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Статті в журналах з теми "Metamorphism (Geology) New South Wales"
Ward, Colin R., Peter R. Warbrooke, and F. Ivor Roberts. "Geochemical and mineralogical changes in a coal seam due to contact metamorphism, Sydney Basin, New South Wales, Australia." International Journal of Coal Geology 11, no. 2 (March 1989): 105–25. http://dx.doi.org/10.1016/0166-5162(89)90001-3.
Повний текст джерелаHendrickx, Marc. "Fibrous Tremolite in Central New South Wales, Australia." Environmental and Engineering Geoscience 26, no. 1 (February 20, 2020): 73–77. http://dx.doi.org/10.2113/eeg-2273.
Повний текст джерелаPacey, Adam, Jamie J. Wilkinson, and David R. Cooke. "Chlorite and Epidote Mineral Chemistry in Porphyry Ore Systems: A Case Study of the Northparkes District, New South Wales, Australia." Economic Geology 115, no. 4 (June 1, 2020): 701–27. http://dx.doi.org/10.5382/econgeo.4700.
Повний текст джерелаRoper, H. "Superposed structures in the Mona Complex at Rhoscolyi Ynys Gybi, North Wales." Geological Magazine 129, no. 4 (July 1992): 475–90. http://dx.doi.org/10.1017/s0016756800019567.
Повний текст джерелаKinny, P. D., E. C. Leitch, and T. G. Vallance. "Thermal metamorphism near Willi Willi, New South Wales." Australian Journal of Earth Sciences 32, no. 4 (December 1985): 333–42. http://dx.doi.org/10.1080/08120098508729336.
Повний текст джерелаBevins, R. E., S. C. White, and D. Robinson. "The South Wales Coalfield: low grade metamorphism in a foreland basin setting?" Geological Magazine 133, no. 06 (November 1996): 739. http://dx.doi.org/10.1017/s0016756800024584.
Повний текст джерелаBryant, E. A., and R. W. Young. "Bedrock-Sculpturing by Tsunami, South Coast New South Wales, Australia." Journal of Geology 104, no. 5 (September 1996): 565–82. http://dx.doi.org/10.1086/629852.
Повний текст джерелаCarr, Paul, Malcolm Southwood, and Jeff Chen. "Fluorapatite from Broken Hill, New South Wales, Australia." Rocks & Minerals 97, no. 1 (December 20, 2021): 16–27. http://dx.doi.org/10.1080/00357529.2022.1989948.
Повний текст джерелаOch, D. J., E. C. Leitch, G. Caprarelli, and T. Watanabe. "Blueschist and eclogite in tectonic melange, Port Macquarie, New South Wales, Australia." Mineralogical Magazine 67, no. 4 (August 2003): 609–24. http://dx.doi.org/10.1180/0026461036740121.
Повний текст джерелаMcIntyre, J. I. "Northwestern New South Wales regional magnetics and gravity." Exploration Geophysics 22, no. 2 (June 1991): 261–64. http://dx.doi.org/10.1071/eg991261.
Повний текст джерелаДисертації з теми "Metamorphism (Geology) New South Wales"
Stevenson, Ross Kelley. "Implications of amazonite to sulfide-silicate equilibria." Thesis, McGill University, 1985. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=63377.
Повний текст джерелаPucillo, Kevin. "Quaternary palaeochannel evolution and groundwater movement in the Coleambally Irrigation District of New South Wales." School of Earth and Environmental Sciences - Faculty of Science, 2005. http://ro.uow.edu.au/theses/406.
Повний текст джерелаFanning, Patricia C. "Beyond the divide: a new geoarchaeology of Aboriginal stone artefact scatters in Western NSW, Australia." Australia : Macquarie University, 2002. http://hdl.handle.net/1959.14/45010.
Повний текст джерелаIncludes bibliographical references: p. 228-232.
Geomorphology, archaeology and geoarchaeology: introduction and background -- Surface stone artefact scatters: why can we see them? -- Geomorphic controls on spatial patterning of the surface stone artefact record -- A temporal framework for interpreting surface artefact scatters in Western NSW -- Synthesis: stone artefact scatters in a dynamic landscape.
Surface scatters of stone artefacts are the most ubiquitous feature of the Australian Aboriginal archaeological record, yet the most underutilized by archaeologists in developing models of Aboriginal prehistory. Among the many reasons for this are the lack of understanding of geomorphic processes that have exposed them, and the lack of a suitable chronological framework for investigating Aboriginal 'use of place'. This thesis addresses both of these issues. -- In arid western NSW, erosion and deposition accelerated as a result of the introduction of sheep grazing in the mid 1800s has resulted in exposure of artefact scatters in some areas, burial in others, and complete removal in those parts of the landscape subject to concentrated flood flows. The result is a patchwork of artefact scatters exhibiting various degrees of preservation, exposure and visibility. My research at Stud Creek, in Sturt National Park in far western NSW, develops artefact and landscape survey protocols to accommodate this dynamic geomorphic setting. A sampling strategy stratified on the basis of landscape morphodynamics is presented that allows archaeologists to target areas of maximum artefact exposure and minimum post-discard disturbance. Differential artefact visibility at the time of the survey is accommodated by incorporating measures of surface cover which quantify the effects of various ephemeral environmental processes, such as deposition of sediments, vegetation growth, and bioturbation, on artefact count. -- While surface stone artefact scatters lack the stratigraphy usually considered necessary for establishing the timing of Aboriginal occupation, a combination of radiocarbon determinations on associated heat-retainer ovens, and stratigraphic analysis and dating of the valley fills which underlie the scatters, allows a two-stage chronology for huntergatherer activity to be developed. In the Stud Creek study area, dating of the valley fill by OSL established a maximum age of 2,040±100 y for surface artefact scatters. The heatretainer ovens ranged in age from 1630±30 y BP to 220±55 y BP. Bayesian statistical analysis of the sample of 28 radiocarbon determinations supported the notion, already established from analysis of the artefacts, that the Stud Creek valley was occupied intermittently for short durations over a relatively long period of time, rather than intensively occupied at any one time. Furthermore, a gap in oven building between about 800 and 1100 years ago was evident. Environmental explanations for this gap are explored, but the paiaeoenvironmental record for this part of the Australian arid zone is too sparse and too coarse to provide explanations of human behaviour on time scales of just a few hundred years. -- Having established a model for Stud Creek of episodic landscape change throughout the late Pleistocene and Holocene, right up to European contact, its veracity was evaluated in a pilot study at another location within the region. The length of the archaeological record preserved in three geomorphically distinct locations at Fowlers Gap, 250 km south of Stud Creek, is a function of geomorphic dynamics, with a record of a few hundred years from sites located on channel margins and low terraces, and the longest record thus far of around 5,000 years from high terrace surfaces more remote from active channel incision. But even here, the record is not continuous, and like Stud Creek, the gaps are interpreted to indicate that Aboriginal people moved into and out of these places intermittently throughout the mid to late Holocene. -- I conclude that episodic nonequilibrium characterizes the geomorphic history of these arid landscapes, with impacts on the preservation of the archaeological record. Dating of both archaeological and landform features shows that the landscape, and the archaeological record it preserves, are both spatially and temporally disjointed. Models of Aboriginal hunter-gatherer behaviour and settlement patterns must take account of these discontinuities in an archaeological record that is controlled by geomorphic activity. -- I propose a new geoarchaeological framework for landscape-based studies of surface artefact scatters that incorporates geomorphic analysis and dating of landscapes, as well as tool typology, into the interpretation of spatial and temporal patterns of Aboriginal huntergatherer 'use of place'.
Mode of access: World Wide Web.
vii, 232 p. ill., maps
Nunt-jaruwong, Sorawit School of Biological Earth & Environmental Sciences UNSW. "Engineering geology of the Patonga Claystone, Central Coast, New South Wales, with particular reference to slaking behaviour." Awarded by:University of New South Wales. School of Biological, Earth and Environmental Sciences, 2006. http://handle.unsw.edu.au/1959.4/27335.
Повний текст джерелаWalker, Thomas Bradley. "BEDROCK GEOLOGY AND TECTONIC EVOLUTION OF THE WESTERN CENTRAL MAINE ZONE, SOUTH CENTRAL MASSACHUSETTS." UKnowledge, 2011. http://uknowledge.uky.edu/ees_etds/1.
Повний текст джерелаScott, Justin Robert. "Fractal and multifractal fault simulation : application using soft data and analogues at Wyong, New South Wales, Australia /." [St. Lucia, Qld.], 2005. http://www.library.uq.edu.au/pdfserve.php?image=thesisabs/absthe19562.pdf.
Повний текст джерелаGuo, Bin. "An integrated geophysical investigation of the Tamworth Belt and its bounding faults." Phd thesis, Australia : Macquarie University, 2005. http://hdl.handle.net/1959.14/13240.
Повний текст джерелаBibliography: leaves 202-224.
Introduction -- Geological setting of the New England Fold Belt -- Regional geophysical investigation -- Data acquisition and reduction -- Modelling and interpretation of magnetic data over the Peel Fault -- Modelling and interpretation of magnetic data over the Mooki Fault -- Gravity modelling of the Tamworth Belt and Gunnedah Basin -- Interpretation and discussion -- Conclusions.
This thesis presents new magnetic and gravity data for the Southern New England Fold Belt (SNEFB) and the Gunnedah Basin that adjoins to the west along the Mooki Fault in New South Wales. The SNEFB consists of the Tamworth Belt and Tablelands Complex that are separated by the Peel Fault. The Tablelands Complex to the east of the Peel Fault represents an accretionary wedge, and the Tamworth Belt to the west corresponds to the forearc basin. A total of five east-north-east trending gravity profiles with around 450 readings were conducted across the Tamworth Belt and Gunnedah Basin. Seven ground magnetic traverses of a total length of 60 km were surveyed across the bounding faults of the Tamworth belt, of which five were across the Peel Fault and two were across the Mooki Fault. The gravity data shows two distinct large positive anomalies, one over the Tamworth Belt, known as the Namoi Gravity High and another within the Gunnedah Basin, known as the Meandarra Gravity Ridge. All gravity profiles show similarity to each other. The magnetic data displays one distinct anomaly associated with the Peel Fault and an anomaly immediately east of the Mooki Fault. These new potential field data are used to better constrain the orientation of the Peel and Mooki Faults as well as the subsurface geometry of the Tamworth Belt and Gunnedah Basin, integrating with the published seismic data, geologic observations and new physical properties data. --Magnetic anomalies produced by the serpentinite associated with the Peel Fault were used to determine the orientation of the Peel fault. Five ground magnetic traverses were modelled to get the subsurface geometry of the serpentinite body. Modelling results of the magnetic anomalies across the Peel Fault indicate that the serpentinite body can be mostly modelled as subvertical to steeply eastward dipping tabular bodies with a minimum depth extent of 1-3 km, although the modelling does not constrain the vertical extent. This is consistent with the modelling of the magnetic traverses extracted from aeromagnetic data. Sensitivity analysis of a tabular magnetic body reveals that a minimum susceptibility of 4000x10⁻⁶cgs is needed to generate the observed high amplitude anomalies of around 2000 nT, which is consistent with the susceptibility measurements of serpentinite samples along the Peel Fault ranging from 2000 to 9000 x 10⁻⁶ cgs. Rock magnetic study indicates that the serpentinite retains a strong remanence at some locations. This remanence is a viscous remanent magnetisation (VRM) which is parallel to the present Earth's magnetic field, and explains the large anomaly amplitude over the Peel fault at these locations. The remanence of serpentinite at other localities is not consistent enough to contribute to the observed magnetic anomalies. A much greater depth extent of the Peel Fault was inferred from gravity models. It is proposed that the serpentinite along the Peel Fault was emplaced as a slice of oceanic floor that has been accreted to the front of the arc, or as diapirs rising off the serpentinised part of the mantle wedge above the supra subduction zone.
Magnetic anomalies immediately east of the Mooki Fault once suggested to be produced by a dyke-like body emplaced along the fault were modelled along two ground magnetic traverses and three extracted aeromagnetic lines. Modelling results indicate that the anomalies can be modelled as an east-dipping overturned western limb of an anticline formed as a result of a fault-propagation fold with a shallow thrust step-up angle from the décollement. Interpretation of aeromagnetic data and modelling of the magnetic traverses indicate that the anomalies along the Mooki Fault are produced by the susceptibility contrast between the high magnetic Late Carboniferous Currabubula Formation and/or Early Permian volcanic rocks of the Tamworth Belt and the less magnetic Late Permian-Triassic Sydney-Gunnedah Basin rocks. Gravity modelling indicates that the Mooki Fault has a shallow dip ( ̃25°) to the east. Modelling of the five gravity profiles shows that the Tamworth Belt is thrust westward over the Sydney-Gunnedah Basin for 15-30 km. --The Meandarra Gravity Ridge within the Gunnedah Basin was modelled as a high density volcanic rock unit with a density contrast of 0.25 tm⁻³, compared to the rocks of the Lachlan Fold Belt in all profiles. The volcanic rock unit has a steep western margin and a gently dipping eastern margin with a thickness ranging from 4.5-6 km, and has been generally agreed to have formed within an extensional basin. --The Tamworth Belt, being mainly the product of volcanism of mafic character and thus has high density units, together with the high density Woolomin Association, which is composed chiefly of chert/jasper, basalt, dolerite and metabasalt, produces the Namoi Gravity High. Gravity modelling results indicate that the anomaly over the Tamworth Belt can be modelled as either a configuration where the Tablelands Complex extends westward underthrusting the Tamworth Belt, or a configuration where the Tablelands Complex has been thrust over the Tamworth Belt. When the gravity profiles were modelled with the first configuration, the Peel Fault with a depth extent of around 1 km can only be modelled for the Manilla and Quirindi profiles, modelling of the rest of the gravity profiles indicates that the Tablelands Complex underthrust beneath the Tamworth belt at a much deeper location.
Mode of access: World Wide Web.
xi, 242 leaves ill., maps
Othman, Rushdy School of Biological Earth & 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.
Повний текст джерелаPurdy, David John. "Volcanic stratigraphy and origin of the Wallangarra Volcanics, Wandsworth volcanic group, northern NSW, Australia." Thesis, Queensland University of Technology, 2003.
Знайти повний текст джерелаHenry, Amber Dawn. "Fracture reactivation and gold mineralization in the epithermal environment : structural evolution of the Endeavour 42 gold deposit, New South Wales, Australia." Thesis, University of British Columbia, 2008. http://hdl.handle.net/2429/1192.
Повний текст джерелаКниги з теми "Metamorphism (Geology) New South Wales"
Percival, Ian G. The geological heritage of New South Wales. Sydney, N.S.W: New South Wales Govt., National Parks and Wildlife Service, published on behalf of the Geological Sites and Monuments Sub-Committee of the Geological Society of Australia (New South Wales Division), 1985.
Знайти повний текст джерелаIngram, F. T. Petroleum prospectivity of the Clarence-Moreton Basin in New South Wales. [Sydney?]: Dept. of Mineral Resources, 1996.
Знайти повний текст джерелаSutherland, Lin. Geology of Barrington Tops Plateau: Its rocks, minerals and gemstones, New South Wales, Australia. Sydney, N.S.W: Australian Museum Society, 2003.
Знайти повний текст джерелаG, Barnes Robert. Metallogenic studies of the Broken Hill and Euriowie Blocks, New South Wales. [Sydney, N.S.W.]: Dept. of Mineral Resources, Geological Survey of New South Wales, 1988.
Знайти повний текст джерелаAbell, Robert Sebastian. Geology of the Canberra 1:100 000 sheet area, New South Wales, and Australian Capital Territory. Canberra: Australian Govt. Pub. Service, 1991.
Знайти повний текст джерелаBurger, D. Stratigraphy, palynology, and palaeoenvironments of the Hooray Sandstone, eastern Eromanga Basin, Queensland and New South Wales. [Brisbane]: Queensland Dept. of Mines, 1989.
Знайти повний текст джерелаGeology and Coal Mining Conference (1987 Sydney, N.S.W.). Geology and Coal Mining Conference proceedings: 13-15 October 1987, New South Wales Institute of Technology, Sydney. Sydney: Geological Society of Australia, 1987.
Знайти повний текст джерелаAustralian Beach Safety and Management Program., Surf Life Saving Australia, and University of Sydney. Coastal Studies Unit., eds. Beaches of the New South Wales coast: A guide to their nature, characteristics, surf and safety. 2nd ed. Sydney: Sydney University Press, 2007.
Знайти повний текст джерелаColwell, James B. Rig seismic research cruise 13: Structure and stratigraphy of the northeast Gippsland Basin and southern New South Wales margin : initial report. Canberra: Australian Govt. Pub. Service, 1987.
Знайти повний текст джерелаColwell, James B. Rig seismic research cruise 13: Structure and stratigraphy of the northeast Gippsland Basin and southern New South Wales margin : initial report. Canberra: Australian Government Publishing Service, 1987.
Знайти повний текст джерелаЧастини книг з теми "Metamorphism (Geology) New South Wales"
Gratchev, Ivan, Sinnappoo Ravindran, Dong Hyun Kim, Chen Cui, and Qianhao Tang. "Mechanisms of Shallow Rainfall-Induced Landslides from Australia: Insights into Field and Laboratory Investigations." In Progress in Landslide Research and Technology, Volume 1 Issue 1, 2022, 113–22. Cham: Springer International Publishing, 2023. http://dx.doi.org/10.1007/978-3-031-16898-7_7.
Повний текст джерелаHarris, Anthony C., David R. Cooke, Ana Liza Garcia Cuison, Malissa Groome, Alan J. Wilson, Nathan Fox, John Holliday, and Richard Tosdal. "Chapter 30: Geologic Evolution of Late Ordovician to Early Silurian Alkalic Porphyry Au-Cu Deposits at Cadia, New South Wales, Australia." In Geology of the World’s Major Gold Deposits and Provinces, 621–43. Society of Economic Geologists, 2020. http://dx.doi.org/10.5382/sp.23.30.
Повний текст джерелаFedkin, Valentin V., Theodore D. Burlick, Mary L. Leech, Andrey A. Shchipansky, Peter M. Valizer, and W. G. Ernst. "Petrotectonic origin of mafic eclogites from the Maksyutov subduction complex, south Ural Mountains, Russia." In Plate Tectonics, Ophiolites, and Societal Significance of Geology: A Celebration of the Career of Eldridge Moores. Geological Society of America, 2021. http://dx.doi.org/10.1130/2021.2552(09).
Повний текст джерела