| 太行山南缘新生代的隆升与断陷过程 |
| |
| 关键词:Taihangshan uplift planation surface terrace active fault |
| 基金项目:中国云台山世界地质公园地学背景研究项目; 地质大调查项目(编号:1212010511508) |
| 作者 | 单位 | E-mail | | 马寅生 | 中国地质科学院地质力学研究所,北京100081
中国地质科学院地壳变形地表过程重点开放实验室,北京100081 | mayinsheng@sohu.com | | 赵逊 | 中国地质科学院,北京100037 | | | 赵希涛 | 中国科学院地质与地球物理研究所,北京100029 | | | 吴中海 | 中国地质科学院地质力学研究所,北京100081 | | | 高林志 | 中国地质科学院地质研究所,北京100037 | | | 张岳桥 | 中国地质科学院地质力学研究所,北京100081 | | | 赵汀 | 中国地质科学院矿产资源所,北京100037 | | | 吴珍汉 | 中国地质科学院地质力学研究所,北京100081 | | | 扬守政 | 河南省地矿局第二地质大队,河南焦作454002 | |
|
| 摘要点击次数: 3918 |
| 全文下载次数: 2811 |
| 摘要: |
| The Cenozoic Rifting and Uplifting Process on the Southern Margin of Taihangshan Uplift |
| Based on an investigation into the planation surfaces, terraces, piedmont rift basins and active faults, this paper deals with the process of rifting and uplifting on the southern margin of Taihangshan uplift. It is considered that the tectonic activities on the southern margin of Taihangshan uplift have been characterized by rifting and uplifting of faults since Cenozoic, and these activities can be divided into three relatively stable planation periods and three rapid uplifting stages, which resulted in the formation of three planation surfaces. The rapid uplifting process can be divided into six relatively rapid uplifting and six relatively stable accumulation stages since Quaternary, with the development of six river terraces. Rifting was violent in Paleogene. The faults were not active in Quaternary except the piedmont faults. |
| MA Yin-sheng,ZHAO Xun,ZHAO Xi-tao,WU Zhong-hai,GAO Lin-zhi,ZHANG Yue-qiao,ZHAO Ting,WU Zhen-han,YANG Shou-Zheng.2007.The Cenozoic Rifting and Uplifting Process on the Southern Margin of Taihangshan Uplift[J].Acta Geoscientica Sinica,28(3):219-233. |
| 查看全文 查看/发表评论 下载PDF阅读器 |
|
|
|
|
|