| 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 |
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| 引用本文： | 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].火山地质与矿产,2011(3):177-186. |
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| 作者姓名： | 蔡雄飞 王浩霖 罗中杰 吴衣布 |
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| 作者单位： | [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 [3]中国地质大学数理学院,武汉430074 |
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| 摘 要： | 该区地层由一老一新组成。对一老一新地层须用不同的研究思路和工作方法。中元古界以前的地层用构造与沉积学结合方法。新地层除采用常规方法外，还采用“将今论古”的现代地层学方法。通过对新地层精细研究，尤其把上新统与更新统结合起来，首次查明了内蒙古高原隆升的时间和特点。对现代洪水沉积研究也给我们诸多的启示。
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| 关 键 词： | 新进展 地层学 沉积学 固阳盆地 内蒙古 |
New progress in study on stratigraphy, sedimentology and tectonics in eastern edge of Guyang basin, Inner Mongolia |
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| CAI Xiong-fei,WANG Hao-lin,LUO Zhong-jie,WU Yi-bu.New progress in study on stratigraphy, sedimentology and tectonics in eastern edge of Guyang basin, Inner Mongolia[J].Volcanology & Mineral Resources,2011(3):177-186. |
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| Authors: | CAI Xiong-fei WANG Hao-lin LUO Zhong-jie WU Yi-bu |
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| Institution: | 1. School of Earth Sciences, China University of Geosciences, Wuhan 430074, China) (2. Biology Geology and Environmental Geology of Ministry of Education Key Laboratory, China University of Geosciences, Wuhan 430074, China) (3. Faculty of Mathematics and Physics, China University of Geosciences, Wuhan 430074. Chino |
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| 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. |
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| Keywords: | new progress stratigraphy sedimentology Guyang basin Inner Mongo-lia |
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