Full Text:   <2964>

CLC number: P542; P618.130; P532

On-line Access: 

Received: 2007-02-16

Revision Accepted: 2007-06-19

Crosschecked: 0000-00-00

Cited: 1

Clicked: 5908

Citations:  Bibtex RefMan EndNote GB/T7714

-   Go to

Article info.
1. Reference List
Open peer comments

Journal of Zhejiang University SCIENCE A 2007 Vol.8 No.9 P.1388-1394

http://doi.org/10.1631/jzus.2007.A1388


Dual influence of the rejuvenation of Southern Tianshan and Western Kunlun orogen on the Cenozoic structure deformation of Tarim Basin, northwestern China: A superposition deformation model from Bachu Uplift


Author(s):  HE Guang-yu, HE Zhi-liang, ZHANG Hong-an, ZHU Zhi-xin, CHEN Qiang-lu, QIAN Yi-xiong, GU Yi

Affiliation(s):  Department of Earth Sciences, Structure Research Center of Petroleum Basin of China Education Ministry, Zhejiang University, Hangzhou 310027, China; more

Corresponding email(s):   hegy@zju.edu.cn

Key Words:  Superposition deformation model, Bachu Uplift, Southern Tianshan, Western Kunlun, Cenozoic


HE Guang-yu, HE Zhi-liang, ZHANG Hong-an, ZHU Zhi-xin, CHEN Qiang-lu, QIAN Yi-xiong, GU Yi. Dual influence of the rejuvenation of Southern Tianshan and Western Kunlun orogen on the Cenozoic structure deformation of Tarim Basin, northwestern China: A superposition deformation model from Bachu Uplift[J]. Journal of Zhejiang University Science A, 2007, 8(9): 1388-1394.

@article{title="Dual influence of the rejuvenation of Southern Tianshan and Western Kunlun orogen on the Cenozoic structure deformation of Tarim Basin, northwestern China: A superposition deformation model from Bachu Uplift",
author="HE Guang-yu, HE Zhi-liang, ZHANG Hong-an, ZHU Zhi-xin, CHEN Qiang-lu, QIAN Yi-xiong, GU Yi",
journal="Journal of Zhejiang University Science A",
volume="8",
number="9",
pages="1388-1394",
year="2007",
publisher="Zhejiang University Press & Springer",
doi="10.1631/jzus.2007.A1388"
}

%0 Journal Article
%T Dual influence of the rejuvenation of Southern Tianshan and Western Kunlun orogen on the Cenozoic structure deformation of Tarim Basin, northwestern China: A superposition deformation model from Bachu Uplift
%A HE Guang-yu
%A HE Zhi-liang
%A ZHANG Hong-an
%A ZHU Zhi-xin
%A CHEN Qiang-lu
%A QIAN Yi-xiong
%A GU Yi
%J Journal of Zhejiang University SCIENCE A
%V 8
%N 9
%P 1388-1394
%@ 1673-565X
%D 2007
%I Zhejiang University Press & Springer
%DOI 10.1631/jzus.2007.A1388

TY - JOUR
T1 - Dual influence of the rejuvenation of Southern Tianshan and Western Kunlun orogen on the Cenozoic structure deformation of Tarim Basin, northwestern China: A superposition deformation model from Bachu Uplift
A1 - HE Guang-yu
A1 - HE Zhi-liang
A1 - ZHANG Hong-an
A1 - ZHU Zhi-xin
A1 - CHEN Qiang-lu
A1 - QIAN Yi-xiong
A1 - GU Yi
J0 - Journal of Zhejiang University Science A
VL - 8
IS - 9
SP - 1388
EP - 1394
%@ 1673-565X
Y1 - 2007
PB - Zhejiang University Press & Springer
ER -
DOI - 10.1631/jzus.2007.A1388


Abstract: 
Based on new high-resolution seismic profiles and existing structural and sedimentary results, a superposition deformation model for cenozoic bachu Uplift of northwestern Tarim Basin, northwestern China is proposed. The model presents the idea that the bachu Uplift suffered structure superposition deformation under the dual influences of the cenozoic uplifting of southern Tianshan and western Kunlun orogen, northwestern China. In the end of the Eocene (early Himalayan movement), bachu Uplift started to be formed with the uplifting of western Kunlun, and extended NNW into the interior of Kalpin Uplift. In the end of the Miocene (middle Himalayan movement), bachu Uplift suffered not only the NNW structure deformation caused by the western Kunlun uplifting, but also the NE structure deformation caused by the southern Tianshan uplifting, and the thrust front fault of Kalpin thrust system related to the southern Tianshan orogen intrudes southeastward into the hinterland of bachu Uplift and extends NNE from well Pi1 to Xiaohaizi reservoir and Gudongshan mountain, which resulted in the strata folded and denuded strongly. In the end of the Pliocene (late Himalayan movement), the impact of southern Tianshan orogen decreased because of the stress released with the breakthrough upward of Kalpin fault extending NE, and bachu Uplift suffered mainly the structure deformation extending NW-NNW caused by the uplifting of western Kunlun orogen.

Darkslateblue:Affiliate; Royal Blue:Author; Turquoise:Article

Reference

[1] Allen, M.B., Vincent, S.J., 1999. Late Cenozoic structures of Kepingtage thrust zone: implications of the Tian Shah and Tarim Basin, northwest China. Tectonics, 18(4):639-654.

[2] Burtman, V.S., 2000. Cenozoic crustal shortening between the Pamir and Tien Shan and a reconstruction of the Pamir-Tien Shan transition zone for the Cretaceous and Palaeogene. Tectonophysics, 319(2):69-92.

[3] Buslov, M.M., Grave, J.D., Bataleva, E.A.V., Batalev, V.Y., 2007. Cenozoic structure and geodynamic evolution of the Kyrgyz Tien Shan Mountains: A review of geological, thermochronological and geophysical data. J. Asian Earth Sciences, 29(2-3):205-214.

[4] Chen, H.L., Yang, S.F., Jia, C.Z., Dong, C.W., Wei, G.Q., 1998. Confirmation of Permian intermediate-acid igneous rock zone and a new understanding of structure evolution in the northern part of the Tarim basin. Acta Mineralogica Sinica, 18(3):370-376 (in Chinese with English abstract).

[5] Chen, C.M., Lu, H.F., Jia, D., Cai, D.S., Wu, S.M., 1999. Closing history of the southern Tianshan oceanic basin, western China: an oblique collisional orogen. Tectonophysics, 302(1-2):23-40.

[6] Fan, X.T., Lu, H.F., Shi, H.S., Guo, H.D., Shao, Y., 2000. Extraction of weak structural information and evidences of sinistral strike-slip in Kalpin area. Geological Journal of China Universities, 6(1):23-28 (in Chinese with English abstract).

[7] Guo, L.Z., Shi, Y.S., Lu, H.F., Ma, R.S., 1992. Two Long Distance Effect of India-Asia Plate Collision. In: Li, Q.B., Dai, J.X., Liu, R.Q., Li, J.L. (Eds.), Corpus of Modern Geology Research (Part 1). Nanjing University Press, Nanjing, p.1-7 (in Chinese).

[8] He, Z.L., Luo, C.R., Gong, M., 2001. Complex Petroleum System and Cycle Basin in Tarim. Chinese Geology University Press, Wuhan, p.8-18 (in Chinese).

[9] He, W.Y., Li, J.H., Qian, X.L., Zheng, D.M., 2002. Analysis of fault structures in the Kalpin fault uplift, Tarim basin. Geology in China, 29(2):37-43 (in Chinese with English abstract).

[10] Hendrix, M., Damitru, T., Graham, S., 1994. Late Oligocene-early Miocene unroofing in the Chinese Tian Shan: an early effect of the India-Asia collision. Geology, 22(6):487-490.

[11] Jia, C.Z., 1997. The Structural Feature and Petroleum in Tarim Basin, China. Petroleum Industry Press, Beijing, p.1-438 (in Chinese).

[12] Jia, C.Z., Lu, H.F., 2004. Petroleum Accumulation and Exploration of Rejuvenation Foreland Thrust Belt of Kuqa-Kalpin. Science Press, Beijing, p.1-48 (in Chinese).

[13] Jia, C.Z., Yao, H.J., Gao, J., Zhou, D.Y., Wei, G.Q., 1992. Study on Formation System in Tarim Basin. In: Tong, X.G., Liang, D.G. (Eds.), Research Advance in Petroleum Geology in Tarim Basin. Science Press, Beijing, p.34-63 (in Chinese).

[14] Jia, D., Lu, H.F., Cai, D.S., 1998. Structural Features of northern Tarim basin: implication for regional structure and petroleum traps. AAPG, 82(1):147-159.

[15] Jolivet, M., Brumel, M., Seward, D., Xu, Z., 2001. Mesozoic and Cenozoic tectonics of the northern edge of the Tibetan plateau: fission track constraints. Tectonophysics, 343(1-2):111-134.

[16] Kang, Y.Z., Kang, Z.H., 1996. Structure evolution and oil and gas of Tarim basin. J. Southeast Asian Earth Sciences, 13(3-5):317-325.

[17] Liu, Z.H., Lu, H.F., Li, X.J., Jia, C.Z., Lei, G.L., Chen, C.M., Wang, G.Q., Fan, X.T., 2000. Structure evolution of the Kuqa foreland basin. Scientia Geologica Sinica, 35:482-492 (in Chinese with English abstract).

[18] Lu, H.F., Jia, C.Z., 2003. Structure of Rejuvenation Foreland Thrust Belt of Kuqa-Kalpin. Science Press, Beijing, p.67-75 (in Chinese).

[19] Lu, H.F., Jia, D., Cai, D.S.,Wu, S.M., Chen, C.M., Shi, Y.S., Guo, L.Z., 1998. On the Kalpin transpression tectonics of northwestern Tarim. Geological Journal of China Universities, 4(1):49-58 (in Chinese with English abstract).

[20] Lu, H.F., Chen, C.M., Liu, Z.H., Jia, D., Wang, G.Q., 2000. The structural features and origin of the Kuqa rejuvenation foreland thrust belt. Acta Petrolei Sinica, 21(3):18-24 (in Chinese with English abstract).

[21] Mattern, F., Schneider, W., 2000. Suturing of the Proto- and Paleo-Tethys oceans in the western Kunlun (Xinjiang, China). J. Asian Earth Sciences, 18(6):637-650.

[22] Molnar, P., Tapponnier, P., 1975. Cenozoic structures of Asia: effects of continental collision. Science, 189(4201):419-426.

[23] Sobel, E.R., Dumitru, T.A., 1997. Thrusting and exhumation around the margins of the western Tarim basin during the India-Asia collision. J. Geophys. Res., 102(b3):5043-5063.

[24] Tang, L.J., 1994. Structure evolution and structural style of Tarim basin. Earth Science―J. China University of Geosciences, 19(6):742-745 (in Chinese with English abstract).

[25] Tang, L.J., Jia, C.Z., Pi, X.J., Chen, S.P., Wang, Z.Y., Xie, H.W., 2003. Evaporite-associated structure styles in Kuqa foreland fold belt. Science in China (Series D), 33:38-46 (in Chinese with English abstract).

[26] Tian, Z.J., 1996. Structural Styles and Petroleum Prospecting of Southern Tianshan Orogenic Belt and Northern Tarim Foreland Basin. Press of Chengdu University of Science and Technology, Chengdu, p.132 (in Chinese).

[27] Wang, X., 2005. Geometry and kinematics of complex folds, illustrated with examples from Quilitake Anticline of Kuqa and Bapanshuimo Anticline of Keping, Southern Tianshan. Geological Journal of China, 11(4):568-576 (in Chinese with English abstract).

[28] Wang, X., Jia, C.Z., Hubert-Ferrari, A., Suppe, J., 2001. Estimation of the shortening rate since late Pleistocene in the Aksu area on the southern flank of the Tianshan, China. Science in China (Series D), 44(8):708-715 (in Chinese with English abstract).

[29] Wang, Z.H., 2004. Structure evolution of the western Kunlun orogenic belt, western China. J. Asian Earth Sciences, 24(2):153-161.

[30] Windley, B.F., Allen, M.B., Zhang, C., Zhao, Z.Y., Wang, G.R., 1990. Paleozoic accretion and Cenozoic redeformation of the Chinese Tian Shan Range, central Asia. Geology, 18(2):128-131.

[31] Wu, X.F., Wang, X., Yang, S.F., 2004. Analysis on structural sections in the Cenozoic Pamir-Western Kunlun foreland fold-and-thrust belt. Chinese Journal of Geology, 29(2):260-271 (in Chinese with English abstract).

[32] Xiao, A.C., Yang, S.F., Li, Y.J., Wang, Q.H., Chen, H.L., 2005. A studying of Cenozoic fracture systems in Bachu-Kalpin area, Tarim Basin. Oil & Gas Geology, 26(1):78-85 (in Chinese with English abstract).

[33] Xie, X.A., Hu, S.Y., Lu, H.F., 1998. Positive inversion structure in the Bachu fault-uplift in the Tarim basin. Geological Review, 44(1):1-6 (in Chinese)

[34] Yang, G., Guo, H., 2003. Superposed relationship between Kalpin thrust belt and Buch uplift, northwest Tarim. Uranium Geology, 19(1):1-7 (in Chinese).

[35] Yang, X.P., Ran, Y.K., Song, F.M., Xu, X.W., Cheng, J.W., Min, W., Han, Z.J., Chen, L.C., 2006. The analysis for crust shortening of Kalpin thrust structure zone. Seismology and Geology, 28(2):194-204 (in Chinese).

[36] Yang, Y., Liu, M., 2002. Cenozoic deformation of the Tarim plate and the implications for mountain building in the Tibetan Plateau and the Tian Shan. Tectonics, 21(6):1059-1075.

[37] Yang, M.H., Jin, Z.J., Lu, X.X., Pan, W.Q., Hu, J.F., 2007. Basement-involved transpressional structure and the formation of the Bachu Uplift, Tarim Basin, northwestern China. Acta Geologica Sinica, 81(2):158-165.

[38] Yin, A., Nie, S., Craig, P., Harrison, T.M., Ryerson, F.J., Qian, X.L., Yang, G., 1998. Late Cenozoic structure evolution of the southern Chinese Tian Shan. Tectonics, 17(1):1-27.

[39] Zhang, S.B., Ni, Y.N., Gong, F.H., Lu, H.N., Huang, Z.B., Lin, H.L., 2003. Investigate Instruction of Periphery Formation of Tarim Basin. Petroleum Industry Press, Beijing, p.9-123 (in Chinese).

Open peer comments: Debate/Discuss/Question/Opinion

<1>

Please provide your name, email address and a comment





Journal of Zhejiang University-SCIENCE, 38 Zheda Road, Hangzhou 310027, China
Tel: +86-571-87952783; E-mail: cjzhang@zju.edu.cn
Copyright © 2000 - 2024 Journal of Zhejiang University-SCIENCE