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Effects of High Temperature and Overpressure on Deep Reservoir in Qiongdongnan Basin, Northwestern South China Sea

机译:高温和超压对南海西北琼通南盆地深层水库的影响

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Abnormal temperature and pressure with their effects on deep reservoir is the frontier in petroleum geology. Taking Qiongdongnan basin as a case study, the geological settings of this basin are primarily analyzed in this paper. Then, based on the full consideration of sedimentation and diagenesis, effects of abnormal temperature and pressure on deep reservoir are discussed. Main conclusions are drawn as following: (1) high geothermal or geothermal gradient accelerates the reduction of sandstone porosity, (2) high geothermal or geothermal gradient can improve the reservoir properties by promoting the dissolution of carbonate minerals, the filling of hydrocarbon and the development of overpressure, (3) overpressure can preserve partial primary pores, (4) overpressure can inhibit the growth of some cements and slow down the destruction of diagenesis on deep reservoir, and (5) overpressure can generate some secondary pores by enhancing dissolution.
机译:异常温度和压力与其对深层水库的影响是石油地质的前沿。将Qiongdongnan盆地以QIONGDONGNAN盆地为例,该盆地的地质环境主要分析本文。然后,基于对沉降和成岩作用的充分考虑,讨论了异常温度和压力对深层储层的影响。主要结论如下:(1)高地热或地热梯度加速砂岩孔隙率的减少,(2)高地热或地热梯度可以通过促进碳酸盐矿物的溶解,碳氢化合物填充和发育的溶解来提高储层性质过压,(3)过压可以保留部分原发性孔隙,(4)过压可以抑制一些水泥的生长,减缓深层储存器的成岩作用的破坏,(5)过压通过增强溶解可以产生一些次要孔隙。

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