The Shengliqiao pluton in the western Kunlun Mountains is a composite batholith.
论证了西昆仑地区的胜利桥岩体是一个复式岩基。
Lincang granite intrusive body is a composite batholith formed by polyphasic intrusion, whose main rock type is the biotite adamellite.
临沧花岗岩侵入体是一个多期次侵入活动所形成的复式岩基，其主要岩石类型为黑云母二长花岗岩。
Deferent plutons composing Linglong composite granitoid batholith have deferent degrees of anisotropy of magnetic susceptibility.
组成玲珑花岗岩基的各个岩体具有不同的磁化率各向异性度。
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