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- W2381066979 abstract "The genesis of peraluminous granitiods and their tectonic setting are summarized, especially the genesis of peraluminous granite magma and their sign are discussed. It is concluded that peraluminous granite magma can be derived from crust, mantle or crust-mantle commixing source and there may exists continuous spectrum ranging from crust source to mantle source, resulted from interaction of crust and mantle. This paper also introduces the genesis of two main peraluminous granite (CPG and MPG), puts forward four rules to distinguish tectonic settings of peraluminous granite, and points out that peraluminous granitiods can come into being not only in compressional settings during collisional orogeny, but also in extensional backgrounds caused by the lithosphere extension." @default.
- W2381066979 created "2016-06-24" @default.
- W2381066979 creator A5082453359 @default.
- W2381066979 date "2003-01-01" @default.
- W2381066979 modified "2023-09-23" @default.
- W2381066979 title "Genesis of peraluminous granitoids and their tectonic settings" @default.
- W2381066979 hasPublicationYear "2003" @default.
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