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一、前言地貭体經受塑性变形的現象在自然界里可謂触目皆是,最明显的是各式各样的褶皺和挠曲現象。因此闡明地貭体的塑性变形的程度和方式等等,在地貭学上具有重要意义。个九世紀末期,这个問題引起了許多地貭学家的重視,他們一方面从事于野外地貭現象的观察,同时也开始了室內的实驗工作。1867年,列鳥希(Reusch)首次报导了岩盐晶体的塑性变形情况。稍后,O.繆格(Mugge,1883、1889、1901、1920)发表了一系列矿物的实驗变形的資料。岩石的实驗变形工作开展稍迟一些,最初从事这方面工作的是亚
First, the preface to the phenomenon of body deformation under plastic deformation can be described as striking in nature, the most obvious is a wide range of wrinkles and flexing phenomenon. Therefore, it is of great significance in geography to clarify the extent and manner of plastic deformation in geoducks. At the end of the 9th century, this problem attracted the attention of many gensologists who were engaged in the observation of the phenomenon of wild land and the experiment of indoors. In 1867, Reusch first reported the plastic deformation of rock salt crystals. Later, Mugge (1883, 1889, 1901, 1920) published a series of experimental data on the deformation of minerals. Experimental rock deformation experiment carried out a little later, initially engaged in this area is Asia