甘肃冶金
甘肅冶金
감숙야금
Gansu Metallurgy
2015年
4期
94-95
,共2页
构造%热液%大理岩%花岗闪长岩%矽卡岩
構造%熱液%大理巖%花崗閃長巖%矽卡巖
구조%열액%대리암%화강섬장암%석잡암
structure%hydrothermal%marble%granodiorite%skarn
双井子铁铜矿位于塔里木板块东北缘马庄山弧后盆地,矿化体产于大理岩与花岗闪长岩接触带中,主要受北东向构造控制,具有热液型及矽卡岩型成矿特征.
雙井子鐵銅礦位于塔裏木闆塊東北緣馬莊山弧後盆地,礦化體產于大理巖與花崗閃長巖接觸帶中,主要受北東嚮構造控製,具有熱液型及矽卡巖型成礦特徵.
쌍정자철동광위우탑리목판괴동북연마장산호후분지,광화체산우대리암여화강섬장암접촉대중,주요수북동향구조공제,구유열액형급석잡암형성광특정.
The Shuangjingzi iron-copper deposit is located in Mazhuangshan arc basin in northeast margin of the Tarim plate.The mineralized bodies occurred in marble and granodiorite contact zone, mainly due to the northeast trend struct control, with hydrothermal and skarn rock type mineralization characteristics.
