Sulfur- and lead-isotope signatures of orogenic gold mineralisation associated with the Hill End Trough, Lachlan Orogen, New South Wales, Australia

Author:

Downes P. M.,Seccombe P. K.,Carr G. R.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Reference76 articles.

1. Arundell M (1994) Exploration prospecting license no 3747 and exploration license nos. 4191, 4223, 4224 and 4276 Bathurst district, N.S.W., second combined annual report 5th February, 1993 to 4th February, 1994. Geological Survey of New South Wales, File GS19994/196. Available from Geological Survey of New South Wales DIGS website: http://digsopen.minerals.nsw.gov.au/ . Accessed 17 Dec 2007

2. Barron LM, Meakin NS, Cameron RG, Morgan EJ, Pogson DJ, Scott MM, Raymond OL (1999) Ungrouped Devonian intrusions. In: Meakin NS, Morgan EJ (eds) Dubbo 1:250 000 geological sheet SI/55-4, explanatory notes. 2nd edn. Geological Survey of New South Wales, Sydney, pp 223–228

3. Bierlein FP, Crowe DE (2000) Phanerozoic orogenic lode gold deposits. In: Hagemann SG, Brown PE (eds) Gold in 2000. Rev Econ Geol 13:103–139

4. Black LP (1998) SHRIMP zircon U/Pb isotope age dating of samples from the Dubbo 1:250 000 Sheet area, batch 2. Geological Survey of New South Wales, File GS1998/127. Available from Geological Survey of New South Wales DIGS website: http://digsopen.minerals.nsw.gov.au/ . Accessed 17 Dec 2007

5. Carr GR, Dean JA, Suppel DW, Heithersay PS (1995) Precise lead isotope fingerprinting of hydrothermal activity associated with Ordovician to Carboniferous metallogenic events in the Lachlan Fold Belt of New South Wales. Econ Geol 90:1467–1505

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