The conclusions show that the Permian deposition is in possession of characteristic of wide-folding and reverse faults after undergoing multiphase tectonic activity. 在遭受多期構造疊加改造后，殘餘的二疊紀構造層在盆地中表現為西南部殘餘厚度大，東北部殘餘厚度小的現今構造格局。
The early Yanshanian regional tectonic stress field played an important role in the formation and evolution of these faults and gold metallogenesis. 早燕山期構造應力場對這些斷裂的形成演化與金礦的成礦作用有重要的控制意義。
