摘要
本文从沉积学、生物地层学、构造地质学和石油地质学等多学科的相互配合,在研究唐王寨地区泥盆纪沉积-生物地层史的基础上,探讨了该区逆冲推覆体的形成机制,指出了前缘三角区及枫顺场背斜是含油气有利地区。
Based on researching the sedimentation-biostratigraphic history of Devonian at Tangwangzhai Re-gion by use of a wide range of disciplines such as sedlmentology, biostratigraphy, structural geology and petroleum geology, etc., this paper discusses the mechanism of forming overthrust nappe at this region and points out that the frontal delta area and Fengshunchang Anticline are the favourable areas for oil and gas prospects.
出处
《天然气工业》
EI
CAS
CSCD
北大核心
1990年第6期1-8,共8页
Natural Gas Industry
关键词
泥盆纪
生物地层学
推覆体
油气
Longmen Mountains,Devonian,biostratigraphy,nappe,oil-and gas-bearing.
