中生代中酸性脉岩为成矿期脉岩,且与黄泥河花岗岩岩基有着密切的成因联系。
Mesozoic intermediate and acidic dykes which are closely related to Huangnihe granite were formed during the mineralization period.
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。
Deferent plutons composing Linglong composite granitoid batholith have deferent degrees of anisotropy of magnetic susceptibility.
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。
Lincang granite intrusive body is a composite batholith formed by polyphasic intrusion, whose main rock type is the biotite adamellite.
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