High-Temperature Metamorphic Garnets from Grenvillian Granulites of Southwestern Oaxacan Complex (Southern Mexico): Petrology, Geochemistry, Geothermobarometry, and Tectonic Implications

نویسندگان

چکیده

The basement of eastern Mexico comprises Grenvillian-age granulite-facies metamorphic rocks. Oaxacan Complex represents the largest outcrop belt this in Mexico. In work, southwestern garnets are studied from a petrographical, geochemical, and geothermobarometrical perspective for first time. display different grain sizes nucleated polyphase evolution. almandine end member proportion is similar all lithotypes. highest pyrope concentrations found Qz Fsp paragenesis ultramafic rocks lowest amphibolite. grossular spessartine amphibolite lithotype. Southwestern paraderivate samples more enriched Rb, Ba, Pb, Ni, Zn than those orthoderivate Ti V. This fact related to nature protoliths mineral phases that fractionate same minor trace elements. Garnets para- 0.02–1.1 Eu/Eu* anomalies. indicates almost formed while plagioclase was stable, it does not rule out interpretation some were peritectic. pressure obtained using Grt-Opx-Pl-Qz geobarometer higher northern part Complex, consistent with granulites Novillo Gneiss northeastern Geothermobarometric studies reveal P-T features at study site, so structural levels orogen inferred.

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ژورنال

عنوان ژورنال: Minerals

سال: 2021

ISSN: ['2075-163X']

DOI: https://doi.org/10.3390/min11080805