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Porphyry type deposits associated with adakite magmas: Case study of porphyry Cu-Au and Cu-Mo deposits in mongolia

机译:与埃达克岩岩浆有关的斑岩型矿床——以蒙古斑岩型铜金和铜钼矿床为例

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Major porphyry type deposits are spatially and temporally associated with adakitic magmas. Such magmas show high Sr/Y, high Al2O3, and high La/Yb geochemical signature. Case study of late Devonian Oyu Tolgoi and Carboniferous Shuteen deposits show that porphyry Cu-Au are associated with oxidized, high Sr/Y mafic-inermediate adakitic magma. Magma associated with Erdenet and Bayan Uul porphyry Cu-Mo deposits has shown high Sr/Y signature through a combination of fractionation, crustal melting and assimilation. Long-lived magmatic-hydrothermal system is potential for large porphyry deposits.
机译:主要斑岩型矿床在空间和时间上与埃达克岩浆有关。这些岩浆显示出高Sr/Y、高Al2O3、高La/Yb的地球化学特征。晚泥盆世Oyu Tolgoi和石炭纪Shuteen矿床的案例研究表明,斑岩Cu-Au与氧化的、高Sr/Y镁铁质矿物介导的埃达克岩浆有关。与Erdenet和巴彦Uul斑岩铜钼矿床相关的岩浆通过分馏、地壳熔融和同化的组合显示出高Sr/Y特征。长寿命岩浆热液系统是大型斑岩矿床的潜力所在。

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