• 责任者：Li Yangchun (Faculty of Earth Science and Resources ; China University of Geosciences ; Beijing 100083 ; China) ; Wang Yan
• 刊名：Geology in China
• 出版年：2013
• 卷期：40(2)
• 关键词：碎屑岩 ; clastic rocks ; 物源区 ; provenance ; 元素地球化学 ; elements geochemistry ; 大兴安岭 ; Greater Hinggan Mountains
• 页码：p.391-402
• 图表：9 illus., 3 tables, 37 refs.
• 分类号：0803
• issnNo：ISSN1000-3657
• isbnNo：CN11-1167/P

     The Tongshan Formation is a very important part of Zalantun-Duobaoshan island arc tectonic belt in northern Zalantun area of the Da Hinggan Mountains. The properties, deposition epoch and tectonic environment type of the source area of Tongshan Formation are important links in the study of the island arc tectonic belt, and also constitute an important window in the study of early tectonic evolution of the old Asian Ocean tectonic domain. The research results provide an important basic material for determining the evolution of the early Paleozoic Zalantun-Duobaoshan island arc tectonic belt and also offer a new constraint for the investigation of the continental crustal evolution on the southern margin of the Siberia plate and the researches on tectono-dynamics.