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Geochemical Characteristics of Intrusive Rocks, Southeastern Mindanao, Philippines: Implication to Metallogenesis of Porphyry Copper-gold Deposits

机译:菲律宾棉兰老岛东南部侵入岩的地球化学特征:对斑岩型铜金矿的成矿意义

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摘要

This paper describes petrologic and geochemical characteristics of intrusive rocks associated with porphyry copper deposits in south-eastern Mindanao, the Philippines, where the Kingking deposit is located. Intrusive rocks at the Kingking deposit, are classified into biotite-bearing diorite porphyry, hornblende diorite porphyry and diorite porphyry. Intrusive rocks in other areas in south-eastern Mindanao, including Batoto, Bukal, Maragusan, Masara, Amacan and Sumlog, are hornblende diorite porphyry and hornblende quartz diorite. They are adakitic in Sr/Y-Y diagram, but not in La/Yb-Yb diagram due to relatively low REE contents. The magmas are oxidizing as suggested by the high X_(Mg) of mafic silicate phenocrysts and SO_3 contents of micro-phenocrystic apatite. An Oligocene-Miocene diorite intrusive complex formed by calc-alkaline, hydrous, oxidizing magma is considered to be associated with porphyry-type copper-gold mineralization.
机译:本文描述了金刚金矿床所在的菲律宾棉兰老岛东南部与斑岩铜矿床有关的侵入岩的岩石学和地球化学特征。 Kingking矿床的侵入岩分为含黑云母的闪长斑岩,角闪闪长闪长斑岩和闪长斑岩。棉兰老岛东南部其他地区的侵入性岩石,包括角闪闪闪长闪闪岩斑岩和角闪闪闪闪发光的石英闪闪岩,包括巴图托,布卡尔,马拉古桑,马萨拉,阿马坎和苏姆洛格。由于稀土元素含量较低,它们在Sr / Y-Y图中呈胺状,但在La / Yb-Yb图中呈胺状。如镁铁质硅酸盐隐晶石的高X_(Mg)和微隐晶磷灰石的SO_3含量所暗示的,岩浆正在氧化。由钙碱性,含水,氧化岩浆形成的渐新世-中新世闪长岩侵入复合体被认为与斑岩型铜金矿化有关。

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