Granitoid intrusions are received to have the potential to offer metal elements when mineralized by the analyses of ore-controlling factors.
控矿因素分析表明该区花岗岩类侵入体具有提供成矿金属的潜力。
The most important metallogenic granitoid intrusions are mainly formed in Mesozoic, secondly late Variscan period.
已知成矿的花岗岩类侵入体主要为中生代岩体,其次为晚古生代华力西期岩体。
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