Crustal structure and fluid or melt originating in the deep crust mantle are critical regional magmatic mineral systems. However, crustal processes that entrain focus fluids from a deep-source region to metallogenic belt remain relatively undisclosed. We present magnetotelluric (MT) study of eastern Qimantagh Metallogenic Belt (QMB) northern Tibetan Plateau. Data 33 MT stations two sections 7 d...
