• 责任者：Cai Xiongfei (School of Earth Sciences ; China University of Geosciences ; Wuhan 430074 ; China) ; Wang Haolin
• 刊名：Resources Survey & Environment
• 出版年：2011
• 卷期：32(3)
• 关键词：地层学 ; stratigraphy ; 沉积学 ; sedimentology ; 构造地质学 ; structural geology ; 内蒙古 ; Inner Mongolia
• 页码：p.177-186
• 图表：5 illus., 1 table, 6 refs.
• 分类号：1200
• 出版序号：1886
• issnNo：ISSN1671-4814
• isbnNo：CN32-1640/N

Strata in the studied area are mainly composed of contrastive old and new strata that caused the authors to adopt different ideas and working methods to study them respectively. The old strata prior to the Middle Proterozoic are researched by using a combinative method of tectonics with sedimentology, while the new strata are studied by using a recent stratigraphic method besides a conventional method. Basing on the study on the recent strata, particularly, by the combinative study of Pliocene and Pleistocene, this paper identified the time and characteristics of uplifting of Inner Mongolia Plateau.