Relevant bibliographies by topics / Metamorphism (Geology) New South Wales Broken Hill

Academic literature on the topic 'Metamorphism (Geology) New South Wales Broken Hill'

Author: Grafiati
Published: 10 December 2022
Last updated: 28 January 2023

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Journal articles on the topic "Metamorphism (Geology) New South Wales Broken Hill"

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Carr, 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.

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2

Birch, William D. "Broken Hill New South Wales, Australia: Its Contribution to Mineralogy." Rocks & Minerals 82, no. 1 (January 2007): 40–49. http://dx.doi.org/10.3200/rmin.82.1.40-49.

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Parr, Joanna. "The preservation of pre-metamorphic colloform banding in pyrite from the Broken Hill-type Pinnacles deposit, New South Wales, Australia." Mineralogical Magazine 58, no. 392 (September 1994): 461–71. http://dx.doi.org/10.1180/minmag.1994.058.392.11.

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AbstractTwo distinct generations of pyrite, with different morphologies, are described from the Proterozoic Broken Hill-type Pinnacles deposit in western NSW. The earlier, py1, forms concentric layers interpreted as colloform banding. Although the textures are somewhat similar to those observed in supergene alteration zones, textural relationships in fresh rocks suggest that these are pre-metamorphic and that the pyrite formed as the result of precipitation from hydrothermal fluids in open veins, vugs and fissures. The second generation, py2, post-dates py1 and forms euhedral overgrowths on it. It is interpreted as being synchronous with the main phase of base metal sulphide mineralisation. The textures reported here are previously unrecorded for Broken Hill-type mineralisation, and have implications for the regional identification of feeder zones to the Broken Hill deposit. The evidence supports a model in which mineralising conditions at the Pinnacles were characterised by slightly higher oxygen and lower sulphur fugacity (further constrained by Fe contents of sphalerite) than at Broken Hill, where pyrrhotite is the major Fe sulphide.The pre-metamorphic textures observed in the pyrite at the Pinnacles deposit are also unusual because they have survived granulite facies metamorphism and five phases of deformation, whereas previously the preservation of such textures has not been recognised at metamorphic grades greater than amphibolite facies.
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Parr, Joanna M., Brian P. J. Stevens, Graham R. Carr, and Rodney W. Page. "Subseafloor origin for Broken Hill Pb-Zn-Ag mineralization, New South Wales, Australia." Geology 32, no. 7 (2004): 589. http://dx.doi.org/10.1130/g20358.1.

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STEVENS, B., R. BARNES, R. BROWN, W. STROUD, and I. WILLIS. "The Willyama Supergroup in the Broken Hill and Euriowie Blocks, New South Wales." Precambrian Research 40-41 (October 1988): 297–327. http://dx.doi.org/10.1016/0301-9268(88)90073-3.

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James, S. D., J. A. Pearce, and R. A. Oliver. "The Geochemistry of the Lower Proterozoic Willyama Complex Volcanics, Broken Hill Block, New South Wales." Geological Society, London, Special Publications 33, no. 1 (1987): 395–408. http://dx.doi.org/10.1144/gsl.sp.1987.033.01.27.

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7

Parr, Joanna M. "The geology of the Broken Hill-type Pinnacles Pb-Zn-Ag deposit, western New South Wales, Australia." Economic Geology 89, no. 4 (July 1, 1994): 778–90. http://dx.doi.org/10.2113/gsecongeo.89.4.778.

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8

Lavin, Owen P., and Ian Nichol. "Applications of some statistical techniques to weathered rock geochemical data from the Broken Hill area, New South Wales, Australia." Journal of Geochemical Exploration 40, no. 1-3 (August 1991): 427–51. http://dx.doi.org/10.1016/0375-6742(91)90051-u.

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Maidment, David W., George M. Gibson, and John W. Giddings. "Regional structure and distribution of magnetite: implications for the interpretation of aeromagnetic data in the Broken Hill region, New South Wales." Exploration Geophysics 31, no. 1-2 (March 2000): 8–16. http://dx.doi.org/10.1071/eg00008.

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10

Parr, Joanna M. "Rare-earth element distribution in exhalites associated with Broken Hill-type mineralisation at the Pinnacles deposit, New South Wales, Australia." Chemical Geology 100, no. 1-2 (October 1992): 73–91. http://dx.doi.org/10.1016/0009-2541(92)90103-c.

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Dissertations / Theses on the topic "Metamorphism (Geology) New South Wales Broken Hill"

1

Rutherford, Lachlan Stuart. "Developing a tectonic framework for the Southern Curnamona Cu - Au Province : geochemical and radiogenic isotope applications." 2006. http://hdl.handle.net/2440/37818.

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"Two independent geochronological techniques specifically targeting post-kinematic or late-stage growth of kyanite, staurolite and late-stage garnet in the southern Curnamona Province has found that these minerals grew during the Delamerian Orogeny (~530-500 Ma). Prograde metamorphism during the Delamerian Orogeny attained kyanite-staurolite-garnet grade (amphibolite-facies). Previous interpretations of an anticlockwise P-T path for the Olarian Orogeny need revising, as these interpretations have been shown in this study to be based on textural relationships spanning ~1100 million years. This highlights the importance of in situ geochronological techniques in defining robust P-T-t paths for a region." --p. 121 of source document.
Thesis (Ph.D.)--School of Earth and Environmental Sciences, 2006.
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Books on the topic "Metamorphism (Geology) New South Wales Broken Hill"

1

G, 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.

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