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- W2376915240 abstract "Beidashan rock belt in Alxa located at southern of Alxa block, at south of enger-wsu suture zone. Abundance of Hercynian igneous rock, including mafic-ultramafic rock, quartz diorite, quartz monzonite, quartz syenite and myoite, are yielded. The ~(40)Ar-~(39)Ar dating on biotite from the Gashuntatale quartz monzonite yields a plateau age of 275.0±4Ma and hornblende from quartz diorite yields a plateau age of 277.0±3.8Ma, both of which are product of Hercynian magma activity. According to element geochemistry, quartz diorite is characterized by high Al2O3, CaO, Mg# and low K2O,(La/Yb)N, ΣREE value, indicate its mantle source feature; and the quartz monzonite of study area with a character of high K2O,(La/Yb)N, ΣREE, Al2O3, and low CaO, Mg# value, indicate its crust affinity. Synthesize trace element geochemistry and tectonic setting, the quartz diorite and quartz monzonite maybe a product of active continental margin." @default.
- W2376915240 created "2016-06-24" @default.
- W2376915240 creator A5010922072 @default.
- W2376915240 date "2007-01-01" @default.
- W2376915240 modified "2023-09-23" @default.
- W2376915240 title "~(40)Ar-~(39)Ar Age and Geochemical Features of Hercynian Intermediate Acidity Rock in Beidashan Rock Belt, Alxa" @default.
- W2376915240 hasPublicationYear "2007" @default.
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