The ballas type grown at the transition to the graphitic deposition is characterized by a homogenous micro-twinned matrix.
在向石墨沉积转变中生成的半刚石种类的特征是均匀的显微孪晶基体。
The ballas type grown at the transition to the graphitic deposition is characterized by a homogenous micro-twinned matrix.
在向石墨沉积转变中生成的半刚石种类的特征是均匀的显微孪晶基体。
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