New progress of petroleum resources survey in South Yellow Sea basin
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摘要:
南黄海盆地是中-古生代海相沉积盆地与中-新生代陆相沉积盆地相叠加的大型沉积盆地，其油气调查与勘探始于20世纪60年代初，经历了陆相盆地调查与勘探、探索与研究、海相盆地勘查3个阶段。由于地震地质条件复杂、盆地演化历史复杂、地质构造复杂、勘探程度相对较低，50多年的调查与勘探未获得商业性油气发现。经过2005年以来的长期地震调查技术攻关，初步形成了以“高覆盖次数、富低频信号、强震源能量”的采集技术和“高分辨率、富低频成分、强反射能量”的处理技术相结合的盆地深部“高富强”地震探测技术，并获得深部海相层的有效地震反射。近年来的进一步调查和研究发现：(1)南黄海盆地不仅是扬子板块在海域的延伸，而且是下扬子地块的主体；(2)南黄海盆地与四川盆地在中-古生代海相盆地沉积时期具有相同的沉积建造和沉积演化历史；(3)南黄海陆相中-新生界以下残留有巨厚的中-古生代海相地层，存在可追踪对比的三套地震反射标志层组，据此建立了中-古生代海相沉积层的地震层序；(4)发育下寒武统荷塘组(或幕府山组)、上奥陶统五峰组-下志留统高家边组、上二叠统龙潭组-大隆组三套优质烃源岩，三套完整的生储盖组合，具备形成大型油气田的物质基础；(5)理论模拟和包体分析表明，海相中-古生界存在多源多期成藏特征；(6)崂山隆起是海相下古生界油气远景区，勿南沙隆起是海相上古生界的油气远景区；(7)崂山隆起高石稳定带是有利勘探区带，是寻找类似于四川盆地“威远型”和“安岳型”油气田的重要地区；(8)高石3号构造是古生界的首选钻探目标。下一步工作重点是实施以下古生界为主要目的层的参数井钻探，建立区内完整的中-古生代地层层序，获取资源评价参数，实现南黄海油气调查的战略发现和勘探认识突破。
Abstract:The South Yellow Sea basin is a large-scale sedimentary basin composed of a Paleo-Mesozoic marine sedimentary basin superimposed by a Meso-Cenozoic continental sedimentary basin. Petroleum geological survey and exploration started there in the early 60s of the last century, and up to date has passed through three stages, i.e. the stage of investigation and exploration of terrestrial basin, the stage of summarization and scientific research, and the stage of investigation and exploration of the marine basin. For more than 50 years, commercial petroleum discoveries have not yet been gained because of ceomplex geological conditions, complicated history of basin evolution and geological structures, and relatively low exploration levels. After a long-term research on seismic exploration technnology since 2005, we have preliminary developed a method called "high, rich, strong" in abbreviation for seismic exploration technology for the deep basin, which is a combination of acquisition technology with "high coverage, rich low-frequency signals, and strong source energy" and processing technology of "high-resolution, low-frequency, high-reflection-energy". With the method, we have obtained effective seismic reflections from deep marine layers. Further investigation and studies in recent years have led to following conclusions. 1. The South Yellow Sea Basin is not only an extension of the Yangtze Plate into the sea, but also the main body of the Lower Yangtze Block; 2. The South Yellow Sea Basin and the Sichuan Basin aresimilarin sedimentary sequences and evolutionary history during the period while the marine Meso-Paleozoic was deposited; 3. In the thick marine Meso-Paleozoic deposits below the continental facies of Meso-Cenozoic strata, there are three sets of seismic reflection markers traceable in the region, upon which the seismic sequence stratigraphy of the Meso-Paleozoic marine sediments is established; 4. There are three sets of high-quality source rocks and three sets of source-reservoir-cap assemplages in the basin, including the Hetang Formation (or Mufushan Formation) of Lower Cambrian, the Wufeng Formation of Upper Ordovician plus Gaojiabian Formation of Lower Silurian, and the Longtan and Dalong Formations of Upper Permian, which founded the material basis for formation of large-scale oil and gas fields; 5. Theoretical simulations and inclusion analysis indicate that there aremulti-source and multi-stagepetrolem accumulation in the marine Meso-Paleozoic basin; 6. The Laoshan uplift is a Early Paleozoic marine facies petroleum prospect and the Wunansha uplift is a marine facies of petroleum prospect of Late Paleozoic; 7. The Gaoshi stability zone of the Laoshan uplift is a favorable exploration target, and there are possiblities to find the "Weiyuan type" and "Anyue type" oil and gas fields discovered in the Sichuan Basin; 8. Gaoshi 3 structure is the preferred drilling target in the Paleozoic. Efforts should be devoted tothe implementation of the planned parameter well with the lower Paleozoic as the main target layers, the establishment of a complete Meso-Paleozoic stratigraphic sequence in the region, and the collection of resource assessment parameters. A breakthrough in strategic discovery and exploration of the petroleum survey is expectable at the South Yellow Sea.
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Key words:
- petroleum resources survey /
- new progress /
- new understanding /
- Laoshan uplift /
- South Yellow Sea basin
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表 1 南黄海盆地钻井情况
Table 1. Drilling holes in the South Yellow Sea basin
序号 井号 类型 井深/m 作业者 完井时间 井底地层及测试情况 1 H1 预探井 1544 MGMR 1974 三垛组，见荧光 2 H2 预探井 1769 MGMR 1975 震旦系?见气显示 3 H3 预探井 535 MGMR 1975 事故报废 4 H4 预探井 2276 MGMR 1976 阜宁组，未见显示 5 H5 预探井 2310 MGMR 1977 阜宁组二段，未见显示 6 H6 预探井 2413 MGMR 1978 戴南组，未见显示 7 H7 预探井 2393 MGMR 1979 泰州组，未见显示 8 H9 预探井 2320 MGMR 1979 阜宁组二段，未见显示 9 WX20-ST1 参数井 3500 BP 1980 阜宁组四段，未见显示 10 WX5-ST1 参数井 3259 BP 1981 龙潭组，未见显示 11 CZ6-1-1A 预探井 3907 BP 1984 阜宁组三段，折算日产原油2.45t 12 WX13-3-1 预探井 2228 C/T 1984 栖霞组，未见油气显示 13 CZ12-1-1A 预探井 3511 C/T 1985 黄龙组，气测异常 14 CZ6-2-1 预探井 2600 BP 1985 三垛-戴南组，未见显示 15 CZ24-1-1 预探井 3546 C/T 1985 青龙组，气测异常 16 ZC1-2-1 预探井 3433 CLUF 1986 泰州组，岩心裂隙原油渗出 17 ZC7-2-1 预探井 1625 CLUF 1988 泰州组，未见显示 18 FN23-1-1 预探井 2784 CNOOC 1993 阜宁组，未见显示 19 WX4-2-1 预探井 2733 CNOOC 2000 青龙组，未见显示 20 CZ35-2-1 预探井 2726 CNOOC 2001 栖霞组，未见显示 21 RC20-2-1 预探井 3273 CNOOC 2008 侏罗系，未见显示 22 ZC7-1-1 预探井 2341 DEVON 2008 阜宁组，未见显示 23 CSDP-2 科探井 2843 QIMG 2016 高家边组，古生界多层油气显示 24 WX19-3-1 预探井 3750 CNOOC 2018 阜宁组，未见显示 25 ⅡH-1 预探井 826 Gulf 1972 事故终孔, 未见显示 26 ⅡH-1Xa 预探井 3467 Gulf 1973 白垩系，未见显示 27 ⅡC-1X 预探井 2017 Gulf 1973 震旦系?未见显示 28 Inga-1 预探井 4103 MPC/PEDCO 1989 白垩系，气显示 29 Kachi-1 预探井 2726 MPC 1991 青龙组，气显示 30 Haema-1 预探井 2541 PEDCO 1991 白垩系，未见显示 注释：MGMR—地质矿产部；CNOOC—中国海洋石油集团有限公司；BP—英国石油开发有限公司；C/T—美国雪佛龙(CHEVRON)/德士古(TEXACO)石油公司；CLUF—英国克拉夫石油有限公司；DEVON—美国戴维能源公司；QIMG—青岛海洋地质研究所；GULF—美国海湾石油公司；MPC—美国马拉松石油公司；PEDCO—韩国国家石油公司. 
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表 2 2005年以来南黄海地震调查技术攻关施工参数
Table 2. Construction Parameters of seismic surveys technology at the South Yellow Sea since 2005
施工时间 2006年 2007年 2008年 2009年 2010年 2012年 2015年 2016年 调查船 奋斗七号 发现号 发现2号 发现6号 接收道数 336 456 480 480 576 648 576 576 电缆长度/m 4200 5700 6000 6000 7200 8100 7200 576 覆盖次数 56 76 80 80 96 108 96 576 道间距/m 12.5 炮间距/m 37.5 工作压力/Pa 2000 震源容量/ci 2940 2940 2940 3580(3360) 6420 5040 6390 6390 震源沉放深度/m 8(6) 8 8(6、10) 8(6) 10 10-7-7-10 (9-9-9-9) 10-10-10-10 (10-7-7-10) 10-10-10-10 电缆沉放深度/m 12(10) 12 12(8、14) 12(8、10、14) 12(14、16、20) 12 16(20) 16 注：表中括号内为海上试验参数
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表 3 南黄海盆地陆相中—新生界构造单元划分沿革
Table 3. Tectonic units of the terrestrial Mesozoic-Cenozoic basin of the South Yellow Sea basin
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表 4 南黄海盆地海相中-古生界构造单元划分
Table 4. Tectonic units of the Marine Mesozoic-Paleozoic basin of the South Yellow Sea basin
基本构造单元 一级构造活动带 二级构造活动带 总体特征 南黄海盆地 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。 崂山断隆带 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。 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。
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