Abstract
The Karouni orogenic gold deposits are located in north-central Guyana 35 km to the west of the 5 Moz Omai gold deposit. They are hosted in a 2200 to 2100 Ma greenstone belt within the Paleo- to Neoproterozoic Guiana Shield. Karouni consists of two deposits, Smarts and Hicks, located 2 km apart along the NW-striking Smarts-Hicks shear zone. Both deposits are hosted within a sequence of greenschist facies mafic volcanic rocks and felsic intrusions. The hydrothermal alteration mineral assemblages vary according to lithology and are characterized by narrow selvages (
Original language | English |
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Pages (from-to) | 1705-1732 |
Number of pages | 28 |
Journal | Economic Geology |
Volume | 113 |
Issue number | 8 |
DOIs | |
Publication status | Published - Dec 2018 |