日龙色加侵入体位于雀儿山侵入体西南翼,岩性为中细粒花岗闪长岩。岩石主要由钾长石、斜长石、石英以及黑云母和角闪石组成。岩石具有典型的中钾钙碱性岩浆岩特征。龙色加侵入岩体显示花岗闪长岩为板块碰撞前的I型花岗岩特征,反映其来源于地壳重熔,其侵入时代为印支晚期。 The Azuron plus intrusions are located in the southwestern wing of the Queer Shan intrusive body and are lithic fine-grained granodiorites. The rock consists mainly of potash feldspar, plagioclase, quartz and biotite and amphibole. Rock has the typical characteristics of calc-alkaline magmatic rocks. The Longsheng plus intrusive rock shows that the granodiorite is a type I granite before the plate collision, reflecting that it originated from the remelting of the crust. The age of its invasion was the late Indosinian.