanettin Bruno. Roma: Accademia nazionale delle scienze detta deiXL, 2003.
Знайти повний текст джерела1899-, Korzhinskiĭ Dmitriĭ Sergeevich, and Perchuk L. L, eds. Progress in metamorphic and magmatic petrology: A memorial volume in honor of D.S. Korzhinskiy. Cambridge [England]: Cambridge University Press, 1991.
Знайти повний текст джерелаListing of thesis titles by keyword: B.Sc (honours), M.Sc, and Ph.D. : James Cook University of North Queensland, Geology Department, 1969-1985. [Townsville, Qld.]: Geology Dept., James Cook University of North Queensland, 1986.
Знайти повний текст джерелаЧастини книг з теми "Honours; Geology"
Good, Gregory A. "John Herschel’s Geology: The Cape of Good Hope in the 1830s." In The Romance of Science: Essays in Honour of Trevor H. Levere, 135–50. Cham: Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-58436-2_8.
Повний текст джерелаNēmec, Václav. "Introduction." In Computers in Geology - 25 Years of Progress. Oxford University Press, 1994. http://dx.doi.org/10.1093/oso/9780195085938.003.0006.
Повний текст джерелаEmery, K. O., and David A. Ross. "Past and Future Evolution of Marine Geology." In From Shoreline to AbyssContributions in Marine Geology in Honor of Francis Parker Shepard. SEPM Society for Sedimentary Geology, 1991. http://dx.doi.org/10.2110/pec.91.09.0011.
Повний текст джерелаBushey, Jonathan C., Arthur W. Snoke, Calvin G. Barnes, and Carol D. Frost. "Geology of the Bear Mountain intrusive complex, Klamath Mountains, California." In Geological Studies in the Klamath Mountains Province, California and Oregon: A volume in honor of William P. Irwin. Geological Society of America, 2006. http://dx.doi.org/10.1130/2006.2410(14).
Повний текст джерелаDEMCHUK, THOMAS D., and ANTHONY C. GARY. "Geologic Problem Solving with Microfossils: A Volume in Honor of Garry D. Jones." In Geologic Problem Solving with Microfossils, 5–6. SEPM (Society for Sedimentary Geology), 2009. http://dx.doi.org/10.2110/sepmsp.093.005.
Повний текст джерелаCallahan, O. A., Peter Eichhubl, and J. R. Kyle. "Geology and hydromechanical properties of the basement-sediment interface, Llano Uplift, Central Texas." In The Geologic Basement of Texas: A Volume in Honor of Peter T. Flawn. University of Texas at Austin, Bureau of Economic Geology, 2021. http://dx.doi.org/10.23867/ri0286c8.
Повний текст джерелаCallahan, O. A., K. M. Smye, E. A. Horne, Peter Eichhubl, and Carolyn Breton. "The structure of the geologic basement in Texas." In The Geologic Basement of Texas: A Volume in Honor of Peter T. Flawn. University of Texas at Austin, Bureau of Economic Geology, 2021. http://dx.doi.org/10.23867/ri0286c2.
Повний текст джерелаSavvaidis, Alexandros, P. H. Hennings, Cliff Frohlich, Peter Eichhubl, E. A. Horne, Dino Huang, and O. A. Callahan. "Seismogenic environment of the geologic basement of Texas." In The Geologic Basement of Texas: A Volume in Honor of Peter T. Flawn. University of Texas at Austin, Bureau of Economic Geology, 2021. http://dx.doi.org/10.23867/ri0286c9.
Повний текст джерелаPeterson, Curt D., Mark E. Darienzo, Don J. Pettit, Phillip L. Jackson, and Charles L. Rosenfeld. "Littoral-Cell Development in the Convergent Cascadia Margin of the Pacific Northwest, USA." In From Shoreline to AbyssContributions in Marine Geology in Honor of Francis Parker Shepard. SEPM Society for Sedimentary Geology, 1991. http://dx.doi.org/10.2110/pec.91.09.0017.
Повний текст джерелаBest, Tim C., and Gary B. Griggs. "A Sediment Budget for the Santa Cruz Littoral Cell, California." In From Shoreline to AbyssContributions in Marine Geology in Honor of Francis Parker Shepard. SEPM Society for Sedimentary Geology, 1991. http://dx.doi.org/10.2110/pec.91.09.0035.
Повний текст джерелаТези доповідей конференцій з теми "Honours; Geology"
Bodalski, Joe, Victoria Deniken, Matt King, and Daniel Childers. "PHYSICAL GEOLOGY HONORS PROJECT: USING GIS TO MAP THE DELAWARE COUNTY COMMUNITY COLLEGE CAMPUS LANDSCAPE." In 67th Annual Southeastern GSA Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018se-310678.
Повний текст джерелаChilders, Daniel. "UNDERGRADUATE STUDENT RESEARCH ON A SHOESTRING BUDGET: GEOLOGY HONORS OPTION AT DELAWARE COUNTY COMMUNITY COLLEGE." In 67th Annual Southeastern GSA Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018se-311413.
Повний текст джерелаPhillips, C. Dianne, and Nathan Sorey. "USING ESRI ONLINE APPLICATIONS AND GEOSCIENCE DATA IN CAPSTONE PROJECTS FOR HONORS GEOLOGY: 2Y COLLEGE." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-300995.
Повний текст джерелаMcGarvey, Aaron, Kelly Monaghan, Erin McCone, and Daniel P. Childers. "STREAM PROJECT BY PHYSICAL GEOLOGY HONOR STUDENTS AT DELAWARE COUNTY COMMUNITY COLLEGE." In Joint 52nd Northeastern Annual Section and 51st North-Central Annual GSA Section Meeting - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017ne-291138.
Повний текст джерелаMcCone, Erin, Kelly Monaghan, Aaron McGarvey, and Daniel P. Childers. "STREAM PROJECT BY PHYSICAL GEOLOGY HONOR STUDENTS AT DELAWARE COUNTY COMMUNITY COLLEGE." In 66th Annual GSA Southeastern Section Meeting - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017se-291102.
Повний текст джерелаPandey, Vibhas J. "Applications of Geomechanics to Hydraulic Fracturing - Case Studies from Coal Stimulations." In SPE Hydraulic Fracturing Technology Conference. SPE, 2015. http://dx.doi.org/10.2118/spe-173378-ms.
Повний текст джерелаOliveira, Jansen, Karl Perez H., Alejandro Martin V., Ricard Fernandez T., Teresa Polo N., Lorenzo Villalobos V., Francois Xavier Dubost, et al. "DEEP TRANSIENT TESTING DIGITAL PRODUCTS CREATE NOVEL REAL-TIME RESERVOIR INSIGHTS." In 2021 SPWLA 62nd Annual Logging Symposium Online. Society of Petrophysicists and Well Log Analysts, 2021. http://dx.doi.org/10.30632/spwla-2021-0027.
Повний текст джерелаHernandez, Erika, Suzanne Boekhout, Gijs van Essen, Bert-Rik de Zwart, Nuha Al-Sultan, Basel Al-Otaibi, Adrian Crawford, Michael Obermaier, and Ben Dewever. "The Sabriyah Mauddud Dynamic Model Rebuild – Tackling the History Match of a Giant and Complex Carbonate Reservoir Through a Tailored-Made Sector-Centered History Match Approach." In SPE Reservoir Characterisation and Simulation Conference and Exhibition. SPE, 2023. http://dx.doi.org/10.2118/212586-ms.
Повний текст джерелаAlqallabi, Salahaldeen, Abdul Saboor Khan, Anish Phade, Mohamed Tarik Gacem, Mustapha Adli, Faisal Al-Jenaibi, Sheharyar Mansur, Lyes Malla, and Dario Benedictis. "An Integrated Ensemble-Based Uncertainty Centric Approach to Address Multi-Disciplinary Reservoir Challenges While Accelerating Subsurface Modeling Process in an Onshore Field, Abu Dhabi, UAE." In SPE Annual Technical Conference and Exhibition. SPE, 2021. http://dx.doi.org/10.2118/205854-ms.
Повний текст джерелаAshayeri, Cyrus, and Birendra Jha. "Assessment of Unconventional Resources Opportunities in the Middle East Tethyan Petroleum System in a Transfer Learning Context." In Abu Dhabi International Petroleum Exhibition & Conference. SPE, 2021. http://dx.doi.org/10.2118/207723-ms.
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