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通过对东昆仑东段清水泉地区花岗岩类的详细野外研究，提出造山带地区岩浆岩中普遍存在构造混杂现象，并把构造混杂岩浆岩分为构造岩浆岩片和准构造岩浆岩片两类，为造山带地区侵入岩的研究提供了新思路。
Based on the detailed field study of the granitic rocks in the Qingshuiquan area in the eastern part of East Kunlun Mountains, it is proposed that there are widespread structural miscellaneous phenomena in the magmatic rocks in the orogenic belt, and the structural melange rocks are divided into tectonic magmatic rocks and quasi-structural magmatic rocks. The study of regional intrusive rock provides new ideas.