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- W2357632743 abstract "The Jitang rock group along the Taniantaweng- Leiwuqi- Jitang area of eastern Tibet,is mainly composed of schist,gneiss and mylonite tectonic slices,and have been strongly deformed. Isotopic ages of this rock group range widely from the Paleoproterozoic to the late Paleozoic,and it is thus necessary to divide it in detail. In recent years,geological mapping,cross-section measurement and isotopic age determination have been conducted in this area. In combination with the previous data and comprehensive comparison,the original Jitang Rock Group( the present Taniantaweng metamorphic complex in eastern Tibet) was divided into two sets of geological bodies,i. e.,the Pre-Ordovician- Middle Triassic Leiwuqi gneiss suite and the Pre-Carboniferous Jitang rock group. The Leiwuqi gneiss was further subdivided into five tectonic lithostratigraphic units,i. e.,the pre-Ordovician Chaqiusai rock group( 438. 2 ± 3. 6)~ 700. 0 Ma,the early Permian Doulazha gneiss unit( 282. 1 ± 0. 9) Ma,the late Permian Jiayama gneiss unit( 254. 0 ± 8. 0) Ma,the early Triassic Jialong gneiss unit( 246. 3 ± 0. 8) Ma,and the middle Triassic Ningda gneiss unit( 227. 0 ± 0. 6) Ma. This detailed division of the original Jitang rock group is a major advance of the stratigraphical study in the area,and may contribute to the basic geological research in eastern Tibet." @default.
- W2357632743 created "2016-06-24" @default.
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- W2357632743 date "2015-01-01" @default.
- W2357632743 modified "2023-09-28" @default.
- W2357632743 title "Tectostratigraphical division of the Jitang rock group in the Leiwuqi Region of eastern Tibet,China and the main evidence" @default.
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