HYDROCHEMICAL CHARACTERISTICS OF FORMATION WATER AND THEIR SIGNIFICANCE IN JIANNAN GASFIELD, YUDONG AREA OF WEST HUBEI PROVINCE
-
摘要: 对建南气田地层水常规组分、微量元素、δD、δ18O、δ34S同位素测试成果的分析表明,该区水化学成分纵向变化不同于其它油田,并非正向型或反向型水化学剖面,彼此之间也不存在同源性,而是存在多套独立、封闭的水化学环境.a)香溪群(T3x)地层水有着良好的水化学封闭环境,地表水向下交替程度不大;b) 嘉二段以下具有多套独立而封闭的水化学环境,其中飞三段(T1f3)地层水在燕山晚期—喜山期通过断裂系统与黄龙组(C2h)地层水发生过水化学交替.Abstract: Analysis on the testing results of conventional components,trace elements and δD、δ18O and δ34S isotopes in the formation water of Jiannan gasfield showed that the longitudinal changes of hydrochemical components in this area were different from those in other oilfields.Several sets of independent and enclosed hydrochemical environments existed instead of positive or reverse-typed hydrochemical sections.They were not congenetic.T3x formation water has good enclosed hydrochemical environments,and the alternation degree of surface water downward is not great.Below T1j2,there are several independent and enclosed hydrochemical environments.Among them,hydrochemical alternation of T1f2 formation water with C2h formation water happened in the Late Yanshanina Himalayan period by fault systems.
-
Key words:
- formation water /
- hydrochemistry /
- Jiannan gasfield /
- Yudong area of West Hubei province /
-
[1] 蔡立国,钱一雄,刘光祥,等.塔河油田及邻区地层水成因探讨[J].石油实验地质,2002,24(1):57-60. [2] 董万百,林艳萍,高红.准噶尔盆地腹部及南缘水化学纵向变化规律[J].石油实验地质,2001,23(2):195-199. [3] 王仲侯.克拉玛依油区高矿化度重碳酸钠型水的发现与特征[J].石油实验地质,1998,20(1):39-43. [4] 孙向阳.东营凹陷地层水化学特征与油气聚集关系[J].石油实验地质,2001,23(3):291-296. [5] 杨绪充.油气田水文地质学[M].山东东营:石油大学出版社,1993.79-89. [6] 卢武长.稳定同位素地球化学[M].成都:成都地质学院,1986.117-118,135-142. [7] 郑永飞,陈江峰.稳定同位素地球化学[M].北京:科学出版社,2002.235-245. -
计量
- 文章访问数: 639
- HTML全文浏览量: 69
- PDF下载量: 372
- 被引次数: 0
下载:
苏公网安备32021102000780号