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青藏高原第四纪大陆冰盖对高原隆升的影响
引用本文:郑英龙,韩同林.青藏高原第四纪大陆冰盖对高原隆升的影响[J].现代地质,1992,6(2):201-208.
作者姓名:郑英龙  韩同林
作者单位:中国地质科学院地质力学研究所 (郑英龙),中国地质科学院地质研究所(韩同林)
摘    要:本文依据在青藏高原存在第四纪大陆冰盖的基础上,给定了3个不同厚度的冰盖,应用弹性板模式模拟计算了大陆冰盖消融前后的地壳均衡过程。计算结果表明,由大陆冰盖消融可能引起的高原隆升最大不超过700m。因此,就整个高原的隆升幅度来说可忽略其影响。但由于冰川消融前后高原负荷发生了变化,导致了隆升速度的相应变化,因而引起地表侵蚀强弱程度的不同及其它一些地质现象是不能忽视的。

关 键 词:青藏高原  大陆冰盖  均衡

THE EFFECTS OF THE QUATERNARY CONTINENTAL GLACIAL SHEET IN QINGHAI-XIZANG PLATEAU UPON THE UPLIFT OF THE PLATEAU
Zheng Yinglong Han Tonglin.THE EFFECTS OF THE QUATERNARY CONTINENTAL GLACIAL SHEET IN QINGHAI-XIZANG PLATEAU UPON THE UPLIFT OF THE PLATEAU[J].Geoscience——Journal of Graduate School,China University of Geosciences,1992,6(2):201-208.
Authors:Zheng Yinglong Han Tonglin
Abstract:Under the premise of the fact that the Quaternary continental sheet existed in Qinghai - Xizang plateau. based on the elastic plate model, the author, considering the three sorts of the thickness of the glacial sheet, calculates the subsidence and uplift of the plateau caused by them. It has been shown that the maximum of the uplift of the plateau brought about by the thawing of the continental sheet is no more than 700 meters. There- fore, as the uplift of the whole plateau has been concerned, we can ignore the effects of the glacial sheet upon the uplift of the plateau, However, we cannot ignore some phenom- ena (for example, the changes of the crustal erosive intensities) because of the changes of the uplift velocities caused by the glacial thawing.
Keywords:Qinghai-Xizang plateau  continental glacial sheet  isostasy
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