Geological characteristics and genesis of polymetallic deposits in the Longfengshan area of Shangzhou District,Shangluo City
The polymetallic deposit in the Longfengshan area of Shangzhou District is located about 20km southwest of the urban area,with an area of 75.98km2.The exploration area is located in the Shangdan Kalidong junction zone,where the Shahewan and Caoping rock masses are sandwiched between the ore bearing strata of the Zhashan area,such as the Chigou Formation,Qingshiya Formation,and Danfeng Group.Fault structures are developed,providing channels and storage space for mineralization and ore migration.Multiple periods of magmatic activity provide dynamic conditions for mineralization;Based on the geological characteristics,ore controlling factors,and symbiotic combinations of ore-forming elements in the work area,it is believed that the genesis type of the deposit in this area belongs to the magmatic tectonic hydrothermal vein type polymetallic deposit.This article mainly analyzes and discusses the geological characteristics of the exploration area,studies the genesis of its mineral deposits,and hopes to provide some reference and reference for future mineral exploration work.
Longfeng MountainPolymetallic depositsGeological characteristicsOrigin of mineral depositsShangzhou District,Shangluo City
万方数据
维普
