Analysis on Geological Characteristics and Prospecting Prospects of Wujiaying Silver Polymetallic Deposit in Fengning County
The Wujiaying silver polymetallic deposit in Fengning manchu autonomous county(referred to as Fengning county)is located in the middle section of the Inner Mongolia axis on the northern edge of the North China platform,and the regional fault tectonic activity and Yanshanian magmatic hydrothermal activity are frequent,and the formed silver-lead-zinc deposits are widely distributed.A total of 7 altered mineralization bodies and 7 Cu,Pb,Ag polymetallic ore bodies have been delineated in the mining area,and the ore bodies are mainly distributed in a vein like manner in the porphyry diorite,mostly parallel to the northwest.The genetic type of the deposit is a tectonic controlled medium to low temperature hydrothermal deposit related to the late Yanshan intermediate acidic intrusive rocks.Taking the Wujiaying silver polymetallic deposit in Fengning county as an example,combined with the regional geological background and geological characteristics of the deposit,the genesis of the deposit is analyzed,in order to guide subsequent exploration work.Research suggests that there may be large vein like ore bodies in the deep part of the study area,which has certain prospecting prospects.
silver polymetallic depositgeological characteristicsprospecting prospectsFengning county