刘平, 童传新, 曾小明, 李伟, 宋鹏. 莺歌海盆地莺东斜坡乐东区中深层地层水特征及其与油气关系[J]. 海洋地质前沿, 2019, 35(8): 44-50. DOI: 10.16028/j.1009-2722.2019.08006
    引用本文: 刘平, 童传新, 曾小明, 李伟, 宋鹏. 莺歌海盆地莺东斜坡乐东区中深层地层水特征及其与油气关系[J]. 海洋地质前沿, 2019, 35(8): 44-50. DOI: 10.16028/j.1009-2722.2019.08006
    LIU Ping, TONG Chuanxin, ZENG Xiaoming, LI Wei, SONG Peng. CHARACTERISTICS OF STRATIGRAPHIC WATER IN THE MIDDLE AND DEEP LAYERS OF LEDONG DISTRICT, YINGDONG SLOPE, YINGGEHAI BASIN AND ITS RELATIONSHIP WITH OIL AND GAS[J]. Marine Geology Frontiers, 2019, 35(8): 44-50. DOI: 10.16028/j.1009-2722.2019.08006
    Citation: LIU Ping, TONG Chuanxin, ZENG Xiaoming, LI Wei, SONG Peng. CHARACTERISTICS OF STRATIGRAPHIC WATER IN THE MIDDLE AND DEEP LAYERS OF LEDONG DISTRICT, YINGDONG SLOPE, YINGGEHAI BASIN AND ITS RELATIONSHIP WITH OIL AND GAS[J]. Marine Geology Frontiers, 2019, 35(8): 44-50. DOI: 10.16028/j.1009-2722.2019.08006

    莺歌海盆地莺东斜坡乐东区中深层地层水特征及其与油气关系

    CHARACTERISTICS OF STRATIGRAPHIC WATER IN THE MIDDLE AND DEEP LAYERS OF LEDONG DISTRICT, YINGDONG SLOPE, YINGGEHAI BASIN AND ITS RELATIONSHIP WITH OIL AND GAS

    • 摘要: 油气田伴生地层水地球化学特征蕴含多种油气地质及水文地质信息,可以为油气成藏的圈闭条件评价及展布特征分析等提供重要的信息和佐证。由于油气田地层水与油气藏伴生且受成烃成藏环境及后期保存条件等多种地质因素的影响,故其地质地球化学特征与油气运聚成藏过程及后期圈闭保存条件等密切相关。莺歌海盆地乐东区中深层高温超压大气田伴生地层水总矿化度异常高(60 000~80 000 mg/L),pH值为6~8,属于弱酸—弱碱性的盐水和卤水,其地层水类型属CaCl2水型,为一种非常特殊的高矿化度气田伴生地层水。通过莺歌海盆地乐东区中深层气田伴生地层水pH值、常规离子组成、主要元素及其组合特点等统计分析,获取了这种高温超压大气田伴生地层水的大量地质地球化学信息,并深入分析探讨了其与天然气运聚成藏及其分布的成因联系。

       

      Abstract: Associated stratigraphic water in an oil and gas field contains a variety of information on oil and gas geology and may provide important evidence for evaluation of trap conditions and the distribution patterns of hydrocarbon accumulations. It is closely associated with oil and gas reservoirs and affected by many geological factors, such as hydrocarbon formation and storage conditions, post-storage conditions, geological and geochemical characteristics related to hydrocarbon migration and accumulation processes and the later trapping and preservation conditions. The total mineralization or salinity of the associated stratigraphic water in the middle-deep layers of the gas fields under high temperature and overpressure in the Ledong District of the Yinggehai Basin is abnormally high (60 000 mg/L-80 000 mg/L). It is a kind of weak acid-weak alkaline brine rich in CaCl2 with a pH of 6-8. Based upon the geological and geochemical characteristics of the associated stratigraphic water, we discussed in this paper the genetic relationship between the stratigraphic water and the migration and accumulation of gas.

       

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