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自６０年代以来，国际上进行了许多大地地球物理研究，包括重力、地震测深和热流等，对高亚洲下部地壳和地幔的结构揭示出许多新现象。特别应该指出的是，在高亚洲，包括帕米尔—喜马拉雅地区、青藏高原，都反映出一组穿透地壳、错开莫霍面的高角度深断裂。但是，对这组深断裂的分析研究很不足。本文将对这组断裂进行讨论，辨认出它们是一组垂直的转换断层，命名为垂直转换断层（Ｖｅｒｔｉｃａｌｔｒａｎｓｆｏｒｍｆａｕｌｔｓ）。它们在高亚洲隆升和年青造山作用（Ｍｏｕｎｔｉａｎ－ｂｕｉｌｄｉｎｇ）方面具有独特的动力学作用。垂直转换断层在古老山带也应该有自己的位置和作用
Since the 1960s, many earth geophysical researches, including gravity, seismic sounding and heat flow, have been carried out internationally, revealing many new phenomena in the structure of the lower crust and mantle in the high Asia. In particular, it should be pointed out that in the high Asia, including the Pamir-Himalayas and the Tibetan Plateau, a group of high-angle deep faults that penetrate the crust and stagger the Moho are reflected. However, the analysis of deep fracture in this group is not enough. This article will discuss the group of faults and identify them as a set of vertical transition faults, termed Vertical Transform Faults. They have a unique kinetic role in the uplift of Asia and the Mountian-building. Vertical transformation fault in the ancient mountain should have its own position and role