Characteristics of Geotemperature-Geopressure System of the Qianjiang Formation in the Qianjiang Depression and Their Relationship with Petroleum Accumulation
详细信息   
摘要
///Based on the measured temperature, pressure and acoustic log data of more than two hundred wells, the distribution characteristics of geothermal field, geopressure field and the geothermal-geopressure system of the Qianjiang Formation in the Qianjiang Depression are analyzed by using the theory of geothermal-geopressure system. The results show that the Banghu and Zhouji syncline belts have higher geothermal gradient, which is favorable to the maturation of the Qianjiang Formation source rock expulsion. The present pressures of the Qianjiang Formation and stones mostly belong to normal range, whereas the deep Qianjiang Formation mudstones present uncompaction which enhanced its seal ability. In vertical, the T-P system of the Qianjiang Formation includes two kinds of static pressure and overpressure.

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