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The Upper Oligocene San Rafael Intrusive Complex 2021 by javicol70 is a document available to read on EtoBox.
The upper Oligocene San Rafael intrusive complex (SRIC) in southeast Peru is the largest known high-grade tin deposit, with significant geological and geochemical insights into its formation. The study reveals that the SRIC consists mainly of peraluminous granites formed through the mingling of various magmas, with tin mineralization resulting from the interaction of metal-rich fluids and granitic rocks. The findings suggest that the granitic pluton acted as a structural host for mineralization rather than
- Author
- javicol70
- Language
- EN