Regional evaluation of oil and gas resources in offshore China and exploration of marine Paleo-Mesozoic oil and gas in the Yellow Sea and East China Sea
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摘要:
2019年是青岛海洋地质研究所重建40周年。40年来，研究所根据公益性油气资源调查的基本定位，按照“立足黄东海、面向中国海、辐射全球海”的空间业务布局，紧密围绕国家和社会重大需求、瞄准国际海洋科技前沿，以摸清中国海域油气资源家底、掌握资源分布状况、实现新区新层系油气突破、服务国家能源战略和海洋强国战略为己任，持续开展了中国海域油气资源区域评价与黄东海盆地油气资源调查，大体分为海域及邻区沉积盆地对比研究、中国海域区域评价战略研究和黄东海海域新区新层系油气资源调查3个阶段。先后主持编制了中国海域沉积盆地分布图和油气资源勘探开发（动态）形势图，开展了海域及邻区含油气盆地对比、中国海域油气勘探开发形势动态分析和油气资源区域评价战略研究、黄东海海域油气资源调查研究与评价，取得了一批原创性的成果。主要体现在：①海域油气资源早期评价技术和沉积盆地深部地震探测技术取得突破性进展；②中国海域油气资源丰富，下一步的调查与勘探方向包括：新层系、近海天然气、富生烃凹陷潜山油气藏、南海深水油气、南海生物礁和非常规天然气；③明确了南黄海盆地的基底性质、海相盆地地层层序和构造区划、侏罗纪前陆盆地特征、海相盆地的油气地质条件和有利区带；④明确了东海中生代盆地的地层层序、盆地结构和两期盆地性质、“大东海”中生代地层分布特征、中生界油气地质条件和有利区带；⑤发现了南黄海古生界古油藏。上述成果和认识为海洋油气资源调查与勘探的下一步工作奠定了坚实的基础。
Abstract:40 years have passed since the reestablishment of the Qingdao Institute of Marine Geology in 1979. In the past 40 years, following the basic objective to carry out public oil and gas surveys in China seas and global waters with the Yellow Sea and East China Sea as major targets so as to meet the increasing demand of energy resources of the nation and society, the institute has devoted a lot to the studies on hydrocarbon resource generation and distribution patterns in China seas, upon the international frontiers of marine science and technology. A great number of breakthroughs have been achieved, such as the discovery of new oil and gas horizons and districts. Under the guidance of national energy strategy and the task to make China a strong marine power, the Institute has persisted in regional evaluation of oil and gas resources in China seas, in particular in the Yellow Sea and East China Sea. The research can be roughly subdivided into three stages: the first stage focusing on comparison of offshore and neibouring basins; the second stage focusing on the study of regional evaluation strategies of China seas and the third stage focusing on new horizons and new districts in the Yellow Sea and East China Sea. A map series on distribution of sedimentary basins in China seas and a set of dynamic situation map of oil and gas exploration and development in China Sea were compared and published successively. During the period, following achievements are necessary to be mentioned: (1) Breakthroughs in early stage oil and gas evaluation technology and the deep seismic detection technology for offshore sedimentary basins; (2) Resource assessment in China seas. Data proves that China is rich in marine oil and gas. And the next cycle of survey and exploration should be placed in the new horizons, such as gas offshore, buried hills oil and gas resources in the hydrocarbon-rich sags, oil and gas in deepwaters, organic reefs in the South China Sea and unconventional gas; (3) Further understandings of basic geology, such as, basement properties, marine stratigraphic sequences, tectonic division, characteristics of Jurassic foreland basins, marine basin hydrocarbon geologic conditions and favorable zones in the South Yellow Sea basins; (4) Solution of some specific geological problems related to oil and gas accumulation. Such as, Mesozoic stratigraphic sequences, two-stage basin architecture, basin properties, Mesozoic stratigraphic distribution patterns and the discovery of “Great East China Sea”, Mesozoic hydrocarbon geologic conditions and favorable zones in the East China Sea; (5) Discovery of Paleozoic reservoirs. These achievements and discoveries have laid a solid foundation for the future oil and gas geological survey and exploration in China seas.
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图 3 南黄海海相中―古生界地震层序及地质属性标定（据参考文献[32]修改）（S1至S7为南黄海海相中―古生界地震层序，T2相当于新近系底界，B1至B3为3套典型地震反射标志层组）
Figure 3.
表 2 中国海域沉积盆地
Table 2. A summary of sedimentary basins in China seas
海域 盆地名称 渤海和黄东海 渤海盆地、北黄海盆地、南黄海盆地 东海陆架盆地、冲绳海槽盆地、台西盆地 南海 台西南盆地、珠江口盆地、北部湾盆地、笔架盆地、笔架南盆地、尖峰北盆地、双峰盆地、西沙海槽盆地、琼东南盆地、莺歌海盆地、中建南盆地、排波盆地、西北巴拉望盆地、礼乐盆地、万安盆地、南薇西盆地、南薇东盆地、永署盆地、九章盆地、安渡北盆地、曾母盆地、北康盆地、南沙海槽盆地和文莱沙巴盆地 
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盆地类型 盆地划分 陆内裂谷盆地 渤海湾盆地、北黄海盆地、南黄海盆地、北部湾盆地 陆缘裂谷盆地 东海陆架盆地、台西盆地、台西南盆地、珠江口盆地、琼东南盆地 走滑拉张盆地 莺歌海盆地、中建南盆地、万安盆地 弧后盆地 冲绳海槽盆地 前弧盆地 文莱沙巴盆地 前陆盆地 曾母盆地 裂离陆块盆地 北康盆地、南薇盆地、礼乐盆地、南薇西盆地、南薇东盆地、
永署盆地、九章盆地、安渡北盆地、西北巴拉望盆地、深海堆积盆地 笔架盆地、笔架南盆地、尖峰北盆地、双峰盆地、西沙海槽盆地、排波盆地
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表 4 南黄海盆地海相中―古生界构造单元划分表（据参考文献[32, 40]）
Table 4. Tectonic units of the marine Meso-Paleozoic in the South Yellow Sea Basin（from references [32, 40]）
基本构造单元 二级构造带 三级构造带 总体特征 南黄海盆地 青岛断褶带 南倾断裂较发育，常与北倾断裂形成地堑或地垒构造，
中―古生代海相地层齐全、厚度大、变形较弱，以隔档式构造为主。崂山断隆带 高石稳定带 深大断裂不发育，浅层断裂较少，正逆共存。中―古生代海相地层层序完整，
变形较弱，构造以宽缓褶皱或断鼻、断块为主。青峰变形带 盖层滑脱型逆掩推覆体系，断裂发育，地层褶皱变形较强烈，古生界发育完整，分布广泛。 烟台冲断带 高角度基底卷入式逆冲，断裂北倾为主，发育逆冲断块，上古生界剥蚀严重，下古生界分布相对稳定。
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