中国石油勘探 ›› 2022, Vol. 27 ›› Issue (2): 131-141.DOI: 10.3969/j.issn.1672-7703.2022.02.012

• 工程技术 • 上一篇    下一篇

古地貌恢复技术在滨里海盆地东缘中—下石炭统岩性勘探中的应用

王燕琨1,王震1,梁爽1,盛善波2,臧真霞3   

  1. 1中国石油勘探开发研究院;2中油国际阿克纠宾油气股份公司;3北京源烃泰克科技有限公司
  • 出版日期:2022-03-15 发布日期:2022-03-15
  • 作者简介:王燕琨(1970-),女,北京人,硕士,2009年毕业于中国石油勘探开发研究院,高级工程师,主要从事哈萨克斯坦滨里海盆地东缘石油地质勘探方面的研究工作。地址:北京市海淀区学院路20号中国石油勘探开发研究院,邮政编码:100083。
  • 基金资助:
    中国石油天然气股份有限公司科学研究与技术开发项目“海外复杂碳酸盐岩精细勘探关键技术研究”(2021DJ3104),“海外油气勘探项目资产评估与规划决策技术研究”(2021DJ3106)。

Application of paleogeomorphology restoration technology in lithologic reservoir exploration of the Middle-Lower Carboniferous in the eastern margin of Pre-Caspian Basin

Wang Yankun1,Wang Zhen1,Liang Shuang1,Sheng ShanBo2,Zang Zhenxia3   

  1. 1 PetroChina Research Institute of Petroleum Exploration & Development; 2 CNPC International Aktobe Oil & Gas Co., Ltd.; 3 Geoseismic Signal Company
  • Online:2022-03-15 Published:2022-03-15

摘要: 哈萨克斯坦滨里海盆地东缘中—下石炭统碳酸盐岩(KT-Ⅱ层)不断获得油气发现。随着勘探的深入,面临的难题是碳酸盐岩薄储层预测。从KT-Ⅱ层沉积前的古地貌入手,还原当时碳酸盐岩沉积背景,厘清储层的分布规律。KT-Ⅱ层由下至上可划分为SQ1、SQ2、SQ3三个三级层序,根据高频层序地震精细解释,分别采用地震层位拉平法、地层残余厚度法和印模法,恢复了SQ1—SQ3沉积前的古地貌。SQ1滩体主要围绕SQ1沉积前的坡折带进行沉积,局部沉积厚度较大;SQ2滩体主要分布于低势区与高势区之间的斜坡带,呈连片的趋势,越往高势区储层越发育;SQ3滩体主要沉积于两条走滑断层之间的斜坡带。

关键词: 滨里海盆地, 中—下石炭统, 碳酸盐岩, 古地貌恢复技术, 滩体

Abstract: Oil and gas have continuously been discovered in the Middle-Lower Carboniferous carbonate rocks (KT-Ⅱ layer) in the eastern margin of Pre-Caspian Basin. With the progress of exploration, the prediction of thin carbonate reservoir is facing challenges. By starting from the paleogeomorphology before the deposition of KT-Ⅱ layer, the depositional settings during the deposition of carbonate rocks is restored, and the law of reservoir distribution is identified. The KT-Ⅱ layer is subdivided into three third-order sequences from bottom to top, i.e., SQ1, SQ2, and SQ3. Based on the fine seismic interpretation of high-frequency sequence, the paleogeomorphology before the deposition of each sequence was restored by using the methods of seismic horizon flattening, residual formation thickness and moulage. The beach body of SQ1 was mainly deposited around the slope break zone, with a large thickness in local area; The beach body of SQ2 was mainly distributed in slope zone between the low potential area and the high potential area, with continuous distribution and more developed reservoir towards the high potential area; While the beach body of SQ3 was mainly deposited in slope zone between two strike-slip faults.

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