Abstract
Based on the study of geological conditions in Lianmuqin area, Turpan-Hami Basin, the structural characteristics of upper Shanshan Group, upper Sandili Dadun Formation, and the top of Kalaza Formation from the bottom to the bottom in the study area are analyzed. According to the structural morphological characteristics of the fault interpretation, comprehensive description of the size and length of the fault, the new fault interpretation. The interpretation process is more logical under the guidance of sedimentary and tectonic theories.
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