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- W2349207761 abstract "The inrusives rocks in northern Cuoqin,Tibet,are dominated by diorite,quartz-diorite,granodiorite,adamellite and feldspar granite,dated from 65.1 to 98.2 Ma,which were produced by the inrusion in late Cretaceous.Light rare earth elements(REE) are enriched in diorite,quartz-diorite,granodiorite and adamellite.However,the light REEs show strong fractionation while the heavy ones are weaker in factionation,showing weak negative Eu anomality or no Eu anomality.These rocks are of low crystal differentiation,with Ba,Ta,Sr,P and Ti lost in different degrees.The feldspar granite in Jiabu,Cuoqin,rich in K and Rb,but poor in Ba,Sr and Ti,is characterized by strong negative Eu abnormality.While the rocks in Jialong-Longle and Kerule in the area consist of I type granite,with the tectonic environment of ilandarc or active continental margin.In contrast,the granite in Jiabu is formed in collision,belonging to I-S transition type." @default.
- W2349207761 created "2016-06-24" @default.
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- W2349207761 date "2009-01-01" @default.
- W2349207761 modified "2023-09-23" @default.
- W2349207761 title "Geochemical Characteristics and Tectonic Environment of the Late Cretaceous Intrusive Rocks in Cuoqin,Tibet" @default.
- W2349207761 hasPublicationYear "2009" @default.
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