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| 太原盆地边缘地貌与新构造运动及其意义 | |
| 引用本文： | 梁文彪,李洪建,杨彩云. 太原盆地边缘地貌与新构造运动及其意义[J]. 山西大学学报(自然科学版), 2000, 23(2): 178-181 |
| 作者姓名： | 梁文彪 李洪建 杨彩云 |
| 作者单位： | 1. 山西省水文水资源勘测局,山西,太原,030001 2. 山西大学黄土高原研究所,山西,太原,030006 3. 太原市大众中学,山西,大原,030024 |
| 摘 要： | 应用构造地貌的观战把太原盆地及其边缘地貌分为：外围断块抬升山地，抬升轻微的丘陵台地，山前堆积的洪积倾斜平原和沉降堆积的冲积平原４种地貌单元。 |
| 关 键 词： | 边缘地貌 新构造运动 洪积扇 水文地质 太原盆地 |
| 文章编号： | 0253-0395(2000)02-0178-04 |
| 修稿时间： | 1999-12-01 |
Edge Geomorphology and Neotectonic Movement in Taiyuan Basin and Their Meanings |
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| LIANG Wen-biao,LI Hong-jian,YANG Cai-yun. Edge Geomorphology and Neotectonic Movement in Taiyuan Basin and Their Meanings[J]. Journal of Shanxi University (Natural Science Edit, 2000, 23(2): 178-181 | |
| Authors: | LIANG Wen-biao LI Hong-jian YANG Cai-yun |
| Affiliation: | LIANG Wen-biao;(Shanxi Survey Bureau of Hydrology and Water Resources, Taiyuan 030024,China);LI Hong-jian;(Institute of Loess Plateau ,Shanxi University , Taiyuan 030006,China);YANG Cai-yun;(Dazhong Middle School, Taiyuan 030024, China) |
| Abstract: | Based on the point of tectonic geomorphology,the geomorphology in and outside the Taiyuan Basin were divided into four geomorphologic units:periphery block rising mountain,slightly rising hill tableland,pluvial sedimentation plain,and alluvial sedimentation plain.By the analysis of edge geomorphol- ogy,landscape,earthquake characteristics,change of river system and developing feature of paleochannel, deposit depth of stratum in cenozoic,the neotectonic movement characteristics in Taiyuan Basin were as follows:rising intensely in western basin and slightly in eastern basin;on the whole rising course there were two rising centers;one was Shiqiangfeng in the northwest,the other is Mian Mountain in the south- east;the neotectonic movement in Taiyuan Basin showed a regularity of central symmetry.Moreover,the use of tectonic geomorphology and neotectonic movementin hydrology were discussed. |
| Keywords: | edge geomorphology neotectonic movement pluvial sedimentation fan paleochannel hydrology |
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