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《Earthquake Research In China》 1996-02
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Late Cenozoic Tectonic Deformation and Mechanism along the Tianshan Mountain, Northwestern China

Zhang Peizhen Deng Qidong Yang Xiaoping Peng Sizhen Xu Xiwei (Institute of Geology, SSB, Beijing 100029, China) Feng Xianyue (Xingjiang Uyger Autonomous Region Seismological Bureau, Ulumuqi 830011, China)  
The Tianshan mountain is a typical Cenozoic rejuvenated mountain belt in the continental Asia. Its styles, amounts, rates, and processes of deformation provide important meaning for understanding geodynamics of other mountains in the interior of continent. On the basis of detailed field studies on major active fold and reverse fault zones in both northern and southern Tianshan, this paper discusses characteristics of late Cenozoic deformation in the Tianshan with the aim of understanding how this intracontinental mountain has been deformed. The late Cenozoic deformation in the Tainshan probably initiated between Pliocene and early Pleistocene time with the peak deformation stage in the period between early and middle Pleistocene. Deformation is characterized by crust shortening where the Tianshan thrusts both to the south and the north to form several folds and reverse fault zones along the range fronts. The newly formed fold and reverse fault zones only develop in the range-front depressions. These fold and reverse fault zones involve thin-skinned deformation of the foreland with major propagating thrust ramps near the range front. Outside the range-front depressions high-angle reverse faults merge to the surface at the base of the range with less amount of crustal shortening than that within the depression. Quantitative measurement across the range-front depressions indicate that the amount of total Quaternary crustal shortening decreases from west to east along the Tainshan mountain. It appears that compression of the Pamir Plateau to the north is probably the major driving force that caused deformation in the Tianshan.
【CateGory Index】: P542
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