岩性油气藏 ›› 2025, Vol. 37 ›› Issue (3): 84–94.doi: 10.12108/yxyqc.20250308

• 地质勘探 • 上一篇    

渤海海域太古界潜山型储层特征及主控因素

王丽娟1,2, 韩登林1,2, 马良帅3, 胡蓉蓉4, 王晨晨2,5, 马斌玉1,2, 闫康1,2, 朱朝彬1,2   

  1. 1. 长江大学 地球科学学院, 武汉 430100;
    2. 长江大学 储层微观结构演化及数字表征实验室, 武汉 430100;
    3. 中海油能源发展股份有限公司工程技术分公司 中海油实验中心, 天津 300452;
    4. 长江大学 石油工程学院, 武汉 430100;
    5. 长江大学 非常规油气湖北省协同创新中心, 武汉 430100
  • 收稿日期:2024-12-06 修回日期:2025-01-19 发布日期:2025-05-10
  • 第一作者:王丽娟（1999—），女，长江大学在读硕士研究生，研究方向为碎屑岩储层地质学。地址：（430100）湖北省武汉市蔡甸区长江大学路特1号。Email：2629434067@qq.com。
  • 通信作者: 胡蓉蓉（1987—），女，博士，实验师，主要从事储层表征和提高高采收率方面的教学与科研工作。Email：hurongrong87@126.com。
  • 基金资助:
    国家自然科学基金项目“凝灰质填隙物沉积—成岩分异特征及其对砂砾岩储层物性的控制作用——以玛湖凹陷三叠系百口泉组为例”（编号：42072121）资助。

Characteristics and main controlling factors of Archean buried hill reservoir in Bohai Sea

WANG Lijuan1,2, HAN Denglin1,2, MA Liangshuai3, HU Rongrong4, WANG Chenchen2,5, MA Binyu1,2, YAN Kang1,2, ZHU Chaobin1,2   

  1. 1. School of Geosciences, Yangtze University, Wuhan 430100, China;
    2. Laboratory of Reservoir Microstructure Evolution and Digital Characterization, Yangtze University, Wuhan 430100, China;
    3. CNOOC Experimental Center, CNOOC Energy TechDrilling and Production Company, Tianjin 300452;
    4. School of Petroleum Engineering, Yangtze University, Wuhan 430100, China;
    5. Cooperative Innovation Center of Unconventional Oil and Gas, Yangtze University, Wuhan 430100, China
  • Received:2024-12-06 Revised:2025-01-19 Published:2025-05-10

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摘要： 依据岩心薄片分析、X射线衍射分析以及测井等资料，对渤海海域M油田中位潜山与渤中19-6低位潜山的储层特征及主控因素进行了研究。研究结果表明：①纵向上，渤海海域M油田中位潜山风化带储层较发育，以孔隙-裂缝型为主；渤中19-6低位潜山储层裂缝尤其发育，风化带和内幕带均以裂缝型储层为主。不同类型潜山在埋藏深度、源储接触及垂向分带等多方面均存在明显差异，进而导致了储层在孔喉空间等微观结构方面也存在差异。②多期构造运动造成不同类型潜山储层分带具有差异性，古地貌构造制约了潜山储层的平面分布及有机酸迁移方向，风化淋滤溶蚀作用间接改善了储层的微观结构，其改善程度受潜山裂缝及风化环境控制。③不同类型潜山的优质储层发育带具有差异性，低位潜山型优质储层主要集中在深层内幕裂缝带，中位潜山型优质储层主要分布在潜山顶部风化带内。

关键词: 潜山储层, 中位潜山, 低位潜山, 微观结构, 裂缝型, 孔隙-裂缝型, 构造运动, 古地貌, 太古界, 渤海海域

Abstract: Based on core thin section analysis，X-ray diffraction analysis and logging data，the reservoir structure characteristics and main control factors of the M oilfield median buried hill and the BZ19-6 low buried hill in Bohai Sea area were studied. The results show that：（1）Longitudinally，the weathering zone reservoir in M oilfield median buried hill reservoir is well developed，and the pore-fracture type is dominant. The fractures in BZ19-6 low buried hill reservoir are particularly developed，and the weathering zone and the inner zone are dominated by fractured reservoirs. There are obvious differences in burial depth，source-reservoir contact and vertical zonation among different types of buried hill，lead to the differences in the microstructure of reservoirs in terms of pore throat space.（2）Multi-stage tectonic movement causes the differences in the zonation of different types buried hill reservoirs，paleogeomorphological structure restricts the plane distribution of buried hill reservoirs and the migration direction of organic acids，and weathering leaching indirectly improves the reservoir structure of different types of buried hills，and its improvement degree is controlled by buried hill fractures and weathering environment.（3）Different types of buried hill high quality reservoir development zone，have different characteristics. The BZ19-6 low buried hills high quality reservoirs are mainly concentrated in the deep inner fracture zone，and the M oilfield median buried hills are mainly distributed in the weathering zone at the top of the buried hills.

Key words: buried hill reservoir, median buried hill, low buried hill, micro structure, fracture type, pore-fracture type, tectonic movement, paleogeomorphology, Archaean, Bohai Sea

中图分类号: 

  • TE122.2
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