莱州湾凹陷明下段砂体结构类型、成因机制及其控藏效应
Structural types, genetic mechanisms and reservoir controll effect of sand bodies in the Lower Member of Minghuazhen Formation in subsag zone of Laizhouwan sag
投稿时间:2026-04-30  修订日期:2026-05-18
DOI:
中文关键词:  砂体结构  切叠型  古气候  物源供给  油气运移  莱州湾凹陷
英文关键词:sand body structure  cutting overlay type  paleoclimate  provenance supply  hydrocarbon migration  Laizhouwan sag
基金项目:中海石油(中国)有限公司“七年行动计划”科技重大专项“渤海油田上产4000万吨新领域勘探关键技术”(CNOOC-KJ135 ZDXM36TJ08TJ)资助
作者单位邮编
王傲林 中海石油(中国)有限公司天津分公司 300457
徐春强* 中海石油(中国)有限公司天津分公司 
高雁飞 中海石油(中国)有限公司天津分公司 
周晓光 中海石油(中国)有限公司天津分公司 
宿雯 中海石油(中国)有限公司天津分公司 
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中文摘要:
      渤海海域莱州湾凹陷明下段发育多套含油气砂体,分布范围广,然而砂体结构特征及其成因机制不清晰,其与含油性的内在关联尚不明确,制约了下一步油气勘探部署。本文利用地震、测井、岩心、薄片等资料,对研究区砂体内部结构特征进行了解剖,进而探讨了不同结构类型砂体的成因机制及其控藏作用。主要研究成果如下:(1)明确了研究区砂体主要存在孤立型、搭接型及切叠型三种内部结构模式,其中切叠型砂体主要发育在沉积早期(明下段V油组),搭接型砂体主要发育在沉积中期(明下段IV、V油组过渡部位),孤立型砂体主要发育在沉积晚期(明下段IV油组);(2)通过系统分析古气候变化与物源供给量等地质要素并类比现代沉积,揭示了砂体内部结构差异的成因机制。具体而言,研究区早期因气候湿润、物源供给充足,促进了切叠连片型砂体的形成;而晚期则因气候趋于干旱、物源供应减少,导致孤立河道型砂体的广泛发育;(3)结合河流相沉积动力学机制和沉积规律,有效识别沉积晚期孤立河道型砂体有利叠置部位,进而创新提出叠置砂体垂向切叠型油气运移模式。研究成果一方面丰富和完善了渤海新近系油气运移理论体系,打破了孤立河道型砂体较难成藏的常规认识,另一方面,对成熟油田开展河流相砂体油气精细勘探具有指导意义。
英文摘要:
      Multiple sets of hydrocarbon sand bodies are developed in the Lower Member of Minghuazhen Formation in Laizhouwan sag, which are widely distributed.However, the structural characteristics and genetic mechanism of sand bodies remain unclear, and the relationship between sand bodies and oil bearing is also ambiguous, which restricts the next exploration. Based on seismic, well logging, core and thin section data, the internal structural characteristics of sand bodies in research area are dissected, and the controlling factors of the sand bodies formation and their relationship with oil bearing are discussed.The results show that: (1)There are three types of internal structures of sand bodies in the study area, namely isolated type, lap type and cutting overlay type, the cutting overlay sand bodies are mainly developed in the early sedimentary stage (the V oil group in the Lower Member of Minghuazhen Formation), the lap type sand bodies mainly developed in the middle sedimentary stage (the transitional part between the IV and V oil group in the Lower Member of Minghuazhen Formation), and the isolated sand bodies are mainly developed in the late sedimentary stage(the IV oil group in the Lower Member of Minghuazhen Formation); (2)Through the systematic analysis of geological factors such as paleoclimate and provenance supply in the study area, the controlling factors of sand bodies with different structures are determined. In the early stage of the study area, the humid climate and sufficient provenance supply promoted the formation of cutting overlay sand bodies. In the late stage of the study area, the arid climate and insufficient provenance supply led to the extensive development of isolated sand bodies; (3)Combined with fluvial sedimentary dynamics and sedimentary rules, the favorable superimposed areas of isolated sand bodies in the late sedimentary stage are effectively identified, and the innovative vertical cutting-overlay hydrocarbon migration model of superimposed sand bodies is proposed. On the one hand, this research achievement enriches and improves the Neogene hydrocarbon migration theory system in the Bohai Sea and ensures the overall reserve scale of the zone. On the other hand, it has guiding significance for the development of reservoir potential in mature oil fields.
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