摘要
///The Yangshan gold deposit in Gansu Province, the largest gold deposit in China, lies in the Shaanxi- Gansu-Sichuan triangle area of the western Qinlin Orogen. Based on the field work, the authors carried out systematic microstructural researches on tectordtes of Anchanghe-Guanyinba fault zone, in the hope of reflecting the macroscopic structure by means of the microscopic structure. According to the research results, the authors hold that the transition of metamorphic facies in the fault zone was high greenschist facies→low greenschist facies→facies lower than greenschist facies from Middle-Late Triassic, whereas the deformation sequence being in order of ductile→ductile-britfle→brittle. The values of regional principal stress were changed from high to low and the regional principal stress orientation was SN compressional→NE compressional→NW and SN compressional.