摘要
潜江凹陷为一陆相断陷湖盆。运用T-R旋回的基本概念与原理,结合潜江凹陷测井、地震及岩心资料,将潜江组划分为8个三级T-R旋回层序,同时建立了该凹陷T-R旋回层序地层学模式。在此基础上,识别出扇三角洲、湖底扇和深湖—半深湖等沉积体系。查明了该区主要层段的砂体分布规律,确立有利于非构造圈闭发育的砂体类型,并提出了有利的勘探方向。
Qianjiang Depression is a continental fault lacustrine basin. By using basic T-R (Transgression Regression) cyclic concepts and principles eight third-grade T-R sedimentary cycles were classi-fled in the Qianjiang Formation according to comprehensive research of log data,seismic data and core samples. And the sequence stratrigraphic framework pattern of T-R cycles in the depression was established. Sedimentary systems were identified including fan delta,sublacustrine fan and deep lake-semi deep lake facies. The sandbodies distribution in major target intervals and favorable sandbody types for nonstructural traps development were recognized, as well as the favorable exploration direction was proposed.
出处
《油气地质与采收率》
CAS
CSCD
北大核心
2008年第2期70-74,共5页
Petroleum Geology and Recovery Efficiency
基金
湖北省自然科学基金项目"断陷湖盆层序地层学格架的盆地模拟实验"(2000A51007)