Carboniferous tectonic-magmatic-hydrothermal related Au-Cu-Cr-Ni metallogenic series in Khabir, Elaine.

Khabir Ga structural belt in Yili is a residual trough located at the edge of Yili micro-block, in which Devonian-Carboniferous ophiolite melange, pyroclastic rock, clastic rock and siliceous rock are deposited. Carboniferous tectonic-magmatic activity was obvious, accompanied by hydrothermal mineralization, forming a gold-copper-chromium-nickel metallogenic series. The most prominent in this series is the gold and copper mineralization related to tectonic-magmatic-hydrothermal process in Tingeda Bay-Chahansala area. This sub-series is located at the northwest end of the Ga arc-groove belt in Khabir, and belongs to a part of the Ga gold-copper belt in Yilian Khabir. Many mineralization points such as iron, copper, nickel, lead, zinc, molybdenum, tungsten, gold and 10 have been found in this area. The deposit type is mainly magmatic hydrothermal gold-copper deposit. The representative deposits are Chahansala magmatic hydrothermal gold deposit and Dawan gold deposit in Tingel. The gold deposits (spots) in this area are mainly produced in tuffaceous siltstone of the Upper Carboniferous Qiergutao Formation, which is closely related to the NE-trending and nearly EW-trending fault structures, and the space of intermediate-acid rock bundles and dikes. Chahansala gold deposit is adjacent to the north side of Chahansala fault, and occurs in fine-grained diorite vein invading tuffaceous siltstone of Qiergutao Formation, which is closely related to faults and diorite veins distributed in the near east-west direction.