FORMATION MECHANISM OF STEEPLY INCLINED REVERSE FAULT: TAKE THE SERIKBUYA FAULT IN TARIM BASIN AS AN EXAMPLE

LI Wei; CHEN Shuping; YUN Jinbiao; LIU Zhina; LIU Shilin; JI Hongying

doi:10.12090/j.issn.1006-6616.2018.24.01.001

Volume 24 Issue 1

Feb. 2018

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LI Wei, CHEN Shuping, YUN Jinbiao, et al., 2018. FORMATION MECHANISM OF STEEPLY INCLINED REVERSE FAULT: TAKE THE SERIKBUYA FAULT IN TARIM BASIN AS AN EXAMPLE. Journal of Geomechanics, 24 (1): 1-8. DOI: 10.12090/j.issn.1006-6616.2018.24.01.001

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FORMATION MECHANISM OF STEEPLY INCLINED REVERSE FAULT: TAKE THE SERIKBUYA FAULT IN TARIM BASIN AS AN EXAMPLE

doi: 10.12090/j.issn.1006-6616.2018.24.01.001

LI Wei^{1, 2
,},
CHEN Shuping^{1, 2},
YUN Jinbiao³,
LIU Zhina^{1, 2},
LIU Shilin³,
JI Hongying^{1, 2}

1.
State Key Laboratory of Petroleum Resources and Prospecting, China University of Petroleum, Beijing 102249, China
2.
College of Geosciences, China University of Petroleum, Beijing 102249, China
3.
Institute of Exploration and development, Sinopec, Beijing 100083, China

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Received: 2017-04-17
Revised: 2018-01-17
Published: 2018-02-01

Abstract

Abstract

Many steeply inclined reverse faults have developed in basins of western China, but we have not yet gained an unified understanding of their formation mechanism. The Serikbuya fault is located in the western Tarim Basin and it is a typical steeply inclined reverse fault, which provides a good example to study the formation mechanism of steeply inclined reverse fault. According to the latest seismic profiles and stratigraphic analysis, the inclination of the upper part of the Serikbuya fault is about 65°. The Serikbuya fault formed through two-staged tectonic movement. The first period ranged from Late Caledonian movement to early Hercynian movement(439~362 Ma), and the second period was during the Medium Himalayan movement(23.3~5.3 Ma). It is the multi-stage movements of the fault that formed the upper steeply inclined fault. That is, the movement of the previous gently inclined reverse fault changed the local stress field and promoted the maximum stress spindle from horizontal to tilt. Then the Coulomb fault inclination occurred steep and back thrusts appeared. At the same time, the results of digital sandbox simulation are used to confirm the above inferences.
- the Serikbuya fault,
- Tarim Basin,
- steeply inclined reverse fault,
- digital sandbox,
- formation mechanism

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FORMATION MECHANISM OF STEEPLY INCLINED REVERSE FAULT: TAKE THE SERIKBUYA FAULT IN TARIM BASIN AS AN EXAMPLE

doi: 10.12090/j.issn.1006-6616.2018.24.01.001

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FORMATION MECHANISM OF STEEPLY INCLINED REVERSE FAULT: TAKE THE SERIKBUYA FAULT IN TARIM BASIN AS AN EXAMPLE

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