Mass-transfer and differential element mobility in metapelites during multistage metamorphism of the Yenisey Ridge, Siberia
Pelitic gneisses and schists from the Garevka Complex (Yenisey Ridge) at the western margin of the Siberian craton contain zoned garnet porphyroblasts that show clear evidence of multistage growth. The three discrete stages define a counter-clockwise pressure–temperature (P–T) path involving initial...
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