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作 者:朱美衡[1]
机构地区:[1]中国石化股份胜利油田分公司地质科学研究院,山东东营257015
出 处:《油气地质与采收率》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)
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.
关 键 词:T-R旋回层序 陆相断陷湖盆 沉积体系 非构造圈闭 预测 潜江凹陷
分 类 号:TE111.3[石油与天然气工程—油气勘探]
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