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DOI: 10.1590/23174889201720160097ARTICLEGranulitefacies metamorphism at ca. 570580 Ma in the Porangatu Granulate Complex, central Brazil: implications for the evolution of the Transbrasiliano Lineament Metamorphism
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Granulite-facies metamorphism is a type of metamorphism that occurs at high temperatures and pressures, resulting in the formation of granulite rocks.
Scientists, geologists, or researchers studying metamorphic rocks in California may be required to file reports on granulite-facies metamorphism.
To fill out a report on granulite-facies metamorphism in California, detailed observations, analysis, and data on the rock samples must be provided.
The purpose of studying granulite-facies metamorphism is to understand the geological processes that have shaped the Earth's crust and interpret the conditions under which these rocks formed.
The report on granulite-facies metamorphism must include details on the mineral assemblages, textures, structures, and any other relevant information observed in the metamorphic rocks.
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