塔里木盆地巴楚隆起西段边界断层联接及变形特征

张宇航; 汤良杰; 邱海峻; 云露; 杨勇; 谢大庆; 蒋华山

doi:10.3799/dqkx.2013.057

Volume 38 Issue 3

May 2013

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Article Navigation > Earth Science > 2013 > 38(3): 573-580

ZHANG Yu-hang, TANG Liang-jie, QIU Hai-jun, YUN Lu, YANG Yong, XIE Da-qing, JIANG Hua-shan, 2013. Linkages of the Boundary Faults and Deformation Features in the West of Bachu Uplift, Tarim Basin. Earth Science, 38(3): 573-580. doi: 10.3799/dqkx.2013.057

Citation:

ZHANG Yu-hang, TANG Liang-jie, QIU Hai-jun, YUN Lu, YANG Yong, XIE Da-qing, JIANG Hua-shan, 2013. Linkages of the Boundary Faults and Deformation Features in the West of Bachu Uplift, Tarim Basin. Earth Science, 38(3): 573-580. doi: 10.3799/dqkx.2013.057

Citation:

ZHANG Yu-hang, TANG Liang-jie, QIU Hai-jun, YUN Lu, YANG Yong, XIE Da-qing, JIANG Hua-shan, 2013. Linkages of the Boundary Faults and Deformation Features in the West of Bachu Uplift, Tarim Basin. Earth Science, 38(3): 573-580. doi: 10.3799/dqkx.2013.057

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Linkages of the Boundary Faults and Deformation Features in the West of Bachu Uplift, Tarim Basin

doi: 10.3799/dqkx.2013.057

ZHANG Yu-hang^{1, 2
,},
TANG Liang-jie^{1, 2},
QIU Hai-jun³,
YUN Lu⁴,
YANG Yong^{1, 2},
XIE Da-qing⁴,
JIANG Hua-shan⁴

1.
State Key Laboratory of Petroleum Resource and Prospecting, China University of Petroleum, Beijing 102249, China
2.
Basin and Reservoir Research Center, China University of Petroleum, Beijing 102249, China
3.
Oil and Gas Resources Strategic Research Center, Ministry of Land and Resources, Beijing 100034, China
4.
Northwest Oilfield Company, SINOPEC, Urumqi 830011, China

Received Date: 2012-08-20
Publish Date: 2013-05-15

Abstract

Abstract

Based on the interpretation of the new drilling and seismic data, the structural characteristics of the Selibuya fault and Kangtakumu fault, which are the boundary faults between the western Bachu uplift and Maigaiti slope, are analyzed in this paper. The Selibuya and Kangtakumu faults are basement-involved thrust faults interacting by soft-linkage. Along the SE strike, the displacement of the Selibuya fault gradually decreases, while the displacement of the Kangtakumu fault increases. The transform zone between the two faults transferred their displacements, and kept the conservation of fault displacements in western part of the Bachu Uplift. The transform zone belongs to the synthetic overlapping zone which is in the evolution stage of complex. There are much secondary faults and fractures, which is good basis for the formation of fractured-type reservoirs and hydrocarbon migration. The transform zone is the favorable objective for petroleum exploration in the Bachu area.
- faults soft linkage,
- transfer zone,
- Selibuya fault,
- Kangtakumu fault,
- Bachu uplift,
- petroleum,
- structural geology

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References(34)

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Linkages of the Boundary Faults and Deformation Features in the West of Bachu Uplift, Tarim Basin

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