南黄海盆地基底及海相中、古生界地层分布特征
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摘要
南黄海盆地是大型海相中、古生界和陆相中、新生界两期叠合型盆地,本文根据最新地震资料结合钻井资料及与海陆地质资料的对比研究对盆地内地震层序进行了划分,得到了陆相中、新生界盆地基底即中、古生界海相盆地的顶界埋深、三叠系和上二叠统的残留厚度,推断了陆相层基底地层分布,并根据磁力异常资料推测了海相中、古生界盆地结晶基底埋深,推断了海相中、古生界整体残留情况.下三叠统青龙组和上二叠大隆及龙潭组在南黄海盆地南部坳陷及勿南沙隆起广泛存在,而在北部坳陷的分布则狭窄,中部隆起则由于隆起和剥蚀作用导致这两套地层几乎没有残余.对中-古生界海相盆地和中-新生界陆相盆地的基底特征进行了比较,认为海相中、古生界在南黄海地区区域性存在,海相层厚度分布特征受基底起伏控制,同时受到印支板块运动的影响,中部隆起区是海相中、古生界比较稳定的地区.下古生界可能在南黄海盆地广泛分布,但受资料限制,还难以获知其残余地层的特征.
The South Yellow Sea basin is a large superposed basin composed of a PaleozoicMesozoic marine sedimentary basin and Mesozoic-Cenozoic terringenous sedimentary basin.The structure and stratigraphic distribution of the lower crystal basement and the upper folded basement of the two kinds of basins are discussed based on integrated geological and geophysical data.New seismic data interpretation combined with drilling data and geological correlation between land and sea are used to identify the marine Paleozoic-Mesozoic stratigraphic sequence.The depth of the top surface of the marine Paleozoic-Mesozoic strata is determined by seismic interpretation;undulation of the bottom surface is derived by magnetic inversion.The residual thickness of Triassic Qinglong limestone and upper Permian strata is also analyzed in order to understand the distribution and structure features of the marine Paleozoic-Mesozoic strata.The thickness and distribution of the marine sequence are mainly controlled by the undulation of the basement,and also influenced greatly by the Indosinian movement.The thickness of the marine Paleozoic-Mesozoic strata is comparatively stable in the central uplift.The lower Triassic Qinglong formation and the upper Permian Dalong and Longtan formations are widely distributed in the southern depression and the Wunansha uplift of the South Yellow Sea basin,while the distribution of this sequence in the northern depression is very limited;in the central uplift,few are left due to uplift and denudation.At present,the residual thickness of the lower Paleozoic remains unknown due to limited data.
The South Yellow Sea basin is a large superposed basin composed of a PaleozoicMesozoic marine sedimentary basin and Mesozoic-Cenozoic terringenous sedimentary basin.The structure and stratigraphic distribution of the lower crystal basement and the upper folded basement of the two kinds of basins are discussed based on integrated geological and geophysical data.New seismic data interpretation combined with drilling data and geological correlation between land and sea are used to identify the marine Paleozoic-Mesozoic stratigraphic sequence.The depth of the top surface of the marine Paleozoic-Mesozoic strata is determined by seismic interpretation;undulation of the bottom surface is derived by magnetic inversion.The residual thickness of Triassic Qinglong limestone and upper Permian strata is also analyzed in order to understand the distribution and structure features of the marine Paleozoic-Mesozoic strata.The thickness and distribution of the marine sequence are mainly controlled by the undulation of the basement,and also influenced greatly by the Indosinian movement.The thickness of the marine Paleozoic-Mesozoic strata is comparatively stable in the central uplift.The lower Triassic Qinglong formation and the upper Permian Dalong and Longtan formations are widely distributed in the southern depression and the Wunansha uplift of the South Yellow Sea basin,while the distribution of this sequence in the northern depression is very limited;in the central uplift,few are left due to uplift and denudation.At present,the residual thickness of the lower Paleozoic remains unknown due to limited data.
引文
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Yin Y H,Wen Z H.2010.Regional Tectonic Map(in Chinese).//Zhang H T,Zhang X H,Wen Z H,et al.Map Series ofGeology and Geophysics of Eastern China Seas and AdjacentRegions(1∶10000000).Beijing:Ocean Publishing House.
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Zhang H Q,Chen J W,Li G,et al.2009.Discovery from seismicsurvey in Laoshan uplift of the south Yellow Sea and thesignificance.Marine Geology&Quaternary Geology(in Chinese),29(3):107-113.
Zhang M H,Xu D S,Chen J W.2007.Geological structure of theyellow sea area from regional gravity and magnetic interpretation.Applied Geophysics,4(2):75-83.
Zhou X J,Yang F.2007.Tectonic evolution and prototypes analysisfrom neoproterozoic to early Paleozoic in South China.Petroleum Geology&Experiment(in Chinese),29(5):446-451.
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Cao S H.1988.Application of aeromagnetic anomalies in thebasement character study of Sichuan Basin and the reginaltectonic features of Sichuan Province.Acta Geological Sichuan(in Chinese),(2):1-9.
Chen H J,Qiu Z J.1988.Comparative petroleum geological studybetween middle Yangtze area and upper and lower Yangtzeareas.Experimental Petroleum Geology(in Chinese),10(4):305-314.
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Chen J W,Xiao G L,Liu S Q,et al.2003.Strategy of oil and gasresources explorations in China seas.Marine Geology&Quaternary Geology(in Chinese),23(4):77-82.
Dai C S.2011.Oil Gas Basin Group of China Seas and EarlyResource Assessment Techniques(in Chinese).Beijing.OceanPress.
Dai C S,Li G,Cai F,et al.2003.The pretertiary and itshydrocarbon exploration targets in Yellow Sea.China OffshoreOil and Gas(Geology)(in Chinese),17(4):225-231.
Feng Z Q,Yao Y J,Zeng X H,et al.2002.The new understandingon Mesozoic-Paleozoic structural feature and hydrocarbon prospect inthe Yellow Sea.Marine Geology Letters(in Chinese),18(11):17-20.
Guo T L.2005.Regional magnetic anomalies and basementcharacteristics of Lower Yangtze Area.Journal of Oil and GasTechnology(JJPI)(in Chinese),27(3):329-333.
Hao T Y,Mancheol S,Wang Q S,et al.2002.A study on theextension of fault zones in Yellow Sea and its adjacent areasbased on gravity data.Chinese Journal of Geophysics(inChinese),45(3):385-397.
Hou F H,Tian Z X,Zhang X H,et al.2012.Joint inversion ofgravity,magnetic and seismic data of the South Yellow SeaBasin.Oil Geophysical Prospecting(in Chinese),47(5):808-814.
Huang S,Hao T Y,Xu Y,et al.2010.Study on macro distributionof residual basin of south Yellow Sea.Chinese J.Geophys.(inChinese),53(6):1344-1353.
Jiang W W,Liu Y K,Hao T Y,et al.2001.Comprehensive studyof geology and geophysics of Sichuan basin.Progress inGeophysics(in Chinese),16(1):11-23.
Li G,Chen J W,Xiao G L,et al.2003.Petroleum prospect ofmarine Paleozoic in the South Yellow Sea.Marine GeologyLetters(in Chinese),19(8):12-16.
Li G,Zhang Y,Chen J W,et al.2004.Seismic reflectioncharacteristics and selection of hydrocarbon prospective areas inthe Terrestrial Mesozoic strata of the Yellow Sea.Periodical ofOcean University of China(in Chinese),34(6):1069-1074.
Lin N T,Gao D H,Sun J,et al.2012.Seismic attributes of thePermian and Triassic in Qingdao depression,South Yellow SeaBasin and their geological significance.Acta Petrolei Sinica(inChinese),33(6):987-995.
Liu G.1987.Basement structure and tectonic evolution of theMiddle Yangtze area.Journal of Jianghan Petroleum Institute(in Chinese),9(2):6-13.
Liu G D.1997.Preliminary discussion on residual basins.Petroleum Explorationist(in Chinese),2(3):1-4.
Liu G D.2001.Pre-Cenozoic marine residual basins.Progress inGeophysics(in Chinese),16(2):1-7.
Liu G D,Song H B,Zhang F Q.1999.A preliminary study ofChinese offshore pre-cenozoic residual basins.Progress inGeophysics(in Chinese),14(3):1-8.
Liu X L.1983.Discussion on the boundaries and tectonic evolutionof the Yangtze paraplatform in the South Yellow Sea.MarineGeology&QuaternaryGeology(in Chinese),3(2):63-77.
Ouyang K,Zhang X H,Li G.2009.Characteristics of stratigraphicdistribution in the middle uplift of South Yellow Sea.MarineGeology&Quaternary Geology(in Chinese),29(1):59-66.
Qi J H,Wen Z H,Zhang X H,et al.2013.Lithostratigraphiccorrelation of Mesozoic and Palaeozoic marine strata betweensouth Yellow Sea and upper Yangtze region.Marine Geology&Quaternary Geology(in Chinese),33(1):109-119.
Shan X L.1993.On the property of the basement formation in thepaleozoic basins of the Yangtze area.Experimental PetroleumGeology(in Chinese),15(4):370-384.
Sun H Z.1985.The evolution of basement of the Yangzi faultingblock.Scientia Geologica Sinica(in Chinese),(4):334-341.
Wan T F.2004.An Outline in tectonic of China(in Chinese).Beijing:Geological Publishing House.
Wang F,Li H J,Zhang Y G.2010.Stratigraphic geologic attributeand hydrocarbon geology in Laoshan uplift of South Yellow Sea.Marine Geology&Quaternary Geology(in Chinese),30(2):95-102.
Wu Z Q,Wu S G,Tong S Y,et a1.2004.A study on seismicacquisition basic on marine carbonate hydrocarbon exploration inthe southern Yellow Sea.Chinese J.Geophys.(in Chinese),54(4):1061-1074.
Yang J Y,Wu Z Q,Yao C L.2008.Application of 2.5gravity,magnetic and seismic joint inversion to the geological study in thesouth Yellow Sea.Marine Geology Letters(in Chinese),24(8):33-38.
Yang Q,Chen H Y.2003.Tectonic evolution of the north Jiangsusouth Yellow Sea basin.Petroleum Geology&Experiment(inChinese),25(S1):562-565.
Yin Y H,Wen Z H.2010.Regional Tectonic Map(in Chinese).//Zhang H T,Zhang X H,Wen Z H,et al.Map Series ofGeology and Geophysics of Eastern China Seas and AdjacentRegions(1∶10000000).Beijing:Ocean Publishing House.
Zhang H,Zhou L Q,Li J Q.2006.Hydrocarbon explorationpotential analysis of the lower marine formation assemblage inthe lower Yangtze region.Petroleum Geology&Experiment(in Chinese),28(1):15-20.
Zhang H Q,Chen J W,Li G,et al.2009.Discovery from seismicsurvey in Laoshan uplift of the south Yellow Sea and thesignificance.Marine Geology&Quaternary Geology(in Chinese),29(3):107-113.
Zhang M H,Xu D S,Chen J W.2007.Geological structure of theyellow sea area from regional gravity and magnetic interpretation.Applied Geophysics,4(2):75-83.
Zhou X J,Yang F.2007.Tectonic evolution and prototypes analysisfrom neoproterozoic to early Paleozoic in South China.Petroleum Geology&Experiment(in Chinese),29(5):446-451.
蔡乾忠.2002.黄海含油气盆地区域地质与大地构造环境.海洋地质动态,18(11):8-12.
曹树恒.1988.应用航磁异常探讨四川盆地基底性质及四川省区域构造特征.四川地质学报,(2):1-9.
陈焕疆,邱之俊.1988.中扬子区与上、下扬子区油气地质条件的对比分析.石油实验地质,10(4):305-314.
陈沪生,张永鸿,徐师文等.1999.下扬子及邻区岩石圈结构构造特征与油气资源评价.北京:地质出版社.
陈建文,肖国林,刘守全等.2003.中国海域油气资源勘查战略研究.海洋地质与第四纪地质,23(4):77-82.
戴春山.2011.中国海域含油气盆地群和早期评价技术.北京.海洋出版社.
戴春山,李刚,蔡峰等.2003.黄海前第三系及油气勘探方向.中国海上油气(地质),17(4):225-231.
冯志强,姚永坚,曾祥辉等.2002.对黄海中、古生界地质构造特征及油气远景的新认识.海洋地质动态,18(11):17-20.
郭彤楼.2005.下扬子地区区域磁异常和基底特征研究.石油天然气学报(江汉石油学院学报),27(3):329-333.
郝天珧,Mancheol S,王谦身等.2002.根据重力数据研究黄海周边断裂带在海区的延伸.地球物理学报,45(3):385-397.
侯方辉,田振兴,张训华等.2012.南黄海盆地两条地震剖面的重
磁数据联合反演效果.石油地球物理勘探,47(5):808-814.
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