• 责任者：Wan Tianfeng (School of Earth Sciences and Resources ; China University of Geosciences ; Beijing 100083 ; China)
• 刊名：Earth Science Frontiers
• 出版年：2011
• 卷期：18(3)
• 关键词：板块碰撞 ; plate collision
• 页码：p.48-56
• 图表：illus., 79 refs.
• 分类号：0300
• 出版序号：713
• issnNo：ISSN1005-2321
• isbnNo：CN11-3370/P

Based on the isotopic ages collected in some collision zones of China and Europe continents, the process from subduction to collision between plates is discussed; in this process the following events occurred in sequence: the decrease in the moving velocity of plates, the disappearance of the oceanic crust on the surface, the beginning of the collision, the formation of the strong deformation and dynamic metamorphism, the occurrence of a series of magmatism and, at last, the uplifting of mountains. Above events have extremely different isotopic ages. The initial collision age is younger than that of the oceanic crust disappearing on the surface, and older than that of the formation of strong deformation and dynamic metamorphism. Obviously, it is very difficult to determine the initial age of subduction by using the isotopic age of only one geological event.oft-com:office:office" />