Transport Of Gold In High Temperature, Low Pressure, Gas Phases With C12, Co, H2s: A Clue To Gold Mobilization From The Lower Crust

Society for Mining, Metallurgy & Exploration
R. J. Puddephatt S. Zhou W. S. Fyfe
Organization:
Society for Mining, Metallurgy & Exploration
Pages:
7
File Size:
600 KB
Publication Date:
Jan 1, 1989

Abstract

Gold is easily mobilized at temperatures within range 600-11OO°C by gases such as Cl2, CO, H2S, in gas mixtures, at low pressures. Such gases are relevant to conditions of granulite facies metaomorphism in environments of magma underplating. These observations suggest an efficient mechanism for moving gold to the upper crust during major thermal events. The efficiency of precipitation of gold at lower temperatures is related to available mineral surfaces and pyrite appears to be an excellent substrate for gold precipitation.
Citation

APA: R. J. Puddephatt S. Zhou W. S. Fyfe  (1989)  Transport Of Gold In High Temperature, Low Pressure, Gas Phases With C12, Co, H2s: A Clue To Gold Mobilization From The Lower Crust

MLA: R. J. Puddephatt S. Zhou W. S. Fyfe Transport Of Gold In High Temperature, Low Pressure, Gas Phases With C12, Co, H2s: A Clue To Gold Mobilization From The Lower Crust. Society for Mining, Metallurgy & Exploration, 1989.

Export
Purchase this Article for $25.00

Create a Guest account to purchase this file
- or -
Log in to your existing Guest account