岩性油气藏 ›› 2021, Vol. 33 ›› Issue (3): 5462.doi: 10.12108/yxyqc.20210305
苏敏1,2, 吴康军1,2, 李志军1,2, 曾东方3, 陈颖1,2, 卢科良1,2, 朱敏1,2, 龚燕秀4
SU Min1,2, WU Kangjun1,2, LI Zhijun1,2, ZENG Dongfang3, CHEN Ying1,2, LU Keliang1,2, ZHU Min1,2, GONG Yanxiu4
摘要: 川中北部磨溪-高石梯地区是四川盆地天然气的主要产区,但该区地层水特征及其油气地质意义方面的研究比较薄弱。基于油气运移聚集理论,在分析地层水的离子组成、化学参数、氢氧同位素等特征的基础上,揭示了地层水特征与油气聚集的关系。结果表明:龙王庙组、长兴组、雷一1亚段和须家河组的地层水均以CaCl2型为主,嘉二段以CaCl2,MgCl2,Na2SO4等3种水型为主。雷一1亚段和须家河组地层水的矿化度高,龙王庙组次之,嘉二段和长兴组的矿化度低。5个产层地层水的钠氯系数为0.3~0.8,镁钙系数为0.1~0.5,其中嘉二段脱硫系数最大(大于2),龙王庙组脱硫系数为0.2~0.5,长兴组和雷一1亚段脱硫系数相当,为0.1~0.8,须家河组脱硫系数为0。川中北部地区天然气保存条件较好,须家河组封闭性最好,岩-水作用强,嘉二段封闭性最差,岩-水作用弱。
中图分类号:
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