中文摘要：

近一个世纪以来，关于冰川成因主流的一种理论是冰川发育的构造-气候耦合模式，为了研究构造活动在冰川发育中的作用，选取构造活跃的岷山雪宝顶（5588m）-九寨沟为研究区，以DEM数据为基础材料，结合ArcGIS的地图处理软件ArcMap分析技术，采用面积-高程积分方法对雪宝顶地区、九寨沟地区和岷江西侧的地貌形态特征进行分析。研究结果显示：雪宝顶地区、九寨沟地区和岷江西侧面积-高程积分（HI）分别为0．54、0．46和0．39；面积-高程积分曲线均呈S型形态但逐渐变凹，反应3个区域构造活动特征。地貌演化阶段均属于壮年期，但雪宝顶地区靠近幼年期，岷江西侧接近老年期，反应区域先后抬升或者抬升的幅度依次减小。3个地区1810个板块的HI值呈现出明显的区域分异，显示冰川作用和岩性差异对局部面积-高程积分值的大小的影响。研究区的冰川发育与构造作用密切相关。

英文摘要：

In almost a century, the mainstream theory about glacier development is the coupling effect of uplift and climate model. In order to study the tectonic effect on glacier growth, we select the Xuebaoding-Jiuzhaigou area of Min Shan within an active tectonic movement region （32°23′- 33°18′N, 102°56′- 104°25′E） located in the northeastern Tibetan Plateau. The summit of the study area is Xuebaoding peak with the height of 5588m. Three active faults dominate the regional tectonic movement including two north-south extend named Minjiang Fault and Huya Fault as well as one west-east stretch known as Xueshan Fault, which divide the entire area into three parts called Xuebaoding area, Jiuzhaigou area and the westside of Minjiang. Based on Digital Elevation Model （DEM） data, combined with GIS spatial analysis technology, we adopt Hypsometric Integral method to analysis the geomorphology feathers of the study area. The result indicate Hypsometric Integral （HI） value of Xuebaoding, Jiuzhaigou and the westside of Minjiang are 0.54, 0.46 and 0.39 respectively, representing the geomorphology evolution of the three area in the state of maturity but becoming older. The type of Hypsometric Integral curve for the three areas is all near S but with the trend of become concave from Xuebaoding to the westside of Minjiang. In view of tectonic background and topography profile analysis, we find they have highly consistent and agree well with HI value together with Hypsometric Integral curve, which reflects structure activity from Xuebaoding to the westside of Minjiang become weaker. Tectonic play significant role in controlling geomorphology evolution. To study whether lithology and glaciation impact on HI value, we further divide Xuebaoding, Jiuzhaigou and the westside of Minjiang into 472, 465 and 873 parts respectively. And then calculate HI value for the whole 1810 parts. The result shows regional differentiation for the HI value. That is the more hard rock corresponding to the bigger HI value, and the strong