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- W2382372013 abstract "The Wenquan granite in the western Qinling is the product of the mixing of crust and mantle magmas, and belongs to the aluminum super-saturation and calc-alkali series. The host rocks are characterized by poor in CaO, rich in FeOtot with the ANKC more than 1.1 and the NK/A lower than 0.9, and higher hypothermal metallogenic elements such as Mo, Sn and Cr. The basic mafic magmatic elements have rich in Na2O、K2O and poor in FeOtot, and rich in such as Ba,Rb,Sr,Zr,Th,Hf and Nb, but have poorer siderophile elements. The abnormal distribution of the trace elements indicates the noticeable exchanging and complying between these two. The ratio of LREE/HREE is 10～15 in host rocks, and 9.98～13.5 in basic parts because of the magmas mixing, and the intensively migmatized monzonitic granite shows the remarkable transition between crust and mantle." @default.
- W2382372013 created "2016-06-24" @default.
- W2382372013 creator A5004659728 @default.
- W2382372013 date "2003-01-01" @default.
- W2382372013 modified "2023-09-24" @default.
- W2382372013 title "THE GEOCHEMICAL INFORMATION OF THE MAGMA MIXING FROM THE WENQUAN GRANITE IN THE WESTERN QINLING" @default.
- W2382372013 hasPublicationYear "2003" @default.
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