Analysiss on Palaeocurrent in the Xujiajuan Formation, Xiangshan Group, Middle Ordovician, in Southern <?xml:namespace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" /><st1:place w:st="on"><st1:PlaceName w:st="on">Helan</st1:PlaceName> <st1:PlaceType w:st="on">Mountains</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

Analysiss on Palaeocurrent in the Xujiajuan Formation, Xiangshan Group, Middle Ordovician, in Southern hemas-microsoft-com:office:smarttags" />Helan Mountains hemas-microsoft-com:office:office" />

详细信息

责任者：Li Xiangdong (School of Geoscience ; Yangtze University ; Jingzhou 434023 ; China) ; He Youbin
刊名：Geological Review
出版年：2009
卷期：55(5)
关键词：古水流 ; paleocurrents ; 贺兰山 ; Helan Mountains
页码：p.653-662
图表：4 illus., 2 tables, 24 refs.
分类号：0803
issnNo：ISSN0371-5736
isbnNo：CN11-1952/P

摘要

hemas-microsoft-com:office:office" />

In this paper, the palaeocurrent data recorded in directional sedimentary structure were collected for determining the direction of turbidity currents, the dip of regional slopes in the study area, and the direction of internal wave and internal tide current. The result shows that the palaeocurrent direction of flutes presents a slightly fan-shaped from the north to the south and suggests the direction of turbidity currents, while the palaeocurrent direction of cross beddings are mainly restricted within an elongated zone extending in a NWW—NE direction suggest the direction of internal-wave and internal-tide current.

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