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High-pressure pelitic granulites with a peak assemblage of garnet+kyanite+K-feldspar+plagioclase+biotite+quartz have been found from the Qianlishan Complex in the westernmost part of the Khondalite Belt, an east–west-trending Paleoproterozoic orogen between the Ordos and Yinshan Blocks in the North China Craton. Petrographic evidence indicates that high-pressure pelitic granulites underwent the prograde,...
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