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《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:

第46卷

期数:

2024年第05期

页码:

663-676

栏目:

沉积地质与油气勘探

出版日期:

2024-09-30

文章信息/Info

Title:

Geochemical Characteristics, Genesis and Source Correlation of Permian Formation Water in the Western Sulige Gas Field and the Northern Part of Tianhuan Depression, Ordos Basin, China

文章编号:

1672-6561(2024)05-0663-14

作者:

颜 凯¹; 2; 李博偲¹; 2; 徐建斌³; 徐学敏⁴; 丁佳伟¹; 2; 郑少威¹; 2; 潘志强¹; 2; 何大祥¹; 2*

(1. 长江大学 油气地球化学与环境湖北省重点实验室,湖北 武汉 430100; 2. 长江大学 资源与环境学院,湖北 武汉 430100; 3. 中国石油辽河油田分公司勘探开发研究院,辽宁 盘锦 124010; 4. 中国地质调查局 国家地质实验测试中心,北京 100037)

Author(s):

YAN Kai¹; 2;  LI Bo-cai¹; 2;  XU Jian-bin³;  XU Xue-min⁴;  DING Jia-wei¹; 2;  ZHENG Shao-wei¹; 2;  PAN Zhi-qiang¹; 2;  HE Da-xiang¹; 2*

(1. Hubei Key Laboratory of Petroleum Geochemistry and Environment, Yangtze University, Wuhan 430100, Hubei, China; 2. College of Resources and Environment, Yangtze University, Wuhan 430100, Hubei, China; 3. Research Institute of Oil Exploration and Development, Liaohe Oilfield Company, PetroChina, Panjin 124010, Liaoning, China; 4. National Research Center for Geoanalysis, Chinese Academy of Geological Sciences, Beijing 100037, China)

关键词:

地球化学;  地层水;  离子组成;  保存条件;  二叠系;  苏里格气田;  天环坳陷;  鄂尔多斯盆地

Keywords:

geochemistry;  formation water;  ion composition;  preservation condition;  Permian;  Sulige gas field;  Tianhuan depression;  Ordos Basin

分类号:

P641; P618.13

DOI:

10.19814/j.jese.2024.01027

文献标志码:

A

摘要:

鄂尔多斯盆地苏里格气田西区与天环坳陷北段是鄂尔多斯盆地重要的天然气富集区,其气水关系复杂,气水共存在二者上古生界二叠系气藏中大量存在,目前对上述两个地区二叠系地层水成因及来源的对比研究较为薄弱。通过对苏里格气田西区与天环坳陷北段二叠系35口井地层水样品开展地球化学特征研究,进一步揭示上述两个地区地层水成因、来源及保存条件的异同。结果表明:苏里格气田西区与天环坳陷北段二叠系地层水主体为CaCl₂型,总矿化度平均值分别为31.4和34.6 g·L^-1; 不同类型水化学参数指示了天环坳陷北段地层封闭性更好,两个地区整体经历了强烈的水-岩相互作用,油气保存条件好; 苏里格气田近源运移成藏以及生烃强度与储层非均质性的特点控制了气、水分布格局,天环坳陷北段存在的一系列构造裂缝系统对该区域的气、水分布具有一定的调整作用; 上述两个地区地层水主体为原始沉积地层水,地层中发生了斜长石的钠长石化及白云石化等作用,具有Ca²⁺富集、Na⁺轻微亏损、Mg²⁺亏损的特点。综合研究表明,苏里格气田西区地层水没有统一的气、水界面,局部井位遭受了外来水等流体影响; 天环坳陷北段各井位地层水可能属于统一的流体场。

Abstract:

The western Sulige gas field and the northern part of Tianhuan depression are significant natural gas rich zones within Ordos Basin. The relationship between gas and water is complicated, with gas-water coexistence observed in the Upper Paleozoic Permian gas reservoirs. At present, the study on the genesis and source correlation of Permian formation water in these two regions is relatively weak. By analyzing geochemical characteristics of Permian formation water samples from 35 wells in the above two regions, and the differences in formation water genesis, source, and preservation conditions were furtherly elucidated. The results show that the formation water from both regions are mainly CaCl₂-type, and the average TDS is 31.4 and 34.6 g·L^-1, respectively. The northern part of Tianhuan depression exhibits superior sealing characteristics based on various hydrochemical parameters, and the data also indicate strong water-rock interaction in the above two regions and good preservation conditions for oil and gas. The distribution pattern of gas and water in Sulige gas field is controlled by near-source migration characteristics, hydrocarbon generation intensity, and reservoir heterogeneity. Additionally, a series of structural fracture systems in the northern part of Tianhuan depression play a significant role in regulating the distribution of gas and water within this region. The formation water in the above two regions is mainly the original sedimentary formation water, and the albitization and dolomitization of plagioclase occur in the formation, showing the characteristics of Ca²⁺ enrichment, Na⁺ slight loss and Mg²⁺ loss. The analysis data consistently indicate that the interface between gas and water in the western Sulige gas field lacks uniformity, and local well locations are affected by external water and other fluids, while the formation water in the northern part of Tianhuan depression may belong to a unified fluid field.

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备注/Memo

备注/Memo:

收稿日期:2024-01-16; 修回日期:2024-06-04
基金项目:国家重点研发计划项目(2021YFA0719004)
*通信作者:何大祥(1986-),男,江苏淮安人,副教授,理学博士,E-mail:hedaxiang127@163.com。

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