On reuse of Shaliuhe Group in the northern margin of Qaidam basin

XIN Hou-tian; ZHOU Shi-jun; WANG hui-chu; HAO Guo-jie; CHEN Neng-song; HAN Ying-shan

Northwestern Geology > 2004 > 37(1): 26-33.

XIN Hou-tian, ZHOU Shi-jun, WANG hui-chu, et al. On reuse of Shaliuhe Group in the northern margin of Qaidam basin[J]. Northwestern Geology, 2004, 37(1): 26-33.

Citation:

XIN Hou-tian, ZHOU Shi-jun, WANG hui-chu, et al. On reuse of Shaliuhe Group in the northern margin of Qaidam basin[J]. Northwestern Geology, 2004, 37(1): 26-33.

Citation:

XIN Hou-tian, ZHOU Shi-jun, WANG hui-chu, et al. On reuse of Shaliuhe Group in the northern margin of Qaidam basin[J]. Northwestern Geology, 2004, 37(1): 26-33.

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On reuse of Shaliuhe Group in the northern margin of Qaidam basin

1.
Tianjin Institute of Geology and Mineral Resources, Tianjin 300170, China
2.
China University of Geosciences, Wuhan 400037, China
3.
Qinghai Institute of Geological Survey, Xining 810012, China

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Received Date: February 17, 2003
Revised Date: June 11, 2003
Published Date: March 04, 2004

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Abstract

Abstract

There is very complicated composition in the metamorphic basement of the northern margin of Qaidam. In the south part of the area appears marble, garnet-quartz-mica-schist, quartzite, ecligite and other paragneiss system and they are named Shaliuhe Group. With the Neoproterozoic granite-gneiss, it constituents Qaidam block mass. In Oulongbuluke micro-block appears mid-high-metamophic crust system with extensive potassic migmatization and they are named Dakendaban Group.
- the northern margin of Qaidam,
- Shaliuhe Group,
- Dakendaban Group,
- ziron U-Pb isotopic age,
- ecligite

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On reuse of Shaliuhe Group in the northern margin of Qaidam basin

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