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- W2365744304 abstract "The genesis type, evolution, structural setting and geodynamic characteristics of Palaeogene magmatic rocks in Gengma are discussed according to the study of their geological, petrographic and geochemic characteristics.They intrude into the red formation K_1n and river-lake facies Em, which are more basic than the Triassic granite and show characteristics of syncollision and volcanic arc granite. The crust thickening and inland orogenic force cause the ultramafic accumulative crystal to detach and sink in the mantle, which is partly melted. The magma of melted detaching and sinking crystal completely mixes with that of the melted crust in the magmatic chamber of crust, which forms the Palaeogene syncollision and volcanic arc magma. In the rising process, the separate crystallization of this mixed magma takes place and the Palaeogene granite unit with different lithologic characteris formed by many times of pulse emplacement. According to the isotope dating and other geological events, we think it is formed by the process resulting the detaching and sinking in inland during late orogenic stage and its intrusion period is Palaeogene." @default.
- W2365744304 created "2016-06-24" @default.
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- W2365744304 date "2004-01-01" @default.
- W2365744304 modified "2023-09-23" @default.
- W2365744304 title "THE GENESIS, EVOLUTION AND STRUCTURAL SETTING OF PALAEOGENE GRANITOID MAGMA IN GENGMA" @default.
- W2365744304 hasPublicationYear "2004" @default.
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