Sedimentological Features of the Xiajiang Group and Their Constraints on the Neoproterozoic Tectonic Evolution of <?xml:namespace prefix = st1 ns = "urn:schemas-microsoft-com:office:smarttags" /><st1:place w:st="on">South China</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

Sedimentological Features of the Xiajiang Group and Their Constraints on the Neoproterozoic Tectonic Evolution of South China

详细信息

责任者：Zhang Chuanheng (State Key Laboratory of Geological Processes and Mineral Resources & Key Laboratory of Lithosphere Tectonics and Lithoprobing Technology of Ministry of Education ; China University of Geosciences ; Beijing 100083 ; China) ; Liu Yaoming
刊名：Acta Geoscientica Sinica
出版年：2009
卷期：30(4)
关键词：沉积盆地 ; sedimentary basins ; 构造演化 ; structural evolution ; 华南地区 ; South China
页码：p.495-504
图表：7 illus., 2 tables, 30 refs.
分类号：0803
issnNo：ISSN1006-3021
isbnNo：CN11-3474/P

摘要

Middle Neoproterozoic geotectonic characteristics and proto-basin types in the western part of South China have aroused much controversy and are important implications for determining the position of the Yangtze Continent within the Rodinia configuration. A debris composition analysis of 33 sandstone samples from the Qingshuijiang Formation in the middle part of the Xiajiang Group suggests that these clastic deposits were derived from a recycled orogenic belt. Geochemical features detected by the normal element analysis further indicate that the Xiajiang Group was developed in a retro-arc rift basin. Based on the above conclusions in combination with the geotectonic features of the Yanbian Group and the Suxiong Formation, it is held that the western part of South China was a component part of an active continental margin during the deposition of the Xiajiang Group.

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