石油学报 ›› 2026, Vol. 47 ›› Issue (7): 1315-1331.DOI: 10.7623/syxb202607001

• 地质勘探 •    

珠江口盆地白云凹陷超深水碳酸盐岩天然气勘探突破及其意义

刘军1,2, 彭光荣1,2, 张忠涛1,2, 刘道理1,2, 徐乐意1,2, 张丽丽1,2, 徐长贵3   

  1. 1. 中海石油(中国)有限公司深圳分公司 广东深圳 518054;
    2. 中海石油深海开发有限公司 广东深圳 518054;
    3. 中国海洋石油有限公司 北京 100010
  • 收稿日期:2026-02-16 修回日期:2026-05-25 发布日期:2026-08-04
  • 通讯作者: 徐长贵,男,1971年10月生,2007年获中国地质大学(北京)博士学位,现为中国海洋石油集团有限公司首席科学家、教授级高级工程师,主要从事石油天然气地质综合研究及油气勘探管理工作。Email:xuchg@cnooc.com.cn
  • 作者简介:刘军,男,1973年1月生,1995年获中国石油大学(华东)学士学位,现为中海石油(中国)有限公司深圳分公司副总经理、总地质师、教授级高级工程师,主要从事油气勘探综合研究。Email:liujun1@cnooc.com.cn
  • 基金资助:
    新型油气勘探开发国家科技重大专项“南海油气成藏机制与勘探开发关键技术”(2025ZD1402702)资助。

Breakthrough of natural gas exploration of ultra-deepwater carbonate rocks in Baiyun sag of Pearl River Mouth Basin and its significance

Liu Jun1,2, Peng Guangrong1,2, Zhang Zhongtao1,2, Liu Daoli1,2, Xu Leyi1,2, Zhang Lili1,2, Xu Changgui3   

  1. 1. Shenzhen Branch, CNOOC China Limited, Guangdong Shenzhen 518054, China;
    2. CNOOC Deepwater Development Limited, Guangdong Shenzhen 518054, China;
    3. CNOOC Limited, Beijing 100010, China
  • Received:2026-02-16 Revised:2026-05-25 Published:2026-08-04

摘要: 珠江口盆地白云凹陷在超深水区云荔低隆起中新统珠江组五段钻获抱球虫混积岩储层,于2024年在荔湾4-1构造的L4井测试获得产量为43×104m3/d的高产天然气流,实现了新勘探领域的重大突破。该类储层兼具碳酸盐与粉砂-泥质碎屑混积的特征,主要发育于云荔低隆起周缘的古地貌高部位,形成于半深海环境,抱球虫体腔格架为高孔隙度储层的形成提供基础。综合古地貌、古海洋背景以及岩心、岩石薄片、粒度、全岩主量元素和有孔虫-生物遗迹等资料,探讨了"浊流-底流"与"底流-古高地"双交互作用控制下抱球虫混积岩储集体的沉积动力、空间展布和成储机制。研究结果表明:①远离物源的末端浊流与底流的交互作用为云荔低隆起提供了粉砂—砂级碎屑颗粒沉积;②底层洋流与古地貌高部位的交互作用决定了抱球虫混积岩的发育规模和空间分布差异;③储层物性受沉积动力分选与埋藏成岩作用共同控制,较强的沉积动力可移除细粒物质、改善储层孔隙,而较高的陆源黏土矿物含量可能抑制胶结物沉淀,有利于原生体腔孔保存;④强胶结作用显著降低储层孔隙度。针对此类"高孔低渗"储层,形成了"沉积成储理论创新、地球物理精准预测、工程工艺一体化改造"技术体系,通过研发新型多基配位螯合酸液体系和长水平井酸化改造,可提高基质渗透率与泄流面积,实现油气藏产能的规模释放。"浊流-底流"与"底流-古高地"双交互作用控制下的抱球虫混积岩沉积模式,突破了深水储层发育严重依赖陆源碎屑的传统认识,指明了珠江口盆地超深水区天然气勘探新领域,为中国深水/超深水油气勘探实践提供了创新思路。

关键词: 抱球虫, 浊流, 底流, 深水, 超深水, 碳酸盐岩, 珠江口盆地

Abstract: A major exploration breakthrough has been achieved in the ultra-deepwater Liwan area of Baiyun sag of Pearl River Mouth Basin, where a unique globigerina mixed reservoir was drilled in the Member 5 of Lower Miocene Zhujiang Formation. In 2024, production testing of Well L4 in the Liwan4-1 structure yielded a high-capacity natural gas flow of 43×104m3/d, marking a significant milestone in this novel exploration domain. This reservoir exhibits mixed carbonate and silt-argillaceous clast characteristics. It is predominantly developed across palaeogeomorphic highs surrounding the Yunli low-uplift with a semi-deep-sea environment, where the intraparticle chambers of globigerina provided the basis for the formation of the high-porosity reservoir. By integrating palaeogeomorphic and paleo-oceanographic frameworks with datasets from cores, thin sections, grain sizes, whole rock major elements, and foraminifer-ichnofossil assemblages, this study elucidates the sedimentary dynamics, spatial distribution, and reservoir-forming mechanisms of the globigerina mixed reservoir under the control of dual interactions between turbidity currents and bottom currents, and between bottom currents and paleo-highs. The research results indicate as follows. (1) The interaction between distal turbidity currents far from the provenance and bottom currents delivered silt- to sand-grade clastic sediments to the Yunli low-uplift. (2) The interaction between bottom currents and paleo-highs dictated the developmental scale and spatial heterogeneity of the globigerina mixed rocks. (3) Reservoir petrophysical properties are co-controlled by hydrodynamic sorting and burial diagenesis. Strong hydrodynamic energy effectively winnowed fine-grained matrix and enhanced reservoir porosity, while high terrigenous clay content potentially inhibited cement precipitation, favoring the preservation of primary intraparticle pores. (4) Intensive cementation significantly reduced porosity. Focusing on high-porosity and low-permeability reservoirs, a technical framework integrating depositional-reservoir theoretical innovation, precise geophysical prediction, and engineering-technology-integrated stimulation was established. By developing a novel multi-dentate coordination chelating acid system and implementing stimulation via long horizontal well acidification, matrix permeability and drainage area were enhanced, enabling the large-scale release of oil and gas reservoir production capacity. The sedimentary model of globigerina mixed rocks, which is controlled by dual interactions between turbidity currents and bottom currents, and between bottom currents and paleo-highs, challenges the traditional consensus that deep-water reservoir development relies heavily on terrigenous clasts, points to a new frontier for natural gas exploration in the ultra-deepwater areas of the Pearl River Mouth Basin, and offers practical insights for deep-water and ultra-deep-water oil and gas exploration in China.

Key words: globigerina, turbidity current, bottom current, deepwater, ultra-deepwater, carbonate rocks, Pearl River Mouth Basin

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