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华北克拉通固结时间较晚，活动性较强，金矿床赋矿围岩以中深变质的镁铁质岩石和花岗岩类岩石为主，大规模金矿床一般产在韧、脆性剪切叠加的构造带中，成矿时代在１８８～４６Ｍａ之间．西澳克拉通固结较早，稳定性较好，金矿床主要产在太古宙花岗岩－绿岩地体中，一般产在韧－脆性剪切过渡带或叠加的构造带中，金矿化年龄在２６４０～２６００Ｍａ之间．华北克拉通金矿床比西澳金矿床形成晚，受剥蚀程度低，许多矿床尚未出露地表，在深部寻找盲矿体前景可观．
The consolidation time of North China Craton is relatively late with high activity. The ore-hosting rocks in the gold deposits are dominated by mid-metamorphic mafic rocks and granitic rocks, and the large-scale gold deposits are generally superimposed on the ductile and brittle shear strata Tectonic belt, the mineralization age between 188 ~ 46Ma. Western Australia Craton early consolidation, stability is good, the gold deposit is mainly produced in the Archean granite - greenstone, generally produced in the ductile - brittle shear transition zone or superimposed structural belt, gold mineralization age Between 2640 ~ 2600Ma. The North China Craton gold deposit was formed later than the Western Australia gold deposit, with a low degree of denudation. Many deposits have not been exposed to the surface and the prospect of finding a blind ore body in the deep is considerable.