川东南地区茅口组地震相分析
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摘要
针对勘探程度不高、钻井分布不均且以二维地震资料为主的川东南地区,通过对茅口组地震相分析,发现了中高频席状地震相、中低频席状地震相、前积地震相、丘状地震相、波状地震相等多种类型。通过单井相分析和井旁地震响应模式的建立,结合区域地质背景分析并以沉积模式为指导开展了沉积相展布特征研究。认为茅口组沉积时期研究区在开阔台地相的整体背景下,局部发育的点礁、滩体、风化壳喀斯特均是有利储层发育部位,是隐蔽油气藏潜在勘探领域。
In the southeast of Sichuan Basin,the level of exporation is low,well drilling is unevenly distributed and the dominating part is 2D seismic data.By analyzing seismic facies of Maokou Formation,more than five seismic facies are identified,including the medium-high frequency mat-shaped,medium-low frequency mat-shaped,prograding structure,dome-shaped,wave seismic facies in the district.By analysing single-well facies,establishing seismic response model,and combined with the regional geological background,the authors study the sedimentary facies guided by the depositional model.They think that the open platform is the main type of sedimentary facies,and in the local area,there are patch reef,bank reservoirs and karst of weathered crust.They are favorable reservoirs and will be the next prospecting fields.This means that it is quite adapt able to carry out in the relatively low degree exploration areas of lacking drill bores,where it is very difficult to analyse plane sedimentary facies merely by drill bores.
In the southeast of Sichuan Basin,the level of exporation is low,well drilling is unevenly distributed and the dominating part is 2D seismic data.By analyzing seismic facies of Maokou Formation,more than five seismic facies are identified,including the medium-high frequency mat-shaped,medium-low frequency mat-shaped,prograding structure,dome-shaped,wave seismic facies in the district.By analysing single-well facies,establishing seismic response model,and combined with the regional geological background,the authors study the sedimentary facies guided by the depositional model.They think that the open platform is the main type of sedimentary facies,and in the local area,there are patch reef,bank reservoirs and karst of weathered crust.They are favorable reservoirs and will be the next prospecting fields.This means that it is quite adapt able to carry out in the relatively low degree exploration areas of lacking drill bores,where it is very difficult to analyse plane sedimentary facies merely by drill bores.
引文
[1]刘癸.地震相分析在深反射地震勘探资料中的应用[J].地质力学学报,2008,11(2):129-131.
[2]Sheriff,Robert.E.Seismic stratigraphy[M].Interna-tional Human Resources Development Corp,1982:25-50.
[3]吴因业,顾家裕.油气层序地层学[M].北京:石油工业出版社,2002.72-83.
[4]Gao Dengliang.Application of seismic texture modelregression to seismic facies characterization and inter-pretation[J].The Leading Edge,2008,27(3):394-397.
[5]Gao Dengliang.Application of three-dimensional seis-mic texture analysis with special reference to deep-marine facies discrimination and interpretation[J].AAPG Bulletin,2007,91(12):1665-1683.
[6]朱剑兵,赵培坤.国外地震相划分技术新进展[J].勘探地球物理进展,2009,32(3):167-171.
[7]赵正望.川东南地区构造特征及其对油气成藏的控制作用[D].北京:中国地质大学能源学院,2005.
[8]刘宝珺.沉积岩石学[M].北京:地质出版社,1980:424-430.
[9]陈宗清.四川盆地中二叠统茅口组天然气勘探[J].勘探战略,2007,2(5):1-11.
[10]于良肖.贵州赤水地区阳新统、中上三叠统及下侏罗统沉积相和储层特征研究[D].成都:西南石油学院,2003.
[11]张三元,谢迟初,凡睿.天堂坝地区茅口组岩溶缝洞体储层地震异常识别[J].江汉石油职工学报,2006,19(6):10-14.
[12]张万选,张厚福,曾洪流.陆相地震地层学[M].东营:石油大学出版社,1993:23-76.
[13]徐怀大,王世飞,陈开远.地震地层学解释基础[M].武汉:中国地质大学出版社,1990:12-145.
[14]李思田,潘元林,陆永潮,等.断陷湖盆隐蔽油藏预测及勘探的关键技术——高精度地震探测基础上的层序地层学研究[J].地球科学:中国地质大学学报,2002,27(5):592-598.
[15]朱筱敏.层序地层学[M].东营:石油大学出版社,2000:167-207.
[16]王银.川东北元坝地区生物礁的识别和追踪[J].天然气技术,2009,3(4):25-29.
[17]胡伟光,蒲勇,赵卓南,等.川东北地区长兴组生物礁的识别[J].石油物探,2010,49(1):46-53.
[18]李登华,唐跃,殷积峰,等.川东黄龙场构造上二叠统长兴组生物礁特征与潜伏礁预测[J].中国地质,2006,33(2):427-435.
[19]蒋东,高培丞,曹刚,等.黄龙场地区生物礁储层预测[J].西南石油大学学报,2009,31(2):5-7.
[20]施泽进,田亚铭,韩小俊,等.川东南下古生界地震相特征及意义[J].石油实验地质,2009,31(1):31-39.
[21]姜在兴.沉积学[M].北京:北京石油工业出版社,2003:403-441.
[2]Sheriff,Robert.E.Seismic stratigraphy[M].Interna-tional Human Resources Development Corp,1982:25-50.
[3]吴因业,顾家裕.油气层序地层学[M].北京:石油工业出版社,2002.72-83.
[4]Gao Dengliang.Application of seismic texture modelregression to seismic facies characterization and inter-pretation[J].The Leading Edge,2008,27(3):394-397.
[5]Gao Dengliang.Application of three-dimensional seis-mic texture analysis with special reference to deep-marine facies discrimination and interpretation[J].AAPG Bulletin,2007,91(12):1665-1683.
[6]朱剑兵,赵培坤.国外地震相划分技术新进展[J].勘探地球物理进展,2009,32(3):167-171.
[7]赵正望.川东南地区构造特征及其对油气成藏的控制作用[D].北京:中国地质大学能源学院,2005.
[8]刘宝珺.沉积岩石学[M].北京:地质出版社,1980:424-430.
[9]陈宗清.四川盆地中二叠统茅口组天然气勘探[J].勘探战略,2007,2(5):1-11.
[10]于良肖.贵州赤水地区阳新统、中上三叠统及下侏罗统沉积相和储层特征研究[D].成都:西南石油学院,2003.
[11]张三元,谢迟初,凡睿.天堂坝地区茅口组岩溶缝洞体储层地震异常识别[J].江汉石油职工学报,2006,19(6):10-14.
[12]张万选,张厚福,曾洪流.陆相地震地层学[M].东营:石油大学出版社,1993:23-76.
[13]徐怀大,王世飞,陈开远.地震地层学解释基础[M].武汉:中国地质大学出版社,1990:12-145.
[14]李思田,潘元林,陆永潮,等.断陷湖盆隐蔽油藏预测及勘探的关键技术——高精度地震探测基础上的层序地层学研究[J].地球科学:中国地质大学学报,2002,27(5):592-598.
[15]朱筱敏.层序地层学[M].东营:石油大学出版社,2000:167-207.
[16]王银.川东北元坝地区生物礁的识别和追踪[J].天然气技术,2009,3(4):25-29.
[17]胡伟光,蒲勇,赵卓南,等.川东北地区长兴组生物礁的识别[J].石油物探,2010,49(1):46-53.
[18]李登华,唐跃,殷积峰,等.川东黄龙场构造上二叠统长兴组生物礁特征与潜伏礁预测[J].中国地质,2006,33(2):427-435.
[19]蒋东,高培丞,曹刚,等.黄龙场地区生物礁储层预测[J].西南石油大学学报,2009,31(2):5-7.
[20]施泽进,田亚铭,韩小俊,等.川东南下古生界地震相特征及意义[J].石油实验地质,2009,31(1):31-39.
[21]姜在兴.沉积学[M].北京:北京石油工业出版社,2003:403-441.
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