Mechanisms of reaction-enhanced deformability in minerals and rocks
Mechanisms of reaction-enhanced deformability in minerals and rocks
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矿物和岩石的反应增强变形机制
DOI：
10.1007/978-94-011-6827-4_11
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发表时间：
1990
期刊：
影响因子：
--
通讯作者：
D. Rubie
中科院分区：
文献类型：
--
作者：
D. Rubie
我们目前对岩石和矿物的变形机制以及这些材料的流变学的理解主要是通过对单晶和单矿物集合体的实验研究获得的。这些研究对于基本了解岩石变形的基本过程是必不可少的。然而，地壳和地幔的岩石很少是单矿物的，因此，为了现实地研究地球的变形过程，有必要对更复杂的多相聚集体进行实验（例如Tullis，本卷）。
Our current understanding of deformation mechanisms in rocks and minerals and the rheology of these materials has been obtained largely through experimental studies of single crystals and monomineralic aggregates. Such studies are essential in obtaining a basic understanding of the fundamental processes of rock deformation. However, rocks of the Earth’s crust and mantle are seldom monomineralic and, therefore, to investigate deformation processes in the Earth realistically it is necessary to perform experiments on more complicated multi-phase aggregates (e.g. Tullis, this volume).