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干旱区地理 ›› 1991, Vol. 14 ›› Issue (1): 32-37.doi: 10.13826/j.cnki.cn65-1103/x.1991.01.006

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阿尔泰山风化作用的初步研究

叶玮   

  1. 中国科学院新疆地理研究所
  • 出版日期:1991-03-25 发布日期:2025-12-25

A PRELIMINARY STUDY ON WEATHERING PROCESS OFALTAI MOUNTAIN

Ye Wei   

  1. Xinjiang Institute of Geography, Academia Sinica
  • Published:1991-03-25 Online:2025-12-25

摘要: 阿尔泰山的风化作用分为两类,即以化学风化作用为主的古风化阶段和风化作用随山体高度变化发生分异的现代风化阶段。占风化作用深入而持久,成了广泛分布而具有不同色彩的古风化壳和氧化带,是寻找原生矿的重要标志。现代风化作用类型复杂而多样,它们对找矿具有指导意义。

关键词: 风化作用, 古风化壳, 阿尔泰山

Abstract: According to the primary research, the weathering process of Altai Mountain is divided into two stages.Before the Neogene period, chemical weathering was prevailing and formed residiums which are mainly composed of clay. It is important to form the placer.After that period, the environment had changed a great deal and weathering process became complex. both processes have played a different part in forming the placers.Needless to say, the careful investigation on weathering process will be helpful to find out a variety of placers in this region.