宁镇,茅山山脉褶皱逆冲一推覆构造带的构造岩类型主要为碎裂岩系列,其次为糜棱岩系列。
The main type of tectonites in the belts of fold thrust - nappes in Ningzhen, Maoshan mountains is the cataclasite series, and then mylonite series.
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.
气管软骨中央带多见衰老的软骨细胞,并见明显核固缩、核碎裂等细胞凋亡形态学特征。
The senescent chondrocytes were distributed in the central zone where apoptotic morphological characteristics obviously appeared, such as pyknosis, karyorrhexis.
气管软骨中央带多见衰老的软骨细胞,并见明显核固缩、核碎裂等细胞凋亡形态学特征。
The senescent chondrocytes were distributed in the central zone where apoptotic morphological characteristics obviously appeared, such as pyknosis, karyorrhexis.
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