万昌地区永二段水下滑塌扇内上倾尖灭砂体识别
摘要
上倾尖灭型油气藏是岩性油气藏的基本类型之一.对上倾尖灭砂体的识别是岩性油气藏勘探的任务之一.在对比单一利用地震资料、地震属性和波阻抗反演等方法进行砂体识别的优缺点后,提出运用波阻抗和瞬时相位相叠合的新方法对砂体进行识别.运用此方法,对万昌地区水下滑塌扇内部上倾尖灭砂体进行了精细解释和分析.得出以下结论:(1)通过钻井岩心识别沉积相类型,结合均方根振幅属性和同沉积断层分布情况,可以准确地确定伊通盆地万昌地区永二段水下滑塌扇的分布范围;(2)用波阻抗和瞬时相位属性联合的方法对水下滑塌扇内部上倾尖灭砂体进行识别取得了较好的效果,万昌地区WC1井附近水下滑塌扇内至少有两期最具油气勘探价值的上倾尖灭砂体.
Updip pinch-out reservoir is one of the lithologic reservoirs.Identifying updip pinch-out reservoir is a major task of lithological reservoir exploration.In this study,analysis of the 3D seismic reflection,instantaneous phase and acoustic impedance is conducted to identify and interpret the sandstone.It is found that the combined data of acoustic impedance and the instantaneous phase has better detectability and is more reliable indicator of the sandstone distribution than any of these individual seismic data including the 3D seismic reflection,instantaneous phase and acoustic impedance.In Wanchang area,combined analysis of the acoustic impedance and instantaneous phase in the subaqueous slump fans is a valid approach for identifying and interpreting the updip pinch-out sandstone.Two major findings are as follows:(1)Combined analysis of the cores,seismic attribution and the distribution of the synsedimentary faults could exactly identify the distribution of the subaqueous slump fans in the Wanchang area.(2)After identifying updip pinch-out sandstone in subaqueous slump fans using acoustic impedance and the instantaneous phase in the Wanchang area,there are at least two stages updip pinch-out sandstone near well WC1 in subaqueous slump fans which are most potential in Wanchang area.
Updip pinch-out reservoir is one of the lithologic reservoirs.Identifying updip pinch-out reservoir is a major task of lithological reservoir exploration.In this study,analysis of the 3D seismic reflection,instantaneous phase and acoustic impedance is conducted to identify and interpret the sandstone.It is found that the combined data of acoustic impedance and the instantaneous phase has better detectability and is more reliable indicator of the sandstone distribution than any of these individual seismic data including the 3D seismic reflection,instantaneous phase and acoustic impedance.In Wanchang area,combined analysis of the acoustic impedance and instantaneous phase in the subaqueous slump fans is a valid approach for identifying and interpreting the updip pinch-out sandstone.Two major findings are as follows:(1)Combined analysis of the cores,seismic attribution and the distribution of the synsedimentary faults could exactly identify the distribution of the subaqueous slump fans in the Wanchang area.(2)After identifying updip pinch-out sandstone in subaqueous slump fans using acoustic impedance and the instantaneous phase in the Wanchang area,there are at least two stages updip pinch-out sandstone near well WC1 in subaqueous slump fans which are most potential in Wanchang area.
引文
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Jia,C.Z.,Zhao,W.Z.,Zou,C.N.,et al.,2004.Two KeyTechnologies about Exploration of Stratigraphic/Lithol-ogical Reservoirs.Petroleum Exploration and Develop-ment,31(3):3-9(in Chinese with English abstract).
Klefstad,L.,Kvarsvik,S.,Rings,J.E.,et al.,2005.Char-acterization of Deeply Buried Heterolithic Tidal Reser-voirs in the Smorbukk Field Using Inverted Post-StackSeismic Acoustic Impedance.Petroleum Geoscience,11(1):47-56.doi:10.1144/1354-079304-630
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Li,B.C.,Sun,K.,Bai,H.B.,et al.,2009.Sequence Strati-graphic Framework and Sequence Components of theYitong Basin.Lithologic Reservoirs,21(4):28-31(inChinese with English abstract).
Li,J.H.,Pang,X.Q.,Song,B.,et al.,2011.A New Quanti-tative Prediction Method for Lithologic Reservoirs Dis-tribution:A Case from the Damintnu Sag.PetroleumExploration and Development,38(6):756-763(inChinese with English abstract).
Li,M.,Hou,L.H.,Zou C.N.,et al.,2005.Lithologic Stra-tigraphic Reservoirs Geophysical Exploration Technolo-gy and Application.Petroleum Industry Press,Beijing,52-146(in Chinese).
Li,X.F.,Chen,Q.M.,Zhang,X.H.,et al.,2002.The Yi-tong Graben—the Structural Features and Evolution ofa Strike-Slip Fault Basin.Petroleum Geology&Exper-iment,24(1):19-24(in Chinese with English ab-stract).
Liang,F.K.,Yu,X.H.,Li,X.P.,et al.,2011.GrowthFaultsin Shenxian Depression and Their Control overthe Sedimentation.Geology in China,38(2):263-270(in Chinese with English abstract).
Rezvandehy,M.,Aghababaei,H.,Raissi,S.H.T.,2011.In-tegrating Seismic Attributes in the Accurate Modelingof Geological Structures and Determining the Storage ofthe Gas Reservoir in Gorgan Plain(North of Iran).Journal of Applied Geophysics,73(3):187-195.doi:10.1016/j.jappgeo.2010.12.008
Shan,J.F.,Chen,Z.Y.,Hui,X.F.,2005.Forming Condi-tions of Lithologic Reservoir in Transition Zone ofWestern Liaohe Depression.Petroleum Explorationand Development,32(6):42-45(in Chinese with Eng-lish abstract).
Shanmugam,G.,Shrivastava,S.K.,Das,B.,2009.SandyDebrites and Tidalites of Pliocene Reservoir Sands inUpper-Slope Canyon Environments,Offshore Krishna-Godavari Basin(India):Implications.Journal of Sedi-mentary Research,79(9):736-756.doi:10.2110/jsr.2009.076
Shi,W.Z.,Kong,M.,Song,Z.F.,2008.Multi-ProvenanceFan Delta in the Sheling Formation,Liangjia Area,Yi-tong Basin,China.Earth Science—Journal of China University of Geosciences,33(3):365-370(in Chinesewith English abstract).
Shi,W.Z.,Zhao,Z.K.,Jiang,T.,et al.,2012.IdentifyingUpdip Pinch-Out Sandstone in Nearshore SubaqueousFans Using Acoustic Impedance and the InstantaneousPhase in the Liangjia Area,Yitong Basin,China.Marineand Petroleum Geology,30(1):32-42.doi:10.1016/j.marpetgeo.2011.10.010
Taner,M.T.,Koehler,F.,Sheriff,R.E.,1979.ComplexSeismic Trace Analysis.Geophysics,44(6):1041-1063.doi:10.1190/1.1440994
Tang,D.Q.,He,S.,Chen,H.H.,et al.,2009.FaultSystem's Characteristics of Yitong Basin and Its Evolu-tion.Journal of Jilin University(Earth Science Edi-tion),39(3):386-396(in Chinese with English ab-stract).
Tang,D.Q.,Chen,H.H.,Sun,J.Z.,et al.,2010.CenozoicTectonic Evolution of the Yitong Part of the Tan LuFault Zone and Its Control on Yitong Basin.Geotectoni-ca et Metallogenia,34(3):340-348(in Chinese withEnglish abstract).
Tong,H.M.,2002.The Property and Evolution of BoundaryFaults of Yitong Graben.Journal of Geomechanics,8(1):35-42(in Chinese with English abstract).
Wang,J.,Xu,X.J.,Chen,X.Y.,et al.,2007.Structural andSedimentary Features and Types of Hydrocarbon Res-ervoir in Southern Chaluhe Fault Depression of YitongGraben.Global Geology,26(2):240-244(in Chinesewith English abstract).
Wang,N.,Chen,B.N.,Zai,J.F.,2000.Reservoir FormingIndex for the Lithological Oil Reservoir.Petroleum Ex-ploration and Development,27(6):4-8(in Chinesewith English abstract).
Wang,X.L.,He,S.,Shi,W.Z.,et al.,2013.The Synsedi-mentary Faults Derived from Strike-Slip MovementControl the Deposition of Sheling Formation in Liangjia-Wanchang District,Yitong Basin.Oil Geophysical Pros-pecting,48(1):134-143(in Chinese with English ab-stract).
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