High-temperature metamorphic garnets from Grenvillian granulites of southwestern Oaxacan Complex (Southern Mexico): petrology, geochemistry, geothermobarometry, and tectonic implications
The basement of eastern Mexico comprises Grenvillian-age granulite-facies metamorphic rocks. The Oaxacan Complex represents the largest outcrop belt of this basement in Mexico. In this work, southwestern Oaxacan Complex garnets are studied from a petrographical, geochemical, and geothermobarometrica...
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格式: | Article |
語言: | English |
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2022
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在線閱讀: | https://hdl.handle.net/10356/160797 |
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