The Geological Characteristics and Genetic Mechanism of Zhuan Shanzi Gold Deposit in Chi Feng, Inner Mongolia

摘要

On the basis of the field research and summarize the results of previous studies, this review summarizes systematically that ZhuanShanzi gold deposit is formed in the geological background, Such as tectonic background, the geochemical characteristics of the Granite rock mass and ore bodies, characteristics.And again, this review also puts on it that the space-time contacts among the mineral provenance,migration and positioning. Research shows that: since the early cretaceous, the edge of the North China carton mantle is thinning strongly, and caused a lot of alkali-calcium alkaline magma and become one of the regional metal metallogenic material sources and heat sources. Magmatic hydrothermal and ductile-brittle fracture is a necessary to form gold deposits. It Concludes Preliminarily that the deposit is related to ductile fracture and magmatic hydrothermal activity.