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- W2364005303 abstract "The study on metamorphism of metamorphic rocks from Xingzi Group shows that they have undergone a hornblende facies metamorphism. The metamorphic temperature is about 480℃~580℃,and pressure is between 300 MPa~500 MPa. It is very different from other Proterozoic rocks distributed along the southern margin of Yangtz Block and has a very special tectonic evolution history. Although the metamorphic features of Xingzi metamorphic rocks are similar to those of Mayuan Group and Badu Group which have the same age with Xingzi Group in Huaxia Block,they have very different geochemical features and tectonic environments. More and more research data indicate that Xingzi Group is the nappe outlier from Huaxia Block, but the Precambrian metamorphic basement caused by crustal extension." @default.
- W2364005303 created "2016-06-24" @default.
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- W2364005303 date "2003-01-01" @default.
- W2364005303 modified "2023-09-25" @default.
- W2364005303 title "THE STUDY ON THE METAMORPHISM AND METAMORPHIC AGE FROM XINGZI GROUP, LUSHAN" @default.
- W2364005303 hasPublicationYear "2003" @default.
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