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随着板块构造学说的问世和发展,混杂地质体愈来愈引起构造地质学者的浓厚兴趣,因为它是古俯冲带或缝合带的主要标志之一。最早研究混杂地质体的当推Griesbash、Diener 和Middlemiss(1883),Kaufmann(1886)在描述阿尔卑斯复理石中的杂乱堆积物时,启用了“野复理石”(Wildflysch),Greenly(1919)首次将“melange”一词引入混杂地质体的研究中,Flores(1955)提出了滑混堆积(Olistostrome)的概念。板块构造学说问世以后,许靖华(1968)把混杂体的成因和板块的俯冲有机地结合起来。A.L.Knipper(1971)和甘塞尔(1974)先后提出了蛇纹混杂体(Serpentinite melan-ge)和蛇绿混杂体(Ophiolitic melange)的概念。
With the advent and development of plate tectonics, mixed geology has increasingly attracted the attention of structural geologists because it is one of the major symbols of ancient subduction or suture. The earliest studies of mixed geologic bodies enabled Wildflysch, Greenly (1919), and Karl Marx (1883) to describe the messy deposits in Alpine flysch by Griesbash, Diener, and Middlemiss (1883) For the first time, the word “melange” was introduced into the study of mixed geology. Flores (1955) proposed the concept of Olistostrome. After the theory of plate tectonics came out, Xu Jinghua (1968) organically combined the genesis of the mixed body with the subduction of the plate. The concepts of Serpentinite melan-ge and Ophiolitic melange have been proposed by A.L. Knipper (1971) and Gansel (1974).