Research on the Characteristics of Reef-Bank Reservoirs in Ordovician, <?xml:namespace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" /><st1:place w:st="on"><st1:PlaceName w:st="on">Tarim</st1:PlaceName> <st1:PlaceType w:st="on">Basin</st1:PlaceType></st1:place> <?xml:namespace prefix = o ns = "urn:schemas-microsoft-com:office:office" /><o:p></o:p>

设为首页

收藏本站

网站地图 | English | 公务邮箱

读者指南

学术客户端

NSTL服务站

科技查新

Research on the Characteristics of Reef-Bank Reservoirs in Ordovician, Tarim Basin

详细信息

责任者：Ruan Zhuang (State Key Laboratory of Petroleum Resource and Prospecting ; China University of Petroleum ; Beijing 102249 ; China) ; Yu Bingsong
刊名：Geoscience
出版年：2009
卷期：23(4)
关键词：生物标志化合物 ; biomarkers ; 礁 ; reefs reservoirs ; 塔里木盆地 ; Tarim Basin
页码：p.691-698
图表：5 illus., 1 table, 12 refs.
分类号：0803
issnNo：ISSN1000-8527
isbnNo：CN11-2035/P

摘要

Reef-bank reservoir in Ordovician has been discovered in several areas, Tarim Basin. Crop, core, thin section and test data indicate that the bank face always accompanies with reef face. Platform edge can be divided into four types according to the lithologic characteristic of bank face, including low energy environment, relatively low energy environment, relatively low energy environment and high energy environment. Framework reef, baffle-reef and lime mud mound represent the environment energy decreasing. Data shows that original reef-bank reservoirs reveal low porosity and permeability and reservoir space is dominated by cavity-fractured type, followed by cavity-freckle type, cavern type, freckle type and complex type. The development of reef-bank reservoirs is controlled by Palaeogeomorphology and structure while high quality reservoirs determined by karstification and clastation.

常见问题　|　交通位置　|　联系我们　|　OA远程办公

地址：北京市海淀区学院路29号邮编：100083

电话：办公室：(+86 10)66554848；文献借阅、咨询服务、科技查新：66554700