Metal anomalies in zircon as a record of granite-hosted mineralization
Granite-hosted magmatic-hydrothermal mineral deposits are major sources of Cu, Mo, Sn, Li, and W, originating via mineralizing fluids exsolved from volatile-saturated magmas. We show how trace elements in zircon sampled from the granite-hosted Zaaiplaats tin deposit, Bushveld Complex, preserve a rec...
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Published in | Chemical geology Vol. 585; p. 120580 |
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Main Authors | , , , , , |
Format | Journal Article |
Language | English |
Published |
Elsevier B.V
20.12.2021
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Subjects | |
Online Access | Get full text |
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