Interpretation Methods and Application of Small Faults

Huan Song Ren; Shuang Fang Lu; Dian Shi Xiao

doi:10.4028/www.scientific.net/AMR.962-965.132

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HomeAdvanced Materials ResearchAdvanced Materials Research Vols. 962-965Interpretation Methods and Application of Small...

Interpretation Methods and Application of Small Faults

Abstract:

It is difficult to distinguish off from <5m fault in sections, because lateral variation of the amplitude and changes arising from differential compaction sand. Seismic coherence cube is to highlight those irrelevant seismic data. Draw three-dimensional seismic coherence with Partial wave analysis in the longitudinal and transverse. Ant agents: the ant, which found in the seismic data volume to meet the pre-fracture conditions, will release of a “signal”. It can call other regions ant for focusing on the breaks in its tracks, until the completion of the fault tracking and identification. Structural heterogeneity imaging can generate several geological attribute bodies, when compound with different geological attribute volume to different geology research target. It can extrude geologic feature we needed. Identifying a series of small faults which development between the main faults using a variety of small faults interpretation. Discovering and implementation of a number of block trap.

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Periodical:

Advanced Materials Research (Volumes 962-965)

Pages:

132-137

DOI:

https://doi.org/10.4028/www.scientific.net/AMR.962-965.132

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Online since:

June 2014

Authors:

Huan Song Ren*, Shuang Fang Lu, Dian Shi Xiao

Keywords:

Ant Agents, Block Trap, Seismic Coherence Cube, Small Fault, Structural Heterogeneity Imaging

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* - Corresponding Author

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