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本文简要介绍了现今山脉隆升历史研究方法的现状 ,指出可以利用同位素作为气候变化的指数 ,以气候变化为桥梁来推断山脉隆升历史。目前 ,该方法主要有两种发展趋势。笔者利用了该方法来推测青藏高原北缘山脉的隆升。结果显示 ,高原北缘山脉在渐新世和中新世早期都曾出现了快速隆升。
This paper briefly introduces the present research status of the up-dating of mountain uplifts and points out that we can make use of isotopes as indices of climate change and use the change of climate as a bridge to infer the uplift history of the mountains. At present, there are mainly two kinds of development trends of this method. The author uses this method to speculate the uplift of the northern margin of the Qinghai-Tibet Plateau. The results show that the northern margin of the plateau in the Oligocene and Early Miocene have had rapid uplift.