Jinbashan copper deposit is set in Heiyingshan area

Ejin Qi

Inner Mongolia

it is a little size Copper deposit of hydrothermal origin.Mining area is located in the middle of Jinbashan fold belt

orebody occur in secondary structure

the direction is same as main fault is NWW.In order to explore the cause of the ore deposit

I did a lot of work

just like field observations

petrology characteristics identification

geochemistry method and so on.This work has carried on the induction summary to the geological characteristics of ore deposit.Research results show that the area of fold and fault development

in the late hercynian magmatic activity is strong

structure and magma activity in composite is the key factors of the copper ore.These work can provide a basis for the next work of the copper deposit prospecting.