内蒙古固阳盆地东北缘更新统洪积物地层的发现及研究意义DISCOVERY AND SIGNIFICANCE OF PLEISTOCENE ALLUVIAL DEPOSITION IN GUYANG BASIN NORTHEAST MARGIN,INNER MONGOLIA
蔡雄飞,智铎强,罗中杰,吴义布
摘要(Abstract)：
关于内蒙古高原的隆升,长期以来研究较少,从更新世的冲、洪积物分布在现今1600～1700m海拔高程的山顶上出发,发现固阳盆地东北缘更新统的洪积物的沉积类型、沉积特点和粗碎屑岩系的组分以及孢粉的资料,无不与内蒙古高原隆升紧密相关。内蒙古高原隆升不是孤立的,而是受青藏高原隆升的控制,它们几乎是同步的或者说紧密相连的。
关键词(KeyWords)： 粗碎屑岩系;高原隆升;更新统;第四系;固阳盆地;内蒙古
基金项目(Foundation): 中国地质调查局宁夏1/5万《要坝幅》、《黄旗口幅》、《木井子幅》和《井子泉幅》区调项目
作者(Author): 蔡雄飞,智铎强,罗中杰,吴义布
DOI: 10.19839/j.cnki.dcxzz.2011.02.010
参考文献(References)：
- 蔡雄飞,刘德民,魏启荣,顾延生,袁晏明,李德威,王国灿,罗中杰.2008.古新世—中新世以来青藏高原北缘隆升的特征——来自可可西里盆地的报告.地质学报,82(2):194-202
- 崔之久等.1996.泥石流沉积与环境.北京:海洋出版社.5-24
- 段志明,李勇,沈战武,祝向平,钟成全.2007.青藏高原腹地温泉地区新生代生态环境演化与高原表面隆升过程分析.中国地质,34(4):688-696
- 刘显臣,赵清华,王洁玉.2004.吉林省敦化市泥石流地质灾害发育规律与防治对策.吉林地质,23(4):28-33
- 徐仁.1981.大陆漂移与喜马拉雅山上升的古植物学证据,见:中国科学院青藏高原综合科学考察队编.青藏高原隆升的时代、幅度和形式问题.北京:科学出版社.8-18
- Cai Xiong-fei,Liu De-min,Wei Qi-rong,Gu Yan-sheng,Yuan Yan-ming,Li De-wei.Wang Guo-can&Lu Zhong-jie.2008.Char-acteristics of north of tibetap plateau uplift at paleocene-mio-cene:the evidence from Kekexili Basin.Acta Geologica Sinica,82(2):194-202
- Cui Zhi-jiuet al.1996.forward debris flow deposition and the envi-ronment.Beijing:Ocean Press.5-24
- Duan Zhi-ming,Li Yong,Shen Zhan-wu,Zhu Xiang-ping&ZhongCheng-quan.2007.Analysis of the evolution of the Cenozoicecological environment and process of plateau surface uplift inthe Wenquan area in the interior of the Qinghai-Tibet Plateau,Geologyin China,34(4):688-696
- Liu Xian-chen,Zhao Qing-hua&Wang Jie-yu.2004.The developedregularities of mud rock flowin the Dunhua area,Jilin Provinceandits controlling.Jilin Geology,23(4):28-33
- Xu Ren.1981.continental drift and the Himalayas rising palaeobo-tanical evidence.In:Chinese Academy of Sciences,the Qing-hai-Tibet Plateau comprehensive scientific expedition team.Times the uplift of the Qinghai-Tibet Plateau,magnitude andform.Beijing:Science Press.8-18