琼东南盆地渐新统煤系(扇)辫状河三角洲特征
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摘要
(扇)辫状河三角洲的沉积模式和类型研究有待丰富.在沉积学、层序地层学理论指导下,精细刻画了琼东南盆地渐新统煤系(扇)辫状河三角洲的发育与分布特征,建立了渐新统层序地层格架,识别出6个三级层序,分别与崖城组和陵水组的3个段对应;根据同沉积地貌、断层活动性等特征,划分了断崖型、断坡型、断沟型、横向背斜型与断弯型5种(扇)辫状河三角洲类型(可进一步细化为外部物源、内部物源两个亚类),分析了渐新统不同沉积期(扇)辫状河三角洲的发育特征与分布规律,归纳了低位、海侵和高位体系域中(扇)辫状河三角洲的发育特征,阐明了层序地层格架下不同体系域内(扇)辫状河三角洲的发育位置、规模和纵向叠加的差异和规律.
More studies are needed in the analyse of sedimentary patterns and types of( fan) braided river deltas. In order to understand the development features and distribution of( fan) braided river delta of Oligocene coal measures in Qiongdongnan Basin,sedimentology and sequence stratigraphy have been studied on the basis of related theories and methods. Through the systematic analysis,the characteristics of the coal measures( fan) braided river delta of the Oligocene were described in detail,the basin wide sequence stratigraphic framework of the Oligocene was established,and 6 third-order sequences were identified,respectively corresponding to the 3 sections of Yacheng Formation and Lingshui Formation. According to the characters of the synsedimentary landform,fault activity,etc,five types of( fan) braided river delta( bluff,cut slope,groove type,horizontal type anticline and fault bend) were divided in Oligocene,and two sub-types of internal source and external source were further identified. It is concluded that the sequence stratigraphic framework show differences and regularity in the location,scale,and longitudinal superposition of( fan) braided river delta in different system tracts.
More studies are needed in the analyse of sedimentary patterns and types of( fan) braided river deltas. In order to understand the development features and distribution of( fan) braided river delta of Oligocene coal measures in Qiongdongnan Basin,sedimentology and sequence stratigraphy have been studied on the basis of related theories and methods. Through the systematic analysis,the characteristics of the coal measures( fan) braided river delta of the Oligocene were described in detail,the basin wide sequence stratigraphic framework of the Oligocene was established,and 6 third-order sequences were identified,respectively corresponding to the 3 sections of Yacheng Formation and Lingshui Formation. According to the characters of the synsedimentary landform,fault activity,etc,five types of( fan) braided river delta( bluff,cut slope,groove type,horizontal type anticline and fault bend) were divided in Oligocene,and two sub-types of internal source and external source were further identified. It is concluded that the sequence stratigraphic framework show differences and regularity in the location,scale,and longitudinal superposition of( fan) braided river delta in different system tracts.
引文
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Feng,Y.L.,2006.Control of Valley and Tectonic Slops Break Zone on Sand Bodies in Rift Subsidence Basin.Acta Petrolei Sinica,27(1):13-16(in Chinese with English abstract).
Gao,X.H.,Fang,J.,Zhang,J.,et al.,2008.Control Factors for Structure of Stratigraphic and Lithologic Reservoirs in the Lower Cretaceous of Erlian Basin.Acta Petrolei Sinica,29(5):663-669(in Chinese with English abstract).
Hu,Z.M.,Zheng,L.J.,Yin,S.L.,et al.,2016.Reservoir Architecture of Braided Delta Front on Gentle Slope.China Sciencepaper,11(9):1005-1010(in Chinese with English abstract).
Jia,Z.Z.,Lin,C.Y.,Dong,C.M.,et al.,2014.Shallow Delta Reservoir Architecture Analysis on Putaohua Oil Formation in Shengping Oilfield.Journal of China University of Petroleum(Natural Science Edition),38(6):9-17(in Chinese with English abstract).
Jiao,Y.L.,Zhou,H.M.,Zhuang,X.G.,et al.,1998.Fan Deltaic Depositional Systems and Their Relationship to Oil and Gas Accumulation.Acta Sedimentologica Sinica,16(1):70-75(in Chinese with English abstract).
Li,S.T.,1996.Study on Sedimentary System of Energy-Bearing Basin.China University of Geosciences Press,Wuhan(in Chinese).
Li,W.H.,Zhang,Z.H.,Li,Y.C.,et al.,2011.Geochemical Characteristics and Hydrocarbon Generation of Paleogene Oligocene Source Rocks in Qiongdongnan Basin.Natural Gas Geoscience,22(4):700-709(in Chinese with English abstract).
Li,X.X.,2004.Study on Structural Dynamics and Hydrocarbon Accumulation in Qiongdongnan Basin(Dissertation),Guangzhou Institute of Geochemistry,Chinese Academy of Sciences,Guangzhou(in Chinese with English abstract).
Li,Y.C.,Mi,L.J.,Zhang,G.C.,et al.,2011.The Formation and Distribution of Source Rocks for Deep Water Area in the Northern of South China Sea.Acta Sedimentologica Sinica,29(5):970-979(in Chinese with English abstract).
Li,Z.X.,He,Y.P.,Liu,H.Y.,et al.,2010.Sedimentology Characteristics and Coal-Forming Models in Yacheng Formation of Qiongdongnan Basin.Acta Petrolei Sinica,31(4):542-547(in Chinese with English abstract).
Li,Z.X.,Lü,D.W.,Han,M.L.,et al.,2011.Coal Forming Environments of the Third Member of Yacheng Formation of the Paleogene in Qiongdongnan Basin for an Example.Energy Exploration&Exploitation,29(2):179-195.https://doi.org/10.1260/0144-5987.29.2.179
Pang,J.G.,Yang,Y.Y.,Pu,X.G.,2011.Identification Characteristics of Fan Delta,Nearshore Subaqueous Fan and Sublacustrine Fan in Fault trough Lake Basin.Journal of Lanzhou University(Natural Sciences),47(4):17-25(in Chinese with English abstract).
Postma,G.,1990.An Analysis of the Variation in Delta Architecture.Terra Nova,2(2):124-130.https://doi.org/10.1111/j.1365-3121.1990.tb00052.x
Qayyum,M.,Lawrence,R.D.,Niem,A.R.,1997.Discovery of the Palaeo-Indus Delta-Fan Complex.Journal of the Geological Society,154(5):753-756.https://doi.org/10.1144/gsjgs.154.5.0753
Sáez,A.,Anadón,P.,Herrero,M.J.,et al.,2007.Variable Style of Transition between Palaeogene Fluvial Fan and Lacustrine Systems,Southern Pyrenean Foreland,NE Spain.Sedimentology,54(2):367-390.https://doi.org/10.1111/j.1365-3091.2006.00840.x
Sanchez,E.N.,Orozco,R.C.,Gorsline,D.S.,1995.Morphology and Sedimentology of Two Contemporary Fan Deltas on the Southeastern Baja California Peninsula,Mexico.Sedimentary Geology,98(1-4):45-61.https://doi.org/10.1016/0037-0738(95)00026-5
Siggerud,E.I.H.,Steel,R.J.,Pollard,J.E.,2000.Bored Pebbles and Ravinement Surface Clusters in a Transgressive Systems Tract,Sant Lloren9 Del Munt Fan-Delta Complex,SEEbro Basin,Spain.Sedimentary Geology,138(1-4):161-177.https://doi.org/10.1016/s0037-0738(00)00148-2
Song,G.Z.,Wang,H.,Gan,H.J.,et al.,2014.Paleogene Tectonic Evolution Controls on Sequence Stratigraphic Patterns in the Central Part of Deepwater Area of Qiongdongnan Basin,Northern South China Sea.Journal of Earth Science,25(2):275-288.https://doi.org/10.1007/s12583-014-0433-7
Song,G.Z.,Wang,H.,Sun,Z.P.,et al.,2014.Paleogene Sydepositional Fault and Its Control on Sequence Architecture of Lingshui Sag,Deepwater Area of Qiongdongnan Basin,South China Sea.Journal of China University of Petroleum(Natural Science Edition),38(4):9-18(in Chinese with English abstract).
Wang,D.D.,2009.Study of High-Resolution Sequence on Paleogene System in Area of Qiongdongnan Basin(Dissertation).Shandong University of Science and Technology,Qingdao(in Chinese with English abstract).
Wang,G.F.,Wu,C.L.,Zhou,J.Y.,et al.,1998.Sequence Stratigraphic Analysis of the Tertiary in the Qiongdongnan Basin.Experimental Petroleum Geology,20(2):124-128(in Chinese with English abstract).
Wang,S.L.,Liu,H.,2014.Seismic Reflection and Depositional System of the Enping Formation in the Kaiping Depression of the Zhujiangkou Basin.Science&Technology Review,32(28-29):64-69(in Chinese with English abstract).
Wei,K.S.,Cui,H.Y.,Ye,S.F.,2001.High-Precision Sequence Stratigraphy in Qiongdongnan Basin.Earth Science,26(1):59-66(in Chinese with English abstract).
Wen,Q.,2011.Sedimentary Characteristic of Hailaer Basin in Cretaceous.Journal of Daqing Petroleum Institute,35(3):17-23(in Chinese with English abstract).
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