斜长石通常呈白色,具有完全解理和聚片双晶。
Plagioclase is usually white-colored with perfect cleavage and albite twins .
透辉石有两个方向的完全解理,通常为孪晶生成,短且成圆柱形,断口参差不平。
Diopside crystals have a perfect cleavage in two directions , are often twinned and are short and columnar , but with an uneven fracture .