2010•Dizhi lunpingRequires access

Characteristics of Fault Structure and Its Control on Deep Gas Reservoir in Xujiaweizi Fault Depression,Songliao Basin

Yu Dan

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Abstract

the characteristics of development and activity of fault in the Xujiaweizi fault depression,Songliao Basin,were analyzed. The control of fault on deep gas reservoir was investigated. Five cases of fault system were developed in the Xujiaweizi fault depression,including the western Xujiaweizi early extensional strike-slip fault system,central Xujiaweizi strike-slip long-term active fault system,eastern Xujiaweizi strike-slip fault system,early extensional and later tenso-shear long-term active fault system,later tenso-shear fault system. Fault activity periods are fault depression period,from K1q deposition to later stage——K1qn deposition period. The Xuxi early extensional strike-slip fault system control the distribution of K1sh source rock,the Xuzhong and Xudong strike-slip fault system control the distribution of K1yc1 and K1yc3volcanic,later-term activity fault was well vertical pathway of gas vertical migration. Fault destructiveness to K1d2 region cap-rock is poor,gas mainly accumulate k1yc formation in Xujiaweizi fault depression,the relationship of lithological juxtaposition was volcanic—sand shale,the fault was lateral seal,the relationship of lithological juxtaposition was volcanic—volcanic,the fault was not lateral seal,later structural reverse was poor,the damage degree of hydrocarbon by fault was poor,it was better to hydrocarbon conserve.

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What this paper is about

the characteristics of development and activity of fault in the Xujiaweizi fault depression,Songliao Basin,were analyzed. The control of fault on deep gas reservoir was investigated. Five cases of fault system were developed in the Xujiaweizi fault depression,including the western Xujiaweizi early extensional strike-slip fault system,central Xujiaweizi strike-slip long-term active fault system,eastern Xujiaweizi strike-slip fault system,early extensional and later tenso-shear long-term active fault system,later tenso-shear fault system. Fault activity periods are fault depression period,from K1q deposition to later stage——K1qn deposition period. The Xuxi early extensional strike-slip fault system control the distribution of K1sh source rock,the Xuzhong and Xudong strike-slip fault system control the distribution of K1yc1 and K1yc3volcanic,later-term activity fault was well vertical pathway of gas vertical migration. Fault destructiveness to K1d2 region cap-rock is poor,gas mainly accumulate k1yc formation in Xujiaweizi fault depression,the relationship of lithological juxtaposition was volcanic—sand shale,the fault was lateral seal,the relationship of lithological juxtaposition was volcanic—volcanic,the fault was not lateral seal,later structural reverse was poor,the damage degree of hydrocarbon by fault was poor,it was better to hydrocarbon conserve.

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Available abstract

the characteristics of development and activity of fault in the Xujiaweizi fault depression,Songliao Basin,were analyzed. The control of fault on deep gas reservoir was investigated. Five cases of fault system were developed in the Xujiaweizi fault depression,including the western Xujiaweizi early extensional strike-slip fault system,central Xujiaweizi strike-slip long-term active fault system,eastern Xujiaweizi strike-slip fault system,early extensional and later tenso-shear long-term active fault system,later tenso-shear fault system. Fault activity periods are fault depression period,from K1q deposition to later stage——K1qn deposition period. The Xuxi early extensional strike-slip fault system control the distribution of K1sh source rock,the Xuzhong and Xudong strike-slip fault system control the distribution of K1yc1 and K1yc3volcanic,later-term activity fault was well vertical pathway of gas vertical migration. Fault destructiveness to K1d2 region cap-rock is poor,gas mainly accumulate k1yc formation in Xujiaweizi fault depression,the relationship of lithological juxtaposition was volcanic—sand shale,the fault was lateral seal,the relationship of lithological juxtaposition was volcanic—volcanic,the fault was not lateral seal,later structural reverse was poor,the damage degree of hydrocarbon by fault was poor,it was better to hydrocarbon conserve.

Key concepts: Geology, Fault (geology), Strike-slip tectonics, Petrology, Shear (geology), Fault scarp, Growth fault, Seismology

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