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- W2382609191 abstract "Ailao Shan-Diancang Mountain Ranges,which are situated in the west part of Yunnan Province,are famous for their distinctive topography,geomorphology and geological structures.The principal part of Ailao Shan-Diancang Mountain Range is composed of high metamorphic rock series,which are considered as the Precambrian metamorphic basement of the Yangtze Plate. In this paper,U-Pb ages of zircons from granodioritic mylonite of Diancangshan Mountain (DCS-1) and biotite granodioritic gneiss of Ailaoshan Mountain (SM07-1) have been determined by sensitive high resolution ion microprobe method (SHRIMP).The zircons from the samples yield a concordant U-Pb ages of 233±2.6Ma (DCS-1,MSWD=1.47) and 239.8±2.8Ma (SM07-1,MSWD=1.9) respectively.According to the former researches on the granitoid rocks in west Yunnan Province and geochronological studies,it is concluded that the west Yunnan areas have been experienced an extensively Triassic magmatism.The protolith was the result of the Triassic magmatic event,which related with the continental rift tectonic environment.The Triassic magmatism brought a great deal of intrusions to the crustal,which have characteristics ofbimodal.The metamorphic rocks in the study area are unlikely to be the metamorphic basement of Yangtze Plate,its metamorphism is due to the process of the rocks uplifting and Cenozoic tectonic evolution." @default.
- W2382609191 created "2016-06-24" @default.
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- W2382609191 date "2008-01-01" @default.
- W2382609191 modified "2023-09-23" @default.
- W2382609191 title "Zircon SHRIMP dating and its geological implications of the metamorphic rocks in Ailao Shan-Diancang Mountain Ranges,west Yunnan" @default.
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