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What is Metamorphic Study of Mawat Ophiolite Schist about?
This study investigates the garnet amphibolite schist from the Mawat ophiolite in Northeast Iraq, focusing on its geochemistry, mineral chemistry, and metamorphic evolution. The findings reveal two metamorphic stages, with peak conditions exceeding 800 °C and 8-10 kbar, indicating significant partial melting and retrogression processes. The research concludes that the gabbro is the protolith of the schist, which has undergone eclogite facies metamorphism followed by amphibolite facies overprinting.
- Author
- sitrakaalifa
- Language
- EN