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- W2364145652 abstract "The Muchen pluton, outcropping at the southeast side of the southwestern part of Jiangshan- Shaoxing Fault, is characterized by occurrence of dark enclaves and rapakivi feldspars, and has obvious magma mixing. In this pluton, the host rocks consist of monzonite and quartz monzonite, and the enclaves consist of monzonite diorite and monzonite. The rock- forming minerals in these rocks include potash feldspar, plagioclase, quartz, hornblende and biotite. The whole rocks are rich in alkali (Na2O+ K2O=6.58% ～ 10.42% , with an average of 8.41% ) and have high potassium contents (K2O/Na2O=0.72～ 1.45, and 1.16 in the average), but poor in titanium (TiO2= 0.37% ～ 1.22% , and 0.76% in the average), and are enriched in large ion lithophile elements and light rare earth elements. All these features show that the rocks belong to shoshonitic series. The pluton was emplaced in the tectonic setting of postcollisional arc, and resulted from the important tectonic- magmatic event in Early Cretaceous in this region." @default.
- W2364145652 created "2016-06-24" @default.
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- W2364145652 date "2007-01-01" @default.
- W2364145652 modified "2023-09-23" @default.
- W2364145652 title "Geochemical characteristics and tectonic implications of Muchen quartz monzonite pluton in Zhejiang Province" @default.
- W2364145652 hasPublicationYear "2007" @default.
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