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康古尔塔格金矿带是近几年新疆东天山境内发现的重要成矿带。以康古尔塔格─黄山断裂为一级板块边界，其南发育晚古生代岛弧系和巨型韧性剪切带，后者东西延伸数百km，强弱应变相间，分四期变形，第二、三期变形与金矿关系最为密切。晚古生代碰撞构造及其演化与金成矿亦具有重要的时空控制关系。碰撞花岗岩系列特征与成矿对应关系明显。成矿构造演化分三个阶段，提出了六条该区构造演化与成矿规律方面的认识，表明该带构造控矿和动力（变质）热液成矿均较明显。
Kanggurtag gold deposit is an important metallogenic belt discovered in eastern Tianshan, Xinjiang in recent years. With the Kanggutage-Huangshan fault as the first-level plate boundary, the Late Palaeozoic island arc system and giant ductile shear zone developed in the south, and the latter extended hundreds of km in east-west direction with strong- , The third phase of the deformation and gold most closely. Late Paleozoic collision structure and its evolution and gold mineralization also have important space-time control relationship. The characteristics of collisional granite series have obvious relationship with mineralization. The metallogenic tectonic evolution is divided into three stages and the understanding of tectonic evolution and metallogenic regularity in the six areas is proposed. It shows that the ore-controlling and dynamic metamorphic hydrothermal mineralization of the belt is obvious.