南黄海盆地油气资源调查新进展
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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。
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 60 s 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 LowerYangtze 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.
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 60 s 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 LowerYangtze 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.
引文
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