Response of the North China Craton to Rodinia Supercontinental Events ——GOSEN Joining Hypothesis
详细信息
- 责任者：Lu Songnian (University of Shandong Science and Technology ; Qingdao 266510 ; China) ; Xian Zhenqun
- 刊名：Acta Geologica Sinica
- 出版年：2012
- 卷期：86(9)
- 关键词：克拉通 ; craton ; 超大陆 ; supercontinents ; 华北地台 ; North China Platform
- 页码：p.1396-1406
- 图表：5 illus., 2 tables, 23 refs.
- 分类号：0300
- issnNo：ISSN0001-5717
- isbnNo：CN11-1951/P
摘要
The North China Craton （NCC） was clearly different from the Yangtze and Tarim cratons during the Late Mesoproterozoic to Early Neoproterozoic period because no distinct geological records have been found about the thermotectonic events related to assembly and breakup of the Rodinia Supercontinent. Therefore, various assumptions occur regarding relation between the NCC and the Rodinia. On the basis of the assumption, we propose a hypothesis （GOSEN joining hypothesis） that the Grenville Orogen, the southeastern margin of Siberia and eastern NCC were linked.