1、The Fangshan granodiorite pluton of Lower Cretaceous occupies the middle of core.
核部有強(qiáng)力侵位的早白堊世的房山花崗閃長巖株。

2、The Shengliqiao pluton in the western Kunlun Mountains is a composite batholith.
論證了西昆侖地區(qū)的勝利橋巖體是一個(gè)復(fù)式巖基。

3、The Shuanghe pluton is S-type granite and formed in the zone of the intercontinental collision.
雙合巖體形成于板塊碰撞同期，屬S型花崗巖；