南京大学学报(自然科学版) ›› 2012, Vol. 48 ›› Issue (3): 308315.
石砒石1,2,解宝玉2,孟凡巍3 **
Shi Di-Shi1,Xie Bao一Yu2,Meng Fan Wei3
摘要: 油田水的成分和变化是含油气盆地演化历史的重要部分.由于油田水的取样十分困难且数据有限很难进行系统分析,木文通过包裹体显微测温学与油田水采样的结果相结合的方法,对东营牛庄洼陷中油田水的成分进行了研究.砂岩中穿插石英颗粒的最后一期包裹体,记录了最晚期的油田水成分.对最晚期的流体包裹体的显微测温学结果表明,晚期流体包裹体主要为NaCI - CaCI2一H2O体系,这与相同或者相近深度油井油田水采样的成分基木一致,证明了该方法的有效性.这种方法便捷、有效,有着良好发展前景.
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