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通过推覆剪切热估算和花岗岩岩石学特征的研究，作者认为达拉布特地区的花岗岩岩体是由推覆剪切重熔形成的，并与齐求Ｉ号金矿床的形成有直接的关系
Based on the studies of the shear-heat estimation of the thrust and the petrological characteristics of the granites, the authors believe that the granitic rocks in the Darabut area were formed by shearing-remelting and are directly related to the formation of the Qi-Qiu-I gold deposit relationship