断层岩在平面上分带特征明显,可划分为碎裂岩-节理密集带,磨砾岩-剪切旋转带和断层泥-局部压溶带等三个带。
The fault exists obviously in three bands: cataclasite concentrated joint band, worn braciation shearing rotation band and gouge partial pressure solution band.
对低碳钢板材进行表面球磨处理,利用电子显微术研究剪切变形方式下深度方向的组织演变。
A low carbon steel was treated by means of ball milling, and the shear-stress induced microstructural evolution along the depth was examined by using electron microscopy.
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