塔中北坡“复合花状”构造发育特征及成因机制

韩晓影; 汤良杰; 曹自成; 魏华动; 付晨阳

doi:10.3799/dqkx.2017.600

Volume 43 Issue 2

Feb. 2018

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Article Navigation > Earth Science > 2018 > 43(2): 525-537

Han Xiaoying, Tang Liangjie, Cao Zicheng, Wei Huadong, Fu Chenyang, 2018. Characteristics and Formation Mechanism of Composite Flower Structures in Northern Slope of Tazhong Uplift, Tarim Basin. Earth Science, 43(2): 525-537. doi: 10.3799/dqkx.2017.600

Citation:

Han Xiaoying, Tang Liangjie, Cao Zicheng, Wei Huadong, Fu Chenyang, 2018. Characteristics and Formation Mechanism of Composite Flower Structures in Northern Slope of Tazhong Uplift, Tarim Basin. Earth Science, 43(2): 525-537. doi: 10.3799/dqkx.2017.600

Citation:

Han Xiaoying, Tang Liangjie, Cao Zicheng, Wei Huadong, Fu Chenyang, 2018. Characteristics and Formation Mechanism of Composite Flower Structures in Northern Slope of Tazhong Uplift, Tarim Basin. Earth Science, 43(2): 525-537. doi: 10.3799/dqkx.2017.600

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Characteristics and Formation Mechanism of Composite Flower Structures in Northern Slope of Tazhong Uplift, Tarim Basin

doi: 10.3799/dqkx.2017.600

1.
State Key Laboratory of Petroleum Resource and Prospecting, China University of Petroleum, Beijing 102249, China
2.
College of Geosciences, China University of Petroleum, Beijing 102249, China
3.
Exploration and Production Research Institute of Northwest Oilfield Branch Company, SINOPEC, Urumqi 830000, China

Received Date: 2017-09-30
Publish Date: 2018-02-15

Abstract

Abstract

Developmental stages and mechanisms of the strike-slip faults on the northern slope of the Tarim basin remains controversial despite many studies. However, a more detailed study of the strike-slip faults in the area is possible due to the availability of high-quality 3D seismic data now. It is found that a series of strike-slip faults, which cut through the basement strata and straight up to the Middle Devonian strata, developed in the study area based on detailed 3D seismic interpretations. On the 3D seismic profiles, the strike-slip fault shows complex geometric feature that consists of a lower positive flower structure and an upper negative flower structure that is bounded by the Late Ordovician strata. On the seismic coherency slices, the lower strike-slip faults show NE linear extension and the upper strike-slip faults are NW trending and present right-order en-echelon arrangements. According to changes of the rising height of the interface and fault throw changes, the development history of the strike-slip faults may be divided into two stages including the Late Ordovician and the Middle Silurian-Middle Devonian. Combined with tectonic background analyses on the structures surrounding Tarim basin, the lower strike-slip faults and the upper en-echelon normal faults may be genetically linked. In the Late Ordovician, the Tazhong uplift experienced a strong compression from ancient Kunlun ocean subducting in NE direction, which resulted in the formation of NNE-trending strike-slip faults. During the Middle Silurian-Middle Devonian, intense folding orogeny of the Arkin tectonic domain caused the reactivation of the lower strike-slip faults and made the formation of the en-echelon normal faults was controlled by the early-stage basement weak zones.
- strike-slip fault,
- composite flower structure,
- linear structure,
- en-echelon normal fault,
- northern slope of Tazhong uplift,
- petroleum geology

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References(60)

References

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