The paper systematically illustrates the tectoniclithofacies condition, metallotectonic framework after Meso-cenozoic era, regional metallotectonic evolution, metallogenic regularity and patter of the gold deposit formation, mainly probes into the correlation between regional tectonic evolution and metallogenic regularity. It consides that the intercontinental orogenic tectonic movement, which had been taken place at Yanshan age of post-indosinian orogeny in great extent way, is the key factor to result in metallization and ore-forming of this metallotectonic belt. The research shows that it is important to guide the exploration of gold deposit with the view of tectonic disturbance in this region, it is a significant role to find the new hidden ore deposit and to make the metellogenic prognosis further.