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国土资源遥感  2013, Vol. 25 Issue (4): 113-121    DOI: 10.6046/gtzyyg.2013.04.18
  技术应用 本期目录 | 过刊浏览 | 高级检索 |
龙门山断裂带晚新生代以来分段活动的地形地貌表现
张微1, 姚琪2, 杨金中1, 于浩3, 吴建勇4
1. 中国国土资源航空物探遥感中心, 北京 100083;
2. 中国地震台网中心, 北京 100045;
3. 新疆维吾尔自治区地质矿产勘查开发局信息中心, 乌鲁木齐 830000;
4. 浙江省地质矿产研究所, 杭州 310012
Geomorphic characteristics of segmental activities of the Longmenshan fault zone since late Cenozoic
ZHANG Wei1, YAO Qi2, YANG Jinzhong1, YU Hao3, WU Jianyong4
1. China Aero Geophysical Survey and Remote Sensing Center for Land and Resources, Beijing 100083, China;
2. China Earthquake Networks Center, Beijing 100045, China;
3. Information Center of Xinjiang Bureau of Geology and Mineral Resources Exploration and Development, Urumqi 830000, China;
4. Zhejiang Institute of Geology and Mineral Resources, Hangzhou 310012, China
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摘要 为研究龙门山断裂带晚新生代以来分段活动性导致断裂周边地区差异隆升的问题,利用航天飞机雷达地形测绘使命(shuttle radar topography mission,SRTM)数字高程模型(DEM)对龙门山断裂带及其周边地区进行地形地貌整体趋势、分段性高程起伏和坡度变化特征的综合分析。分析结果表明,龙门山断裂带在地形上基本保持了上新世至早更新世强烈活动的遗迹,表现出南高北低的趋势; 但地形起伏的分布表现出明显的分段性,地形段落边界与龙门山断裂带主要段落边界一致。龙门山断裂带北段的地形地貌主要受河流侵蚀控制,但在青川断裂附近地形起伏受构造活动影响甚大; 断裂带中段地形起伏明显受构造控制; 断裂带南段构造活动对地形起伏的控制仅出现在靠近鲜水河断裂的区域。此外,地表破裂带分布的地形起伏与汶川地震造成的地表同震位移的分段性和区域变形场分布也是一致的,表明这种最新构造活动对地形地貌的改造现今仍在继续。
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王迅
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关键词 高寒草地粗蛋白监测模型HJ-1A/1B生物量    
Abstract:The segmental activity of the Longmenshan fault belt resulted in the difference in uplift of its neighboring areas. In this paper, the authors used SRTM(shuttle radar topography mission) digital elevation model(DEM) to analyze the topography,local relief and slope of the Longmenshan fault zone and its adjacent areas. The topography of the study area basically maintains the tendency of decreasing elevation from south to north which was caused by strong tectonic movements in Pliocene-early Pleistocene period. However,the local relief shows obvious characteristics of segmentation. The borders of these segments coincide with the segment border of the Longmenshan fault belt. The geomorphic feature along the northern section of the Longmenshan fault zone is mainly controlled by river erosion,whereas the local relief beside the Qingchuan fault is greatly impacted by tectonic movements. The local relief of the middle section is obviously controlled by the latest tectonic movements. However,in the southern section,the latest tectonic movements only control the area near the Xianshuihe fault. In addition,the local relief along the surface rupture zone of 2008 Wenchuan earthquake is consistent with the surface co-seismic displacement segmentation and regional deformation field. These data indicate that the tectonic movements since late Cenozoic are still reshaping the geographic and geomorphic characteristics nowadays.
Key wordsalpine grassland    crude protein    monitoring model    HJ-1A/1B    biomass
收稿日期: 2012-10-09      出版日期: 2013-10-21
:  TP75  
基金资助:国土资源部地质大调查项目(编号: 1212011120887)和国家自然科学基金项目(编号: 41004037)共同资助。
作者简介: 张微(1980- ),男,博士,高级工程师,主要从事遥感技术在矿产资源调查及新构造运动方面的应用研究,已发表论文60余篇。E-mail:zhangwei@agrs.cn。
引用本文:   
张微, 姚琪, 杨金中, 于浩, 吴建勇. 龙门山断裂带晚新生代以来分段活动的地形地貌表现[J]. 国土资源遥感, 2013, 25(4): 113-121.
ZHANG Wei, YAO Qi, YANG Jinzhong, YU Hao, WU Jianyong. Geomorphic characteristics of segmental activities of the Longmenshan fault zone since late Cenozoic. REMOTE SENSING FOR LAND & RESOURCES, 2013, 25(4): 113-121.
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https://www.gtzyyg.com/CN/10.6046/gtzyyg.2013.04.18      或      https://www.gtzyyg.com/CN/Y2013/V25/I4/113
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