RELATION BETWEEN GEOTHERMAL-GEOPRESSURE SYSTEM AND PETROLEUM ACCUMULATION IN MOLIQING RIFT IN YITONG BASIN
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摘要: 基于地温和地压实测数据及声波测井资料等,利用地温-地压系统的原理,对伊通盆地莫里青断陷的地温场、压力场及温压系统特征进行了剖析,并从油气生成、保存及分布角度探讨了温压系统与油气成藏的关系。研究表明,断陷内各区带地温梯度较高,有利于有机质的成熟与烃类生成;泥岩欠压实段主要出现在双阳组,强化了油气的封闭作用;斜坡带泥岩不发育异常压力,以毛细管压力封闭为主;莫里青断陷发育弱高压型复式温压系统,上下2套温压系统流体能量相差较小,油气垂向运聚活动很少,深部弱高压型温压系统内部最有利于油气富集成藏,双阳组含油气系统是最重要的勘探对象。Abstract: Based on the data of geothermal, geopressure and acoustic log, the characteristics of geothermal and geopressure fields and geothermal-geopressure system of Moliqing rift in Yitong basin are analyzed by using the theory of geothermal-geopressure system. The relation between geothermal-geopressure system and petroleum accumulation is also discussed on the view of hydrocarbon generation, preservation and distribution in the studied area. The research results show that Moliqing area presents high geothermal gradient which is favorable for organic matter maturation and hydrocarbon generation. Undercompaction mudstone appears in the Shuangyang Formation and it enhances the seal of oil-gas. Abnormal pressure does not occur in the ramp region, and capillary pressure acts as the main control factor for sealing the hydrocarbon. Moliqing rift has a geothermal-geopressure system with low overpressure. Because the fluid energy is similar between the upper and the lower geothermal-geopressure system, the vertical migration and accumulation of hydrocarbon are not obvious and the inner low overpressure system is most favorable for hydrocarbon accumulation. The Es2 petroleum system is the most important object for oil-gas exploration in this studied area.
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