姬塬地区长3—长4+5油层组沉积相研究  

Study on the sedimentary facies of the member 3 and 4+5 of Yanchang Formation in Jiyuan area

作　　者：石雪峰[1] 杜海峰[1] 

机构地区：[1]中国地质大学(北京)能源学院

出　　处：《岩性油气藏》2008年第1期59-63,共5页Lithologic Reservoirs

摘　　要：姬塬地区位于鄂尔多斯盆地南部,在区域上处于鄂尔多斯盆地陕北斜坡、天环坳陷2个构造单元之间。姬塬腹地勘探程度较低,对长3和长4+5沉积体系、沉积相和储层的展布、圈闭的成藏、油气富集规律等问题有待进一步认识。该文以露头、岩心、测井曲线为基础,通过对区内岩性特征、测井曲线形态及沉积微相特征进行分析,认为姬塬地区延长组长3和长4+5油层组主要由三角洲沉积体系和湖泊沉积体系组成,并进一步分为2种亚相和5种微相。根据长3和长4+5的沉积微相的展布及演化规律可以得出研究区的沉积模式。Jiyuan area, in southern Ordos Basin, is located at the structure unit between Shanbei Slope and Tianhuan Depression. The exploratory degree is low here, thus, the study on depositional system, sedimentary facies, reservoir distribution, traps accumulation, and the hydrocarbon enrichment of the member 3 and 4＋5 of Yanehang Formation is not enough. Based on the outcrop, core and well log data, the lithologic characteristics, well log form and sedimentary mierofaeies are analyzed. The result shows that the member 3 and 4＋5 are mainly composed of delta and lacustrine depositional systems, which can be further divided into two subfacies and five microfacies. According to the distribution and evolution rule of the sedimentary mierofacies, the depositional model of the study area can be obtained.

关 键 词：沉积相 沉积模式 沉积体系 姬塬地区 

分 类 号：TE121.3[石油与天然气工程—油气勘探]