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Downes, P. M., Seccombe, P. K., Carr, G. R. (2008) Sulfur- and lead-isotope signatures of orogenic gold mineralisation associated with the Hill End Trough, Lachlan Orogen, New South Wales, Australia. Mineralogy and Petrology, 94 (3) 151-173 doi:10.1007/s00710-008-0012-7

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Reference TypeJournal (article/letter/editorial)
TitleSulfur- and lead-isotope signatures of orogenic gold mineralisation associated with the Hill End Trough, Lachlan Orogen, New South Wales, Australia
JournalMineralogy and Petrology
AuthorsDownes, P. M.Author
Seccombe, P. K.Author
Carr, G. R.Author
Year2008 (November)Volume94
Issue3
PublisherSpringer Science and Business Media LLC
DOIdoi:10.1007/s00710-008-0012-7Search in ResearchGate
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Mindat Ref. ID16877Long-form Identifiermindat:1:5:16877:9
GUID0
Full ReferenceDownes, P. M., Seccombe, P. K., Carr, G. R. (2008) Sulfur- and lead-isotope signatures of orogenic gold mineralisation associated with the Hill End Trough, Lachlan Orogen, New South Wales, Australia. Mineralogy and Petrology, 94 (3) 151-173 doi:10.1007/s00710-008-0012-7
Plain TextDownes, P. M., Seccombe, P. K., Carr, G. R. (2008) Sulfur- and lead-isotope signatures of orogenic gold mineralisation associated with the Hill End Trough, Lachlan Orogen, New South Wales, Australia. Mineralogy and Petrology, 94 (3) 151-173 doi:10.1007/s00710-008-0012-7
In(2008, November) Mineralogy and Petrology Vol. 94 (3) Springer Science and Business Media LLC

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Downes, P. M., Seccombe, P. K., & Carr, G. R. (2008). Sulfur-and lead-isotope signatures of orogenic gold mineralisation associated with the Hill End Trough, Lachlan Orogen, New South Wales, Australia. Mineralogy and Petrology, 94(3-4), 151-173.
Downes, P. M., & Seccombe, P. K. (2004). Sulfur isotope distribution in Late Silurian volcanicā€hosted massive sulfide deposits of the Hill End Trough, eastern Lachlan Fold Belt, New South Wales. Australian Journal of Earth Sciences, 51(1), 123-141.
Downes, P. M., Seccombe, P. K. (2004) Sulfur isotope distribution in Late Silurian volcanic-hosted massive sulfide deposits of the Hill End Trough, eastern Lachlan Fold Belt, New South Wales. Australian Journal of Earth Sciences, 51 (1). 123-141 doi:10.1046/j.1400-0952.2003.01048.x
Yangs, K., Thalhammer, O. A. R., Seccombe, P. K. (1995) Distribution of platinum group elements in the Great Serpentinite Belt of New South Wales, Eastern Australia. Mineralogy and Petrology, 54 (3) 191-211 doi:10.1007/bf01162861
Downes, Peter M. (2007) Yerranderie a Late Devonian Silver?Gold?Lead Intermediate Sulfidation Epithermal District, Eastern Lachlan Orogen, New South Wales, Australia. Resource Geology, 57 (1) 1-23 doi:10.1111/j.1751-3928.2006.00001.x
Seccombe, P. K., Hicks, M. N. (1989) The Hill End goldfield, NSW, Australia ?early metamorphic deposition of auriferous quartz veins. Mineralogy and Petrology, 40 (4) 257-273 doi:10.1007/bf01164602
Carr, P. F., Selleck, B., Stott, M., Williamson, P. (2008) Native Lead at Broken Hill, New South Wales, Australia. The Canadian Mineralogist, 46 (1) 73-85 doi:10.3749/canmin.46.1.73
J. H. Gibson and P. K. Seccombe (1997) Vitrinite reflectance and isotopic evidence for epithermal mineralisation at the Copeland goldfield, southern New England Fold Belt, New South Wales. Tectonics and Metallogenesis of the New England Orogen. Geological Society of Australia Special Publication 19,272-289.
Elliott, Peter (2021) Cardite, Zn5.5(AsO4)2(AsO3OH)(OH)3Ā·3H2O, a new zinc arsenate mineral from Broken Hill, New South Wales, Australia. Mineralogy and Petrology, 115 (4) 467-475 doi:10.1007/s00710-021-00750-2
Lu, Jianchun, Seccombe, Philip K., Stewart Eldridge, C. (1996) SHRIMP S-isotope evidence for fluid mixing during gold mineralization in a slate-belt gold deposit (Hill End, New South Wales, Australia) Chemical Geology, 127 (1) 229-240 doi:10.1016/0009-2541(95)00095-x
Glen, R. A., Watkins, J. J. (1999) Implications of Middle Devonian deformation of the eastern part of the Hill End Trough, Lachlan Orogen, New South Wales. Australian Journal of Earth Sciences, 46 (1) 35-52 doi:10.1046/j.1440-0952.1999.00687.x
 
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