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High-P Metamorphism in Oulad Dlim Massif by Yeffer Andreany Chinchia Daza is a document available to read on EtoBox.
This document summarizes a study of high-pressure amphibolite-facies metamorphism in the Adrar-Souttouf Metamafic Complex within the Oulad Dlim Massif in Morocco. The authors analyzed two samples of garnet amphibolite from the northern end of the complex. Thermobarometric modeling indicates peak metamorphic conditions of 650-700°C and 10-13 kbar, representing high-pressure amphibolite facies. In contrast to eclogite-facies rocks found further south, no relict eclogite assemblages were found. This suggests t
- Author
- Yeffer Andreany Chinchia Daza
- Language
- EN