在扁平的半刚石中，D带较小，而石墨峰比粗大的半刚石中的要大。
In flat ballas the D-band is smaller and the graphite peak larger than in coarse ballas.
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.
通过改变沉积条件，发现了几种形貌的半刚石结构，即具有多面的半刚石、平整的半刚石和含石墨杂质的半刚石等等。
Several morphological ballas structures have been observed by varying the deposition conditions, i. e. ballas having faceted areas, flat ballas, ballas with graphitic inclusions, etc.
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