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沾化凹陷仓储层的孔隙度和埋深对油气运聚的影响 被引量:6
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作者 吕希学 《油气地质与采收率》 CAS CSCD 北大核心 2011年第6期6-8,13,共4页
在不考虑幕式排烃的情况下,对沾化凹陷成藏期仓储层进行研究,揭示了仓储层的孔隙度和埋深与油气运聚间的关系。在对现今仓储层的厚度、物性和埋深等基本特征研究的基础上,通过对沉积埋藏史的分析,建立成藏期仓储层埋深及孔隙度的演化函... 在不考虑幕式排烃的情况下,对沾化凹陷成藏期仓储层进行研究,揭示了仓储层的孔隙度和埋深与油气运聚间的关系。在对现今仓储层的厚度、物性和埋深等基本特征研究的基础上,通过对沉积埋藏史的分析,建立成藏期仓储层埋深及孔隙度的演化函数,恢复成藏期仓储层的古埋深和古孔隙度;利用公式计算出成藏期仓储层内油气运移所受的浮力及毛管压力,根据浮力与毛管压力的差值判断仓储层内油气的运聚状态,当差值为正时,说明运移的动力大于运移的阻力,仓储层以运移油气为主;当差值为负时,说明运移的动力小于运移的阻力,油气不能在仓储层中运移,表现为成毯或成藏的状态。利用动、阻力差值的分布规律,结合古孔隙度、古埋深的恢复结果,可对油气运移、成藏的孔隙度和埋深等要素进行界定。结果表明,沾化凹陷古仓储层油气运移的孔隙度下限为34.5%,埋深下限为1300m;现今仓储层油气运移的孔隙度下限为30.9%,埋深下限为1789m。 展开更多
关键词 仓储层网毯式油气成藏体系毛管压力浮力沾化凹陷
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CHARACTERISTICS OF FLUID PRESSURE IN THE TERTIARY DAMINTUN SUB-BASIN OF LIAOHE BASIN IN NORTH CHINACHARACTERISTICS OF FLUID PRESSURE IN THE TERTIARY DAMINTUN SUB-BASIN OF LIAOHE BASIN IN NORTH CHINA 被引量:1
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作者 YE Jia-ren HAO Fang +1 位作者 CHEN Jian-yu CHEN Zhen-yan 《海洋地质与第四纪地质》 CAS CSCD 北大核心 2003年第4期83-94,共12页
The Damintun sub-basin is one of the four sub-basins in the Liaohe basin in North China, and regarded as a rift basin initiated in the Paleogene. Synthesizing the data from boreholes, well tests and seismic surveys, t... The Damintun sub-basin is one of the four sub-basins in the Liaohe basin in North China, and regarded as a rift basin initiated in the Paleogene. Synthesizing the data from boreholes, well tests and seismic surveys, the characteristics of pressure of the Damintun sub-basin are discussed in detail. From the data of sonic logs in 57 wells, shale in the Damintun sub-basin could be of normally pressured, overpressured or highly overpressured characteristics. From 391 pres-sure measurements from 152 wells, pressure-depth gradient in oil-producing intervals is near to unity in general. The fluid-pressures, excess pressures and pressure coefficients in 47 representative seismic profiles were predicted using seismic methods. The resultant pressure profiles showed normal pressure, slight overpressure and intense overpressure increasing with depth. Using the basic principles of fluid pressure evolution and data from drilling, lithology and well tests,the pres-sure evolution in profiles was restored. It showed that the pressure evolution can be divided into three stages of initial over-pressure accumulation, partly overpressure dissipation and overpressure re- accumulation. The intensities of abnormal pres-sures in the Damintun sub-basin were less than those in other areas in the Bohai Bay basin. 展开更多
关键词 pressure distribution pressure evolution intensity of overpressure Damintun sub-basin
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