作者:姜涛;辛仁臣; 时间:2015-01-01 点击数:
姜涛;辛仁臣;
1:中国地质大学(北京)海洋学院
摘要(Abstract):
根据测井、录井、地震、岩心和古生物资料,运用层序地层学、沉积岩石学理论,建立松辽盆地北部西斜坡姚家组层序格架,分析四级层序格架沉积微相的分布和沉积体系的组合类型.结果表明:松辽盆地北部西斜坡姚家组划分为2个四级层序(Cp1-s3、Cs2),其中四级层序Cp1-s3划分为四级湖泊扩张体系域(Ep1)和四级湖泊萎缩体系域(Ss3);四级层序Cs2只发育四级湖泊扩张体系域(Es2).自下而上,Ep1地层分布范围最小,尖灭线位于西斜坡的东部;Ss3地层分布范围增大,尖灭线位于西斜坡的中部;Es2尖灭线继续向西推进,地层分布范围达到最大.剖面上,三级和各四级层序界面附近以富砂的下切谷充填、三角洲前缘和滨浅湖砂质滩坝为主;富泥的滨浅湖混合滩微相在四级层序最大湖泛面附近最为发育.平面上,姚家组沉积初期,湖岸线在西部斜坡区东部波动,物源供给充足,沉积相以三角洲相为主;至姚家组沉积末期,湖岸线向斜坡西侧大规模推移,发育下切谷充填—三角洲—湖泊沉积分布格局.不同的四级层序体系域的沉积微相分布有明显的差异性和一定的继承性.
关键词(KeyWords):松辽盆地北部;西部斜坡;姚家组;层序地层学;沉积微相;沉积岩石学;层序格架
Abstract:
Keywords:
基金项目(Foundation):国家科技重大专项(2011ZX05001002)
作者(Author):姜涛;辛仁臣;
Email:
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