塔里木盆地顺北地区下古生界走滑断裂带断距分段差异与断层宽度关系

周铂文; 陈红汉; 云露; 唐大卿

doi:10.3799/dqkx.2021.073

Volume 47 Issue 2

Feb. 2022

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Article Navigation > Earth Science > 2022 > 47(2): 437-451

Zhou Bowen, Chen Honghan, Yun Lu, Tang Daqing, 2022. The Relationship between Fault Displacement and Damage Zone Width of the Paleozoic Strike-Slip Faults in Shunbei Area, Tarim Basin. Earth Science, 47(2): 437-451. doi: 10.3799/dqkx.2021.073

Citation:

Zhou Bowen, Chen Honghan, Yun Lu, Tang Daqing, 2022. The Relationship between Fault Displacement and Damage Zone Width of the Paleozoic Strike-Slip Faults in Shunbei Area, Tarim Basin. Earth Science, 47(2): 437-451. doi: 10.3799/dqkx.2021.073

Citation:

Zhou Bowen, Chen Honghan, Yun Lu, Tang Daqing, 2022. The Relationship between Fault Displacement and Damage Zone Width of the Paleozoic Strike-Slip Faults in Shunbei Area, Tarim Basin. Earth Science, 47(2): 437-451. doi: 10.3799/dqkx.2021.073

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The Relationship between Fault Displacement and Damage Zone Width of the Paleozoic Strike-Slip Faults in Shunbei Area, Tarim Basin

doi: 10.3799/dqkx.2021.073

Zhou Bowen^{1
,
,},
Chen Honghan^{1
,
,
,},
Yun Lu²,
Tang Daqing¹

1.
Faculty of Earth Resources, China University of Geosciences, Wuhan 430074, China
2.
Sinopec Northwest Oil Company, Urumqi 830011, China

Received Date: 2021-10-11
Publish Date: 2022-02-25

Abstract

Abstract

The Lower Paleozoic No.1 and No.5 strike-slip faults in Shunbei area of Tarim Basin are hot spots for oil and gas exploration at present. It is of great significance to characterize the structure of strike-slip fault zone for exploration and development. The vertical fault spacing and fault width of the Lower Paleozoic were calculated with 200 m vertical interval, and the quantitative relationship between the vertical fault spacing and fault width was established. The results showed that: (1) T74 is the main interface and top-down development in middle Caledonian Ⅲ episode of SB1 strike-slip faults; The en-echelon normal faults are mainly developed in T70 with bottom to top development. T74 is the main interface pressure ridge segment development activities during the middle Caledonian Ⅲ episode in SB5 faults, bottom-up inheritance deformation to T63 interface; In the late Caledonian period, the whole pull-apart activity occurred, and from the T70 interface, the main fault surface was connected with the pressure ridge structure in the form of graben structure and inherited. (2)There is a positive correlation between the vertical fault distance (x) and the fault damage zone width (y) of the strike-slip faults in Shunbei area. Shunbei No.1 fault: y=42.206x+137.74, R²=0.740 4;Shunbei No.5 fault: y=0.072 6x²+15.85x+196.95, R²=0.774 9.
- strike-slip fault,
- fault displacement,
- damage zone width,
- segmented differences,
- Shunbei area,
- Tarim Basin,
- tectonics

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References(42)

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The Relationship between Fault Displacement and Damage Zone Width of the Paleozoic Strike-Slip Faults in Shunbei Area, Tarim Basin

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