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| 太行山东麓滹沱河出山处新生代沉积相与地貌结构 | |
| 引用本文： | 王乃樑,韩慕康,朱之杰,李通文,戴广秀,翟荣庭.太行山东麓滹沱河出山处新生代沉积相与地貌结构[J].第四纪研究,1985,6(1):44-59. |
| 作者姓名： | 王乃樑 韩慕康 朱之杰 李通文 戴广秀 翟荣庭 |
| 作者单位： | 1. 北京大学地理系; 2. 原水电部北京勘测设计院; 3. 地质部水文地质工程地质研究所 |
| 摘 要： | 研究区在大地构造上处于山西台背斜上的五台隆起与辽冀台向斜内的博野拗陷之间的过渡地区,在地貌上位于太行山地与华北大平原之间的过渡带、滹沱河及其主要(右岸)支流冶河出山口地区,是一片点缀有残山的宽广的山前夷平面与冲洪积扇。 |
CENOZOIC SEDIMENTARY FACIES AND LANDFORMS NEAR THE VALLEY MOUTH OF RIVER HUTOUHE ALONG THE EASTERN PIEDMONT OF MOUNTAIN TAIHANGSHAN |
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| Institution: | 1. Department of Geography, Peking University; 2. Former Peking Institute of Prospecting and Designing, Ministry of Electric Power and Water Conservancy; 3. Institute of Engineering and Hydrogeology, Ministry of Geology |
| Abstract: | Our geomorphological investigations discovered that 4 diluvial fans were formed by the river Hutouhe on leaving .the mountain valley at and around the site of the. Huangbizhuang reservoir ( Hebei Province) along the eastern piedmont of Mt. Taihangshan. They fan, Middle Pleistocene rock fan (locally covered with gravels), Eaely Pleistocene red clay and gravel fan, Middle Pleistocene gravel fan, and Late Pleistocene, loess ana gravel fan. With the exception of the middle Pleistocene diluvial fan which is buried in the eastern part of region investigated, the other three fans are geomorphologieally conspicuous, and found to dip gently eastwardl, one covering the other, it shoving that the region under study is located in a broad flexure belt between the strongly uplifted. Taihangshan mountain and the strongly subsided North China Plain.d:\PDF\.pdf |
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