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，殘余的二疊紀構造層在盆地中表現為西南部殘余厚度大，東北部殘余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(chǎng)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。
