Lithospheric controls on the formation of provinces hosting giant orogenic gold deposits

Author:

Bierlein Frank P.,Groves David I.,Goldfarb Richard J.,Dubé Benoit

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics,Economic Geology

Reference102 articles.

1. Aitchison JC, Ireland TR, Blake MC, Flood PG (1992) 530 Ma zircon age for ophiolite from the New England Orogen; oldest rocks known from eastern Australia. Geology 20:125–128

2. Allibone AH, McCuaig TC, Harris D, Etheridge M, Munroe S, Byrne D, Amanor J, Gyapong W (2002) Structural controls on gold mineralization at the Ashanti deposit Obuasi, Ghana. In: Goldfarb RJ, Nielsen RL (eds) Integrated methods for discovery: global exploration in the twenty-first century. Soc Econ Geol Spec Publ 9:65–93

3. Barley ME, Groves DI (1990) Deciphering the tectonic evolution of Archaean greenstone belts: the importance of contrasting histories to the distribution of mineralization in the Yilgarn Craton, Western Australia. Precambrian Res 46:3–20

4. Bierlein FP, Crowe DE (2000) Phanerozoic orogenic lode gold deposits. In: Hagemann SG, Brown PE (eds) Gold in 2000, vol 13. Society Economic Geologists Reviews in Economic Geology, pp 103–139

5. Bierlein FP, Arne DC, Foster DA, Reynolds PR (2001a) A geochronological framework for slate belt-hosted gold mineralisation in central Victoria, Australia. Miner Depos 36:741–767

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