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朱诺地区区域大地构造位置位于冈底斯—拉萨陆块,冈底斯晚燕山—喜马拉雅岩浆弧带二级构造单元内。区内发育石炭系、上侏罗统—白垩系、古近系及第四系地层;断裂构造较为发育;岩浆活动主要表现为大量中酸性复式岩体、岩株及岩脉。强烈的构造、岩浆活动为区内铜、金多金属成矿提供了有利条件。
The regional structure of the Juno area is located within the second-unit tectonic unit of the Gangdise-Lhasa block and the Late Yanshan-Himalayan magmatic arc of the Gangdese. The area is characterized by Carboniferous, Upper Jurassic-Cretaceous, Paleogene and Quaternary strata. The fault structure is well developed. Magmatic activity is mainly characterized by a large number of intermediate-acidic complex rock mass, rock mass and dikes. Strong tectonic and magmatic activities provide favorable conditions for copper and gold polymetallic mineralization in the area.