STUDY ON STRUCTURAL STRESS FIELDS SINCE PERMIAN, BACHU AREA, TARIM BASIN

LI Le; HOU Gui-ting; PAN Wen-qing; JU Yan; ZHANG Qing-lian; SHU Wu-lin; XIAO Fang-feng; JU Wei

Volume 17 Issue 3

Sep. 2011

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Article Navigation > Journal of Geomechanics > 2011 > 17(3): 262-273

LI Le, HOU Gui-ting, PAN Wen-qing, et al., 2011. STUDY ON STRUCTURAL STRESS FIELDS SINCE PERMIAN, BACHU AREA, TARIM BASIN. Journal of Geomechanics, 17 (3): 262-273.

Citation:

LI Le, HOU Gui-ting, PAN Wen-qing, et al., 2011. STUDY ON STRUCTURAL STRESS FIELDS SINCE PERMIAN, BACHU AREA, TARIM BASIN. Journal of Geomechanics, 17 (3): 262-273.

Citation:

LI Le, HOU Gui-ting, PAN Wen-qing, et al., 2011. STUDY ON STRUCTURAL STRESS FIELDS SINCE PERMIAN, BACHU AREA, TARIM BASIN. Journal of Geomechanics, 17 (3): 262-273.

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STUDY ON STRUCTURAL STRESS FIELDS SINCE PERMIAN, BACHU AREA, TARIM BASIN

LI Le^{1, 2, 3
,
,},
HOU Gui-ting^{1, 2, 3},
PAN Wen-qing⁴,
JU Yan⁴,
ZHANG Qing-lian^{1, 2, 3},
SHU Wu-lin^{1, 2, 3},
XIAO Fang-feng^{1, 2, 3},
JU Wei^{1, 2, 3}

1.
School of Earth and Space Science, Peking University, Beijing 100871, China
2.
The Key Laboratory of Orogenic Belts and Crustal Evolution, Ministry of Education, Beijing 100871, China
3.
Institute of Oil and Gas Research, Peking University, Beijing 100871
4.
Institute of Exploration and Development, Tarim Oil and Gas Branch Company, Korla 841000, Xinjiang, China

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Abstract

Abstract

Three periods of structural stress fields can be recognized since Permian in northwest of Tarim Basin and adjacent areas based on structural evolution analysis, which is the end of Permian, the Triassic to paleogene and Neogene. Based on the research of stress-response structures of dykes, joints, slickensides, folds and faults, and analysis of the comparison characters of field of stress, it is found that the direction of the maximum principal stress formed by the collision of middle Tianshan island arc and Tarim basin was NW. The direction of maximum principal stress Triassic to paleogene was NNE, which developed by repression of dextrorotary of Tarim basin. And it was N-S direction since Neogene in Bachu area as a result of the collision of Indian plate with Eurasian plate. Furthermore, the authors simulated the stress field since Neogene based on 2D finite-element method, to deeply analyze the distribution and direction of stresses in the research area.
- Tarim Basin,
- Bachu area,
- structural stress fields,
- maximum principal stress

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References(32)

References

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