Planation Surfaces on the Tibet Plateau,China  

作　　者：ZHANG Xinbao HE Xiubin WANG Yangchun LONG Yi 

机构地区：[1]Institute of Mountain Hazards and Environment, CAS, Chengdu 610041, China [2]State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, GAS, Xi＇an 710075, China [3]Graduate University of the Chinese Academic of Sciences, Beijing 100039, China

出　　处：《Journal of Mountain Science》2008年第4期310-317,共8页山地科学学报（英文）

基　　金：supported by the National Natural Sciences Foundation of China(Grant Nos.40599421 and 90502002)

摘　　要：A planation hypothesis is proposed to explain landform evolution of the Tibet Plateau. A denudation threshold （T）, the maximum potential denudation rate for a certain type of rock, is introduced to explain the combined effects of lithology and tectonics on landform evolution. If the tectonic uplifting rate （U） is equal to or less than the threshold rate （U ≤ T）, the tectonic uplifting and terrain denudation are in dynamic equilibrium, and landforms are in a steady state. The end product should be planation surfaces whether the original landforms are flat plains or deeply dissected mountains. If U 〉 T, uplift and denudation are not able to reach a dynamic equilibrium state. The plateau surface is mostly underlain by soft rocks, such as the Mesozoic epimetamorphic argillites and Tertiary sedimentary rocks, while the mountain ranges comprise hard rocks, such as granite, gneiss and limestone. In soft rock regions, hills are low with a relative relief of mostly less than 100 m and the slopes are gentle at a gradient of 〈200. In contrast, hills can maintain steep slopes in hard rock regions. The Tibet Plateau has been under an equilibrium condition between tectonic uplifting and denudation except for the mountain ranges. The plateau might have reached the present altitudes before the Quaternary.

关 键 词：planation denudation threshold landform evolution Tibet Plateau China 

分 类 号：P942[天文地球—自然地理学]