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- W2369984186 abstract "The results by the joint constraints of Pb、Sr、Nd and O isotopes indicate that the source materials of Darongshan granitoid suite were upper crustal rocks, which had underground at least two-stage evolutions with the range of 10 to 10 2 of the mian μ values and (1100～1500)×10 6 a of crustal provenance ages The Sr-O isotope system reveals that the source materials of Pubei and Taima plutons were relative homogeneous and keep close system during and after diagenetic stage; the Jiuzhou pluton was the mixed product of two different sialic materials by remelting without fully homogeneous The main formation process of Darongshan granitoid suite was crystallization fractionation according to the data of δD-H 2O system" @default.
- W2369984186 created "2016-06-24" @default.
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- W2369984186 date "1999-01-01" @default.
- W2369984186 modified "2023-09-25" @default.
- W2369984186 title "THE CHARACTERISTICS OF ISOTOPES GEOCHEMISTRYOF DARONGSHAN GRANITOID SUITE, GUANGXI" @default.
- W2369984186 hasPublicationYear "1999" @default.
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