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喜马拉雅地区强烈的地质构造运动为珠峰保护区构建了大尺度的地貌格局,形成了以高喜马拉雅山脉和藏南分水岭为骨架,高原湖盆和宽谷为基底,冰川、河流、湖泊、沙漠等并存的多种地貌形态。由于喜马拉雅山脉的阻挡作用,保护区内的气候在水平方向上产生了明显的区域分异,在7000米左右的垂直幅度上,出现了从热带、亚热带到寒带之间
The strong geological tectonic movement in the Himalayas has built a large-scale geomorphological pattern for the Everest Preserved Area and has formed a framework of high Himalayas and South Tibet watersheds, basal plateau lakes and valleys, glaciers, rivers, lakes and deserts A variety of morphological coexistence. Due to the blocking effect of the Himalayas, the climate in the reserve has obvious horizontal differentiation in the horizontal direction. From the tropical and subtropical zones to the cold zone