Fluid inclusion and isotope (O, H, C, Sr) constraints on the orogenic gold mineralization at the Enche Concha and Tunel prospects, Gurupi Belt, Brazil
The gold mineralization at the Enche Concha and Tunel prospects, northwestern portion of the Gurupi Belt, is hosted in dacites and phyllites that belong to the ca. 2160 Ma-old metavolcano-sedimentary Chega Tudo Formation. These host rocks are variably deformed, from a spaced cleavage to schistose an...
Main Authors: | , , , |
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Format: | Article |
Language: | English |
Published: |
Serviço Geológico do Brasil (CPRM)
2020-07-01
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Series: | Journal of the Geological Survey of Brazil |
Subjects: | |
Online Access: | https://jgsb.cprm.gov.br/index.php/journal/article/view/86 |