摘要
根据野外露头、钻井岩心、测井和地震资料,建立松辽盆地各级层序的识别标志和层序地层格架,将松辽盆地地层划分为白垩纪裂谷盆地巨层序和第三纪裂谷盆地巨层序,并将白垩纪裂谷盆地巨层序进一步划分为3个超层序组,7个超层序和19个层序。松辽盆地构造演化经历了断陷期、坳陷期和萎缩期3个阶段,断陷湖盆与坳陷湖盆成因机制不同。因此,层序地层内部特征及充填序列有较大差别。通过对层序地层格架内各体系域生储盖层发育特征、组合规律和油气聚集规律研究认为:水退体系域是储集砂体最发育、油气资源量最多的层段,其次为低水位和水进体系域,高水位体系域含油气较差。
Based on outcrops,cores, well logs and seismic data, the identification mark and the stratigraphic sequence framework of different levels of sequence stratigraphy have been set up. Upper Cretaceous-Tertiary of Songliao Basin can be classified into Cretaceous rift basin megasequence and Tertiary rift basin megasequence. The Cretaceous rift basin megasequence can be classified into 3 supersequence sets, 7 supersequenes and 19 sequences. The tectonic evolution of Songliao Basin can be divided into three stages: fault basin, sag basin and withered basin. So the different mechanism of the fault basin and sag basin results in different sequence features and different filling series.According to the formations of source, reservoir and cover rocks and oil-gas gathering rule of each system tract in the sequence stratigraphic frame it can be concluded that RST developed the best reservoir sandbodies and enough oil-gas resource. On the other hand, LST, TST and HST were relatively poor on both aspects.
出处
《吉林大学学报（地球科学版）》
EI
CAS
CSCD
北大核心
2004年第2期216-221,共6页
Journal of Jilin University：Earth Science Edition
基金
九五"石油天然气总公司重点攻关项目(970210-2-3)
关键词
县序地层
体系域
断陷盆地
坳陷湖盆
油气聚集
Songliao Basin
sequence stratigraphy
systems tract
fault lacustrian basin
depression lacustrian basin
oil-gas gathering rule
