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珠江口盆地油气勘探新进展与潜力区带预测

倪春华 杨俊 王彦青 宋在超 蒋天赐 黄炳祺 阎泽昊 邢泽正 朱珍君 李琦 陈贺贺

倪春华, 杨俊, 王彦青, 宋在超, 蒋天赐, 黄炳祺, 阎泽昊, 邢泽正, 朱珍君, 李琦, 陈贺贺. 珠江口盆地油气勘探新进展与潜力区带预测[J]. 石油实验地质, 2025, 47(3): 451-465. doi: 10.11781/sysydz2025030451
引用本文: 倪春华, 杨俊, 王彦青, 宋在超, 蒋天赐, 黄炳祺, 阎泽昊, 邢泽正, 朱珍君, 李琦, 陈贺贺. 珠江口盆地油气勘探新进展与潜力区带预测[J]. 石油实验地质, 2025, 47(3): 451-465. doi: 10.11781/sysydz2025030451
NI Chunhua, YANG Jun, WANG Yanqing, SONG Zaichao, JIANG Tianci, HUANG Bingqi, YAN Zehao, XING Zezheng, ZHU Zhenjun, LI Qi, CHEN Hehe. Recent advancements in oil and gas exploration and potential zone prediction in Pearl River Mouth Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2025, 47(3): 451-465. doi: 10.11781/sysydz2025030451
Citation: NI Chunhua, YANG Jun, WANG Yanqing, SONG Zaichao, JIANG Tianci, HUANG Bingqi, YAN Zehao, XING Zezheng, ZHU Zhenjun, LI Qi, CHEN Hehe. Recent advancements in oil and gas exploration and potential zone prediction in Pearl River Mouth Basin[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2025, 47(3): 451-465. doi: 10.11781/sysydz2025030451

珠江口盆地油气勘探新进展与潜力区带预测

doi: 10.11781/sysydz2025030451
基金项目: 

中国石化科技部项目 P24180

国家自然科学基金项目 41576066

国家自然科学基金项目 42306083

详细信息
    作者简介:

    倪春华(1981—),男,博士,高级工程师,从事油气地质与地球化学研究。E-mail: nichunhua.syky@sinopec.com

    通讯作者:

    李琦(1969—),男,博士,教授,从事海洋地质与沉积盆地分析研究。E-mail: liqi@cugb.edu.cn

  • 中图分类号: TE132.1

Recent advancements in oil and gas exploration and potential zone prediction in Pearl River Mouth Basin

  • 摘要: 珠江口盆地新生界油气资源丰富,探明储量增长迅速。低角度拆离型断层控烃、古潜山走滑断裂与风化淋滤控储、深水多类型储集体富集等地质认识创新为盆地勘探迎来新机遇。然而,该盆地地质结构复杂、目标类型多样,增加了勘探的难度。因此,在勘探理论突破的指导下,重新评估盆地新生界油气地质条件、明确油气勘探潜力区带至关重要。通过综合分析珠江口盆地的构造—沉积耦合作用、烃源岩条件和储层条件评价、油气运移特征,开展了盆地不同区带的油气地质成功概率评估,并计算了新生界总地质资源量。珠江口盆地在新生代经历了裂陷期、裂后拗陷期及构造活化期的构造演化,形成了陆相沉积、海陆过渡相沉积及浅海相沉积充填特征,控制了古近系两套主要烃源岩及陆、海相两套储层。浅水区的陆丰、惠州、文昌凹陷油气地质条件优越,含油气概率超过20%,地质风险较低,划分为Ⅰ类有利区带。新生界总地质资源量约为138亿吨,其中石油占71%,天然气占29%。基于区带评价和勘探实例,未来应重点加强深层古潜山、古近系及深水油气藏的勘探,特别是在恩平、开平、白云凹陷寻找低角度拆离型油气藏,文昌、阳江凹陷寻找深层走滑断裂潜山裂缝型油气藏,白云、荔湾凹陷寻找深水油气藏。这些凹陷有望成为珠江口盆地未来油气勘探的重要潜力区带。

     

  • 图  1  珠江口盆地区域划分(a)及地质充填特征(b)

    Figure  1.  Regional division (a) and geological filling features (b) of PRMB

    图  2  珠江口盆地各凹陷新生代构造演化过程

    据参考文献[9, 11, 13-14]修改。

    Figure  2.  Cenozoic tectonic evolution process of each sag in PRMB

    图  3  珠江口盆地沉积相平面图

    据参考文献[20-21]修编。

    Figure  3.  Sedimentary facies maps of PRMB

    图  4  珠江口盆地烃源岩评价

    据参考文献[21-26]修编。

    Figure  4.  Evaluation of hydrocarbon source rocks in PRMB

    图  5  珠江口盆地储层评价

    据参考文献[27-31]修编。

    Figure  5.  Reservoir evaluation of PRMB

    图  6  珠江口盆地裂后期断裂体系分布

    据李刚[16],有修改。

    Figure  6.  Distribution of post-rift fault system in PRMB

    图  7  珠江口盆地油气成藏关键时刻

    据施和生等[33],有修改。
    图中断裂系统一栏中,Ⅰ, Ⅱ, Ⅲ和1, 2, 3, 4分别表示凹陷和隆起区断层活动的持续时间级别,其中1代表短期活动断层,而4代表长期活动断层,反映了断层作为油气输导体系的潜在有效性。

    Figure  7.  Key stages of oil and gas accumulation in PRMB

    图  8  珠江口盆地新生界资源潜力估算

    Figure  8.  Estimation of Cenozoic resource potential in PRMB

    图  9  珠江口盆地新生界有利区带优选及评价

    Figure  9.  Selection and evaluation of favorable zones in Cenozoic of PRMB

    图  10  珠江口盆地新勘探进展成藏模式

    剖面位置见图 1a

    Figure  10.  Accumulation models based on new exploration advancements in PRMB

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  • 收稿日期:  2024-10-14
  • 修回日期:  2025-04-15
  • 刊出日期:  2025-05-28

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