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岩石学报 1999
A study of tectonites of granulite facies in Yushugou, South Tianshan, China.
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Abstract:
Tectonites of granulite facies in Yushugou occur as mylonite zones and mylonitized zones with highly rheomorphic foliations, and are characterized by the microstructures of plastic deformation of main rock forming minerals. During the deformation, chemic