Oil & Gas Geology ›› 2011, Vol. 32 ›› Issue (2): 259-264,301.doi: 10.11743/ogg20110214
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Abstract: Sedimentary system in the Liaohe Basin could be divided into prestrikeslip sequence, synstrikeslip sequence, and poststrikeslip sequence according to the strength of strikeslip activities. The poststrikeslip sequence, which was slightly influenced by the strikeslip activities, could be restored by traditional methods of balanced crosssection. By contrast, the syn and pre strikeslip sequences, significantly controlled and influenced by the strikeslip activities, have to be restored with different thickness on both sides of the fault to balance the volume in twodimension. The quantitative balanced crosssection restoration of the strikeslip basin reveals the structural evolution process of the study area during the Mesozoic and Cenozoic. Balanced cross sections in Haiwaihe area show that the Liaohe Basin underwent progressively extension and depression during the Mesozoic, and evolved into a rift basin in the Cenozoic. The basin was modified by the NEtrending dextral strikeslip during the deposition of the first and second members of Shahejie Formation, and was uplifted and eroded again after the deposition of the Dongying Formation. Finally, based on a comprehensive analysis of the petroleum geological characteristics in Haiwaihe area, this paper discusses the model of hydrocarbon accumulation and prospects for exploration.
Key words: Key words: strikeslip activity, balanced crosssection restoration, structural evolution, Haiwaihe area, Liaohe Basin
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URL: http://ogg.pepris.com/EN/10.11743/ogg20110214
http://ogg.pepris.com/EN/Y2011/V32/I2/259