A REVIEW ON THE RESEARCH PROGRESS OF SPATIAL CHARACTERISTICS OF LISTRIC FAULT

CHEN Ya-jun; FU Guang; BAO Ying-chun; HU Ming; CHEN Xue-qing; LI Shi-zhao

Volume 23 Issue 3

Jun. 2017

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CHEN Ya-jun, FU Guang, BAO Ying-chun, et al., 2017. A REVIEW ON THE RESEARCH PROGRESS OF SPATIAL CHARACTERISTICS OF LISTRIC FAULT. Journal of Geomechanics, 23 (3): 451-458.

Citation:

CHEN Ya-jun, FU Guang, BAO Ying-chun, et al., 2017. A REVIEW ON THE RESEARCH PROGRESS OF SPATIAL CHARACTERISTICS OF LISTRIC FAULT. Journal of Geomechanics, 23 (3): 451-458.

Citation:

CHEN Ya-jun, FU Guang, BAO Ying-chun, et al., 2017. A REVIEW ON THE RESEARCH PROGRESS OF SPATIAL CHARACTERISTICS OF LISTRIC FAULT. Journal of Geomechanics, 23 (3): 451-458.

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A REVIEW ON THE RESEARCH PROGRESS OF SPATIAL CHARACTERISTICS OF LISTRIC FAULT

1.
School of GeoSciences in Northeast Petroleum University, Daqing, Heilongjiang Province, 163318, China
2.
Daqing Oil Field company with limited liability, first oil production plant, Heilongjiang, Daqing, 163001, China

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Received: 2017-02-06
Published: 2017-06-28

Abstract

Abstract

Affected by the multiple solutions and limitations of the seismic data interpretation, seismic data interpretation in sedimentary basin is of poor quality and the fault information from seismic data interpretation can't expose the characteristics of the fault space development. With that in mind, based on the brittle plasticity fault development characteristics and fault refraction mechanism, the listric fault spatial characteristics were studied from the aspects of fault spatial displacement relation, inclination angle shearing method model and fault plane spatial combined stress distribution. The comprehensive study results show that the space formed by the hanging wall and footwall of listric fault isn't in a wedge mode but an alternative mode between local compact structure zone and local extension peeling zone. According to the diagram of the displacement relation of the fault space, the smaller the included angle θ between listric fault strike displacement and dip displacement, the greater the stress along trend, the higher of the traction degree towards the stratum, and the thicker the oil-bearing structure favorable to accumulate oil. Inclined shearing method model can predict the actual slip depth of listric faults, strengthening the consciousness of the structure characteristics of middle and deep structures. Listric fault is closed while it's fault plane refraction crack filled by mineral vein, and when combined stress of listric fault plane space is greater than or equal to its compressive strength affecting on rocks, it will cause the closure of the crack or the material compaction, which is favorable for the seal of oil and gas.
- listric fault,
- fault refraction,
- lnclination angle shearing method,
- spatial displacement,
- combined stress

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References(28)

References

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