Volcanic framework, geochronology and geochemical evolution of the El Dorado gold district, El Salvador, Central America
The Pliocene El Dorado epithermal Au-Ag vein system, located in northern El Salvador, is hosted in Tertiary volcanic rocks that accumulated along the Caribbean plate margin in response to the subduction of the Farallon/Cocos plate. The volcanic basement rocks in the district form a >400-meters...
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| Language: | English |
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University of British Columbia
2011
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| Online Access: | http://hdl.handle.net/2429/32325 |