摘要
吉林省松辽盆地白垩系下统青山口组一段是油页岩的含矿层位,形成时为松辽盆地的坳陷期,油页岩是盆地两次最大湖泛期的产物,盆地内油页岩属于典型的深湖相成因。
The ore-bearing bed of oil shale of Qingshankou Formation,lower Cretaceous system in the Songliao Basin,Jilin Province were formed in down-warping stage of the Songliao Basin,which are the products of the largest two times lake deposits,and belong to the type deep lake oil shale in genesis.
出处
《吉林地质》
2010年第2期71-73,93,共4页
Jilin Geology
基金
中国地质调查局项目(1212010633501)
关键词
松辽盆地
青山口组
油页岩
沉积特征
Songliao Basin
Qingshankou Formation
oil shale
sedimentary characteristics
