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发现了3条蛇绿混杂岩带,并以此对本区的构造地层单元进行了合理的划分。在碎石山、拜惹布错一带发现了较为典型的蛇绿混杂岩,从而为西金乌兰-金沙江结合带的西延提供了有力的佐证。认为库牙克断裂与阿尔金断裂为同一条断裂,并首次提出库牙克断裂的断距约80km。在原侏罗系雁石坪群中发现了大量二叠纪化石,为地层的正确划分提供了依据。
Three ophiolitic melange zones have been found, and the tectonic stratigraphy units in this area have been reasonably divided. The more typical ophiolitic melanges were found in the areas of the rock fragments and the Baijasbu fault so as to provide strong evidence for the westward extension of the Xijinwulan-Jinshajiang united belt. It is considered that the Kuyakeke fault and the Altyn Tagh fault are the same fault, and for the first time, the fault distance of the Kuyakeke fault is about 80km. A large number of Permian fossils have been found in the Yanshiping Group of the original Jurassic, providing a basis for the correct division of strata.