资源调查与环境2011，Vol.32Issue(3)：177-186,10.
内蒙古固阳盆地东北缘地层学、沉积学、构造学研究的新进展
New progress in study on stratigraphy, sedimentology and tectonics in eastern edge of Guyang basin, Inner Mongolia
蔡雄飞 1王浩霖 2罗中杰 1吴衣布2
作者信息
- 1. 中国地质大学地球科学学院,武汉430074
- 2. 中国地质大学生物地质与环境地质教育部重点实验室,武汉430074
- 折叠
摘要
Abstract
Strata in the studied area are mainly composed of contrastive old and new strata that caused us to adopt different ideas and working methods to study them respectively. The old strata prior to the Middle Proterozoic are researched by using of a combinative method of tectonics with sedimentology, while the new strata are studied by using of a recent stratigraphie method besides a conventional method. Basing on the careful study on the re- cent strata, particularly, by the combinative study of Pliocene and Pleistocene, this paper identified the time and characteristics of uplifting of Inner Mongolia plateau for the first time. In addition, it draws inspiration for studying flood deposition.关键词
新进展/地层学/沉积学/固阳盆地/内蒙古Key words
new progress/stratigraphy/sedimentology/Guyang basin/Inner Mongo-lia分类
天文与地球科学引用本文复制引用
蔡雄飞,王浩霖,罗中杰,吴衣布..内蒙古固阳盆地东北缘地层学、沉积学、构造学研究的新进展[J].资源调查与环境,2011,32(3):177-186,10.
