Добірка наукової літератури з теми "Granite New South Wales Broken Hill"
Оформте джерело за APA, MLA, Chicago, Harvard та іншими стилями
Ознайомтеся зі списками актуальних статей, книг, дисертацій, тез та інших наукових джерел на тему "Granite New South Wales Broken Hill".
Біля кожної праці в переліку літератури доступна кнопка «Додати до бібліографії». Скористайтеся нею – і ми автоматично оформимо бібліографічне посилання на обрану працю в потрібному вам стилі цитування: APA, MLA, «Гарвард», «Чикаго», «Ванкувер» тощо.
Також ви можете завантажити повний текст наукової публікації у форматі «.pdf» та прочитати онлайн анотацію до роботи, якщо відповідні параметри наявні в метаданих.
Статті в журналах з теми "Granite New South Wales Broken Hill"
Cooper, J. A., and K. R. Ludwig. "Inherited zircons in the Mundi Mundi Granite, Broken Hill, New South Wales." Australian Journal of Earth Sciences 32, no. 4 (December 1985): 467–70. http://dx.doi.org/10.1080/08120098508729344.
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 джерелаCarr, P. F., B. Selleck, M. Stott, and P. Williamson. "NATIVE LEAD AT BROKEN HILL, NEW SOUTH WALES, AUSTRALIA." Canadian Mineralogist 46, no. 1 (February 1, 2008): 73–85. http://dx.doi.org/10.3749/canmin.46.1.73.
Повний текст джерелаInegbenebor, A. I., P. A. Williams, R. E. Bevins, M. P. Lambert, and Alan D. Hart. "Composition of pyromorphites from Broken Hill, New South Wales." Records of the Australian Museum, Supplement 15 (October 16, 1992): 29–37. http://dx.doi.org/10.3853/j.0812-7387.15.1992.81.
Повний текст джерелаBirch, W. D. "Zinc-manganese carbonates from Broken Hill, New South Wales." Mineralogical Magazine 50, no. 355 (March 1986): 49–53. http://dx.doi.org/10.1180/minmag.1986.050.355.07.
Повний текст джерелаBirch, 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.
Повний текст джерелаMillsteed, Paul W. "Faceting Transparent Rhodonite from Broken Hill, New South Wales, Australia." Gems & Gemology 42, no. 2 (June 1, 2006): 151–58. http://dx.doi.org/10.5741/gems.42.2.151.
Повний текст джерелаMillsteed, P. W. "Marshite–miersile solid solution and iodargyrite from Broken Hill, New South Wales, Australia." Mineralogical Magazine 62, no. 04 (August 1998): 471–75. http://dx.doi.org/10.1180/002646198547846.
Повний текст джерелаYOUNG, GRANT M. "Neoproterozoic glaciation in the Broken Hill area, New South Wales, Australia." Geological Society of America Bulletin 104, no. 7 (July 1992): 840–50. http://dx.doi.org/10.1130/0016-7606(1992)104<0840:ngitbh>2.3.co;2.
Повний текст джерелаYellowlees, Peter M., and Anil V. Kaushik. "The Broken Hill Psychopathology Project." Australian & New Zealand Journal of Psychiatry 26, no. 2 (June 1992): 197–207. http://dx.doi.org/10.1177/000486749202600203.
Повний текст джерелаДисертації з теми "Granite New South Wales Broken Hill"
Wozga, Miroslaw Jacek. "Investigation of local fold plunge reversals present at Pasminco's Southern Operations, Broken Hill, New South Wales, Australia /." Title page, table of contents and abstract only, 1991. http://web4.library.adelaide.edu.au/theses/09SB/09sbw938.pdf.
Повний текст джерелаMouat, Jeremy. "Mining in the settler dominions : a comparative study of the industry in three communities from the 1880s to the First World War." Thesis, University of British Columbia, 1988. http://hdl.handle.net/2429/29037.
Повний текст джерелаArts, Faculty of
History, Department of
Graduate
Millsteed, Paul Wayne. "The role of halogens with sulfide melting at Broken Hill, New South Wales, Australia." Phd thesis, 2011. http://hdl.handle.net/1885/156321.
Повний текст джерелаHill, Steven Matthew. "The regolith and landscape evolution of the Broken Hill Block, Western New South Wales, Australia." Phd thesis, 2000. http://hdl.handle.net/1885/148039.
Повний текст джерелаElliott, Peter. "Crystal chemistry of cadmium oxysalt and associated minerals from Broken Hill, New South Wales." Thesis, 2010. http://hdl.handle.net/2440/65481.
Повний текст джерелаThesis (Ph.D.) -- University of Adelaide, School of Earth and Environmental Sciences, 2010
McGee, Tara Kathleen. "Shades of grey : community responses to chronic environmental lead contamination in Broken Hill, New South Wales." Phd thesis, 1996. http://hdl.handle.net/1885/11032.
Повний текст джерелаRutherford, 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.
Повний текст джерелаThesis (Ph.D.)--School of Earth and Environmental Sciences, 2006.
Downes, Peter M. "Sulfur- and lead-isotope signatures of selected middle Silurian to Carboniferous mineral systems of the Lachlan Orogen, eastern New South Wales - implications for metallogenesis." Thesis, 2009. http://hdl.handle.net/1959.13/916207.
Повний текст джерелаSulfur- and lead-isotope signatures for 64 deposits/systems located in the Central and Easternn Subprovinces of the Lachlan Orogen in eastern New South Wales were characterised in the present study. Here are presented four new ⁴⁰Ar/³⁹Ar dates, 644 new sulfur- and 105 new leadisotope analyses, plus a collation of 386 unpublished and 277 published sulfur isotope and over 560 unpublished and published lead isotope analyses for middle Silurian to Early Carboniferous mineralisation. Measured δ³⁴S values for 22 VHMS deposits range between -7.4‰ to 38.3‰. S-isotope values for Currawang East, Lewis Ponds, Mount Bulga, Belara and Accost (Group 1) range from - 1.7‰ to 5.9‰ with the ore-forming fluids for this group of deposits likely to have been reducing and sulfur derived largely from magmatic sources. By contrast, S-isotope signatures for sulfides from Black Springs, Calula, Captains Flat, Commonwealth, Cordillera, Gurrundah, Kempfield, Peelwood mine, Sunny Corner, The Glen, Wet Lagoon and Woodlawn (Group 2) have average δ³⁴S values between 5.4‰ and 8.1‰. These deposits appear to have formed from ore fluids that were more oxidising than those for Group 1 deposits, representing a mixed contribution of sulfur derived from partial reduction of seawater sulfate, in addition to sulfur from other sources. Four deposits, Elsinora, John Fardy, Mount Costigan and Stringers, have heavier average δ³⁴S signatures (10.1‰ to 13.2‰) than Group 2 deposits, suggesting that these deposits included a greater component of sulfur of seawater origin. The S-isotope data for barite from Black Springs, Commonwealth, Stringers, Gurrundah, Kempfield and Woodlawn range from 12.6‰ to 38.3‰. Over 80% of the δ³⁴S values are between 23.4‰ and 30.9‰, close to the previously published estimates for the composition of seawater sulfate during Late Silurian to earliest Devonian times, providing supporting evidence that these deposits formed concurrently with a Late Silurian volcanic event. New Pb isotope data for eleven VHMS deposits included in the present study support earlier Pb-isotope studies which indicate that lead was largely sourced from the host sequence. However, the data for Black Springs, Elsinora and Commonwealth indicate that some lead, included in these deposits, was sourced from units forming basement to the Silurian troughs. Sulfur isotope values for thirteen orogenic gold systems range between -7.5‰ and 16.1‰ (excluding outliers). The Wyoming One–Myall United system has an average δ³⁴S value of -5.5‰ and a primitive mantle-derived lead isotope signature implying that sulfur and gold were sourced from a fractionated mantle-derived intrusion. The δ-isotope data for Adelong, Bodangora, Calarie, Hargraves, Hill End, London–Victoria, Sebastopol, Sofala–Wattle Flat and Stuart Town are all very similar with average δ³⁴S values close to 0‰ (range -2.8 to 3.4‰). Sulfur in these deposits was derived from reduced fluids, sources from magmatic reservoirs either as a direct input or through dissolution and recycling of rock sulfide. For deposits hosted by the northern HET it is suggested that sulfur and gold were sourced from mantle-derived units located beneath the HET rather than the siliclastic fill of the trough itself. Windeyer and Napoleon Reefs have heavier S-isotope signatures suggesting a greater contribution of sulfur derived from reduced seawater sulfate reservoirs. Springfield, located adjacent to the northern HET, has the heaviest S-isotope signature (15.4 δ³⁴S‰) for orogenic gold deposits included in the present study. For this deposit it is suggested that HET-derived basinal fluids containing reduced seawater sulfate migrated along faults and leached gold from Ordovician mantle-derived units forming basement to that area. Seven sulfide-rich orogenic base metal deposits were included in the present study. Average δ³⁴S values for Currawang South, Frogmore, Montrose, Ruby Creek, Wallah Wallah vary between 3.5‰ and 6.0‰ (Group 1), with Kangiara, and Lucky Hit–Merrilla, having heavier average δ³⁴S values (10.0‰ and 8.2‰ respectively — Group 2). Group 1 deposits are small, and S-isotope signatures suggest significant sulfur was sourced from magmatic reservoirs; whereas, Group 2 deposits are larger and δ³⁴S signatures indicate a larger component of sulfur was derived from reduced seawater sulfate reservoirs. The Pb-isotope data for these deposits suggest that the majority of the lead was derived from older Ordovician and Silurian crustal reservoirs. The data for Mount Werong and Merrilla support a Middle Devonian Pb-model age; whereas, those for Wallah Wallah point to an Early Carboniferous Pb-model age. Browns Reef, in the Central Subprovince, is now interpreted to be a syn-deformational orogenic base metal deposit, for which the S-isotope data are similar to Group 2 orogenic base metal deposits and Pb-isotope data suggest lead was sourced from the fill of the Rast Trough. Five epithermal systems were included in the present study. Bauloora, Bowdens and those in the Yerranderie district are intermediate-sulfidation epithermal systems; whereas, Yalwal and Pambula are low sulfidation epithermal systems. Yerranderie, Yalwal, Pambula and Bauloora have δ³⁴S values close to 0‰. Sulfur in these deposits was derived largely from a magmatic reservoir. The Yerranderie system is zoned with respect to S-isotope distribution and shows mineralogical zonation along the Yerranderie Fault. Yalwal is zoned with 0‰ S-isotope values correlating with sericitic alteration assemblages and heavier S-isotope values (up to 17.9 δ³⁴S‰) correlating with assemblages that include minerals characteristic of argillic alteration. Sixteen middle Silurian to Early Devonian intrusion-related deposits were included in the present study. Collector, Dargues Reef, Mayfield, Ryans, Tallawang, Whipstick and Yambulla are located east of the I–S granite line, with Dargues Reef, Majors Creek, Mayfield, Whipstick and Yambulla hosted by or adjacent to their causative intrusion. These deposits have S-isotope signatures close to 0‰ (range -3.6‰ to 3.0‰) similar to that for granites east of the I–S line (range -1.5‰ to 4.9‰). The Pb-isotope data for these deposits includes both crustal- and mantle-derived lead. Deposits distal to their causative intrusions (Collector and Ryans) have heavier S-isotope signatures (7.7‰ and 4.3‰ respectively) indicating that some sulfur was probably sourced from the host sequence. The majority of lead, for these deposits, was sourced from the host sequence and/or older reservoirs. The S-isotope data for Tallawang suggest that the sulfur was largely sourced from the host sequence. Eight deposits are located to the west of the I–S line. Nasdaq, Phoenix, Tara, Rye Park and Mineral Hill have heavier S-isotope signatures (range: 2.6‰ to 7.3‰) which overlap with the range of values typical of granites located to the west of the I–S line (1.9 to 9.6‰) supporting the interpretation that the majority of sulfur was derived from the causative intrusion. The Pb-isotope data for Nasdaq, Mineral Hill and Tara suggest that lead originated from the host sequence or from older lead reservoirs; whereas, at Rye Park and Phoenix lead was probably sourced from the causative intrusion. Ardlethan and Browns Creek deposits have near 0‰ S-isotope signatures, lower than the range of δ³⁴S values for granites west of the I–S line which is accounted for by mantle-derived volatiles and a possible biogenic sulfur component. The Pb-isotope data for these two deposits are consistent with a lead sourced largely from the causative intrusion; although, some mantlederived lead is probably present. Red Hill has the highest S-isotope signature (13.7‰) indicating that the majority of sulfur was sourced from a seawater sulfate reservoir. ⁴⁰Ar/³⁹Ar dating showed that intrusion-related mineralisation at Tara formed at 420 ± 2 Ma; VHMS-related mineralisation at The Glen (Glen E deposit) formed at 418.2 ± 2.2 Ma; and that the Yerranderie and Bauloora intermediate sulfidation epithermal systems formed at 372.1 ± 1.9 Ma and 371 ± 13 Ma (respectively). New dating plus a review of timing constraints to Tabberabberan and Kanimblan cycle-related mineralisation highlighted metallogenic events at ~430 Ma (intrusion-related), ~420 Ma (intrusion- and VHMS-related) and a mid Devonian epithermal event. The timing of orogenic-related mineralisation is diachronous across the study area with the majority of orogenic gold systems in the west forming during the Middle Devonian Tabberabberan Orogeny; whereas, similar mineralisation in the northern HET formed during the Early Carboniferous Kanimblan Orogeny.
Книги з теми "Granite New South Wales Broken Hill"
Scheibner, Erwin, C. M. Powell, and Ross Spencer. Broken Hill-Sydney Tasman-Sea Transect: New South Wales, Eastern Australia. Washington, D. C.: American Geophysical Union, 1991. http://dx.doi.org/10.1029/gt005.
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 джерелаScheibner, E., C. M. Powell, and R. Spencer. Broken Hill-Sydney Tasman-Sea Transect: New South Wales, Eastern Australia. Wiley & Sons, Limited, John, 2013.
Знайти повний текст джерелаScheibner, Erwin. Broken Hill-Sydney-Tasman Sea Transect New South Wales, Eastern Australia (Global Geoscience Transect). American Geophysical Union, 1991.
Знайти повний текст джерелаSilver Lies, Golden Truths: Broken Hill, a Gentle German and Two World Wars. Wakefield Press Pty, Limited, 2015.
Знайти повний текст джерелаЗвіти організацій з теми "Granite New South Wales Broken Hill"
Kositcin, N., J. A. Fitzherbert, P. T. Main, and K. Waltenberg. New SHRIMP U-Pb zircon provenance and in situ monazite metamorphic ages from the Mount Robe Subblock, Broken Hill, New South Wales: July 2015–June 2017. Geoscience Australia and Geological Survey of New South Wales, 2018. http://dx.doi.org/10.11636/record.2018.050.
Повний текст джерела