Cenozoic Stratigraphy Deformation History in the Central and Eastern of Qaidam Basin by the Balance Section Restoration and its Implication

查看全文 作　　者：LIU [1,2]Dongliang;FANG [1]Xiaomin;GAO [3]Junping;WANG [1]Yadong;ZHANG [1]Weilin;MIAO [1]Yunfa;LIU [1,2]Yongqian;ZHANG [4]Yuezhong

机构地区：[1]Center of Basin Resources and Environment, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100085, China;[2]Graduate School, Chinese Academy of Sciences, Beijing 100049, China;[3]Key Laboratory of Western China's Environmental Systems, Ministry of Education of China, College of Resources and Environment, Lanzhou University, Lanzhou 730000, China;[4]Research Institute of Petroleum Exploration and Development, PetroChina Qinghai Oilfield Company, Dunhuang, Gansu 736202, China

出　　处：《Acta Geologica Sinica(English Edition)》索引2009年第83卷第2期,共13页

基　　金：co-supported by the President Fund and Innovation Program of Chinese Academy of Sciences(no.:kzcx2-yw-104);the Chinese National Science Foundation grants(no.:40334038);the Science and Technology Key Project of Ministry of Education of China(no.:306016). 摘　　要：Qaidam 盆,在 Qinghai 西藏高原的北边缘定位了,是大中生代新生代盆,和熊巨大的厚新生代阶层。自从 ∼55 妈,印第安人欧亚的板板碰撞的地质的事件是记录的井。在高分辨率的地层学基于最近的进步,平衡的节的一种技术被用于六东北西南地质的地震侧面在 Qaidam 盆中央、东方重建外壳的弄短变丑历史在新生代碰撞期间。结果证明 Qaidam 盆开始弄短对早碰撞将近同步的变丑,作为弱压缩表明,变丑在中间期间并且晚显著地增加了始新世,然后稍微变弱并且开始后来很快加速了晚中新世,特别第四级,反映这强大的有压缩性的变丑并且快速在 Qaidam 盆附近北西藏的高原高举。 关键词：中新生代盆地柴达木盆地地层变形东欧中欧历史青藏高原北部高分辨率地层学

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Cenozoic Stratigraphy Deformation History in the Central and Eastern of Qaidam Basin by the Balance Section Restoration and its Implication

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