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《Chinese Geology》 2003-04
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Tectonic attribute of the Qoltag orogenic belt in the East Tianshan Mountains, northwestern China

CHEN Fu-wen1, HE Guo-qi2, LI Hua-qin1(1 Yichang Institute of Geology and Mineral Resources, China Geological Survey, Yichang 443003, Hubei, China2 Department of Geology, Peking University, Beijing 100871, China)  
The Joltag orogenic belt is located between the Turpan-Hami basin and Central Tianshan block, in the East Tianshan Mountains. For a long time different views exist as to the tectonic attribute of this orogenic belt, e.g. it is considered as a Late Paleozoic arc island belt, a backarc basin, an aulacogen, a Paleozoic continental-marginal accretion belt or Carboniferous volcanic-type passive continental margins. Based on systematic petrological, petrochemical and rock geochemical studies of the volcanic-sedimentary formations of the Early Carboniferous Yamasu Formation in the belt and the fact that the Qoltag area was in an intraplate extensional dynamic setting rather than a noncompresional collisional dynamic setting during the Early Paleozoic,the authors conclude that the Qoltag orogenic belt should be an extensional tectono-magmatic one.
【Fund】: 国家重点基础研究发展规划项目(2001CB409810)资助。
【CateGory Index】: P542.3
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