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- W2394184426 abstract "Wushan ophiolite is located in the west of North Qinling,north to Shangdan fault. It is comeposed of ultrabic rock , basic dike, metabasalts and marble. Geochemistry Features of metabasalts show it is calc-alkaline , formed at the tectonic settings of continent valley to nascent ocean.Isotopic age of metabasalts is 1 570 Ma, showing original magma formed in Mid-Proterozoic, belonging to the earlier ophiolite belt of continent crust evolution." @default.
- W2394184426 created "2016-06-24" @default.
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- W2394184426 date "2001-01-01" @default.
- W2394184426 modified "2023-09-24" @default.
- W2394184426 title "Characteristics, Isotopic age of Wushan Ophiolite and its Geological Significantce" @default.
- W2394184426 hasPublicationYear "2001" @default.
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