摘要
冀西北下马岭组构成了一个完整的沉积旋回,在这个陆棚沉积层序中,可划分为海侵体系域与高水位体系域,两者之间的黑色页岩、硅质泥岩及油页岩是本区油苗的生油层。
The Xiamaling Formation consists of a complete depositional cycle. The shelf sequence may be divided into the transgressive systems tract and highstand syctems tract between which the black shales, siliceous mudstones and oil shales are ascribed to the cource beds of oil shows in the study area.
出处
《沉积与特提斯地质》
CAS
CSCD
1993年第4期38-45,共8页
Sedimentary Geology and Tethyan Geology
关键词
下马岭组
沉积旋回
生油层
Xiamaling Formation,depositional cycle,source bed
