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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Adakite岩浆有关的斑岩型矿床:以蒙古斑岩型Cu-Au和Cu-Mo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:斑岩型主要矿床在空间和时间上与阿达克质岩浆有关。这些岩浆表现出较高的Sr / Y,较高的Al 2 O 3 和较高的La / Yb地球化学特征。泥盆纪晚生Oyu Tolgoi和石炭纪Shuteen矿床的案例研究表明,斑岩状的Cu-Au与氧化的,高Sr / Y镁铁质中度岩浆岩浆有关。与Erdenet和Bayan Uul斑岩型Cu-Mo矿床有关的岩浆通过分馏,地壳熔融和同化作用的组合显示出较高的Sr / Y特征。长寿命岩浆热液系统对大型斑岩矿床具有潜力。

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