Quick
Search: 
 
advanced search
 GSW Home    GeoRef Home    My GSW Alerts    Contact GSW    About GSW    Journals List    Help 
Economic Geology GSW 2008 Users' Group Meeting
JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS

Economic Geology; February 1984; v. 79; no. 1; p. 106-123
This Article
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Email this article to a friend
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Right arrow Order Hardcopy of Full Text via AGI/GeoRef
Citing Articles
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Sillitoe, R. H.
Right arrow Articles by Castro, H.
Right arrow Search for Related Content
GeoRef
Right arrow GeoRef Citation

Geologic exploration of a molybdenum-rich porphyry copper deposit at Mocoa, Colombia

Richard H. Sillitoe, Luis Jaramillo, and Hector Castro

8 West Hill Park, London, United Kingdom
UNDP, Colombia
Ingeominas, Colombia

Concealed porphyry copper-molybdenum target. High-grade mineralization. Drilling to date has delineated >260 million metric tons of hypogene ore averaging a little more than 1 percent Cu equivalent. The deposit is associated with a partly unroofed stock of biotite dacite porphyry, which was emplaced into broadly cogenetic andesitic and dacitic volcanic rocks during the Jurassic. A composite batholith of intermediate composition is located only 1.7 km from the deposit but was emplaced 30 to 40 m.y. earlier. The cylindrical orebody contains chalcopyrite, molybdenite, and local traces of bornite. The orebody is largely overlain by an essentially barren quartz-sericite-pyrite lithocap up to several hundred meters thick. High-grade copper-molybdenum ore is hosted by multiple hydrothermal breccias. Although the Mocoa porphyry system is overlain by a jarositic zone of partial leaching up to 260 m thick, rapid erosion during the late Cenozoic precluded generation of a significant zone of supergene chalcocite enrichment. The high precipitation caused nearly complete removal of abundant hypogene anhydrite and supergene gypsum to depths of at least 900 m.--Modified journal abstract.

This record provided courtesy of AGI/GeoRef.







JOURNAL HOME HELP CONTACT PUBLISHER SUBSCRIBE ARCHIVE SEARCH TABLE OF CONTENTS
Copyright © 2008 by Society of Economic Geologists