在侵入岩中的角闪石多呈长柱状晶体,但在某些花岗岩、花岗闪长岩中,角闪石的一向伸长的结晶习性并不显著。
Amphibole in the intrusive rock in a long columnar crystal, but in some granite, granodiorite, hornblende has elongated crystal habit is not significant.
中部为细小的胞晶和柱状晶;且晶体生长受结晶学各向异性影响。
The microstructure at the top and middle was the regular pine tree eutectic crystal and small cell and column crystal, respectively.
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