Contrasting coeval paragenesis of gold and scheelite in an orogenic hydrothermal system, Macraes mine, New Zealand

Author:

MacKenzie Doug,Farmer Lauren,Moore Jonathan,Craw Dave

Funder

University of Otago

Ministry for Business, Innovation and Employment

Publisher

Elsevier BV

Subject

Economic Geology,Geochemistry and Petrology,Geology

Reference58 articles.

1. Sm-Nd dating of scheelite and tourmaline; implications for the genesis of Archean gold deposits, Val d'Or, Canada;Anglin;Econ. Geol.,1996

2. Fluid-inclusion and stable-isotope studies of gold-tungsten bearing hydrothermal deposits, Saucelle-Barruecopardo Area, Spain;Antona;Eur. J. Mineral.,1994

3. Geometry and petrography of stockwork vein swarms, Macraes mine, Otago Schist, New Zealand;Begbie;N. Z. J. Geol. Geophys.,2006

4. Structural controls on the development of fault-hosted scheelite-gold mineralization in Glenorchy, northwest Otago, in Geology and Exploration of New Zealand Mineral Deposits (eds: A B Christie and R L Brathwaite);Begbie;The Australasian Institute of Mining and Metallurgy Monograph,2006

5. Phanerozoic orogenic lode gold deposits. In: gold in 2000, Hagemann, S.G., Brown, P.E., (eds);Bierlein;Rev. Econ. Geol.,2000

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