西藏昌都玉曲河源区冰川构造的性质、特征与演化
The nature， characteristics and evolution of glaciotectonics in source area of the Yuqu River， Changdu， Tibet， China
西藏昌都玉曲河源区冰川构造的性质、特征与演化 |
| 李德文, 马保起, 田勤俭, 史嘉骥, 赵杰 |
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The nature， characteristics and evolution of glaciotectonics in source area of the Yuqu River， Changdu， Tibet， China |
| Dewen LI, Baoqi MA, Qinjian TIAN, Jiaji SHI, Jie ZHAO |
| 图2 冰川构造地貌与典型剖面分布图（背景图层为在Landsat OLI影像上叠置的EarthData DEM数据。实心圆点为主要考察点。箭头代表冰川构造指示的不同时期运动方向，其中紫色实线小箭头为C1层，黄色虚线粗箭头为C2层，细节见正文） |
| Fig. 2 Glaciotectonic landform and typical profile distribution （The background is overlaid EarthData DEM data on the Landset 8 OLI images. The solid dots are the main observation points. The arrows represent the movement directions indicated by the glaciotectonics. The small arrowss with purple solid lines are C1 layers， and the thick arrows with yellow dotted lines are C2 layers. Details in the text） |
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