P-T-fluid-deformation regime of the Ediacaran Serra do Cavalo Magro orogenic gold deposit, Ribeira Belt, Brazil
Abstract
The Serra do Cavalo Magro orogenic gold deposit is located in the southern Ribeira Belt, Brazil. Gold-quartz veins are hosted in Calymmian (1500–1450 Ma) metasedimentary and metabasic rocks and Ediacaran (610–600 Ma) granitic rocks. Geochronological data available in previous literature and structural-petrological relationships with host rocks and shear zones indicate that the gold mineralization was formed within 580–540 Ma during the...
Paper Details
Title
P-T-fluid-deformation regime of the Ediacaran Serra do Cavalo Magro orogenic gold deposit, Ribeira Belt, Brazil
Published Date
May 1, 2020
Journal
Volume
120
Pages
103384 - 103384
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