Phase equilibria modeling of anatexis during ultra-high temperature metamorphism of the crust
Ultra-high temperature (UHT) granulite-facies metamorphism is commonly identified in Mg–Al-rich rocks. Many such lithologies are thought to be metasedimentary rocks based on the presence of detrital zircon. However, whether a metasedimentary protolith is required to form diagnostic mineral assemblag...
| Prif Awduron: | , , |
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| Fformat: | Journal article |
| Iaith: | English |
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Elsevier
2021
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