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Wei LI, Shuping CHEN, Jinbiao YUN, Zhina LIU, Shilin LIU, Hongying JI. FORMATION MECHANISM OF STEEPLY INCLINED REVERSE FAULT: TAKE THE SERIKBUYA FAULT IN TARIM BASIN AS AN EXAMPLE[J]. Journal of Geomechanics, 2018, 24(1): 1-8. doi: 10.12090/j.issn.1006-6616.2018.24.01.001
Citation: Wei LI, Shuping CHEN, Jinbiao YUN, Zhina LIU, Shilin LIU, Hongying JI. FORMATION MECHANISM OF STEEPLY INCLINED REVERSE FAULT: TAKE THE SERIKBUYA FAULT IN TARIM BASIN AS AN EXAMPLE[J]. Journal of Geomechanics, 2018, 24(1): 1-8. doi: 10.12090/j.issn.1006-6616.2018.24.01.001
shu

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

  • 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

Received Date:  17 April 2017
Revised Date:  17 January 2018
    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.
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