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- W767061662 abstract "The granitoids in Geoje island are classified into diorite, Jisepo granodiorite and Geoje granite. The Jisepo granodiorite (biotite-hornblende granodiorite) is homogeneous in mineralogy, chemistry and texture, whereas the Geoje granite is inhomogeneous. The Geoje granite is thus divided into normal biotite-hornblende granite, porphyritic granite, and micrographic granite occurring as dike. According to petrochemistry of major and trace elements, the granitoids in Geoje island are plotted in the range of intermediate alkalic to alkalic-rich and salic in the variation of Niggli values. The granitoids are generally metaluminous to peraluminous, medium to high-K in the variation of alumina and potassium content respectively. The granitoids in Geoje island are differentiated from calc-alkaline series magma, similar to the Cretaceous to early Tertiary granitoids in southern Korea. The temperature of minimum melts probably ranges 750℃ to 700℃ under 2 kbar total pressure. The geochemical characteristics indicate that the Geoje granitoids may be continental arc to volcanic arc granite fractionated from a talc-alkaline magma which was derived from partial melting of mantle or igneous protoliths of the lower crust under the compressional plate margin." @default.
- W767061662 created "2016-06-24" @default.
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- W767061662 date "1999-01-01" @default.
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- W767061662 title "Petrology and Petrochemistry of the Granitoids in the Geoje Island, Korea" @default.
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