摘要
To confirm the existence of the Early Cretaceous marine sediments in the Qiangtang Basin,this paper conducted a research on Shenglihe-Tuonamu region. The results show that original Suowa Formation is in the Late Jurassic-Early Cretaceous,Suowa formation is in the Late Jurassic,Weimingming Formation is in the Early Cretaceous,and Xueshan Formation is in the late Early Cretaceous-early Late Cretaceous.The formation comparison shows that the era which was initially judged as Late Jurassic-Early Cretaceous shale limestone-gypsum marine strata should be Early Cretaceous.This stratum is oil shale and the thickest in Shenglihe-Changsheshan region,which gradually becomes thinner along the east and transits into shale sediment,and into limestone sediment in the west.Regionally,the existence of the Early Cretaceous strata is important to the conditions of the underlying oil and gas storage.