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High-Resolution Geochronology of the Coroccohuayco Porphyry-Skarn Deposit, Peru: A Rapid Product of the Incaic Orogeny

机译:秘鲁Coroccohuayco斑岩-斯卡恩矿床的高分辨率年代学:印相造山运动的快速产物

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摘要

Precise and accurate determination of the timing and duration of ore-forming processes in porphyry systems is a fundamental step in understanding their genesis and placing them in a regional context. Here, we take advantage of the considerable improvements in the field of geochronology over the last decade to provide a robust geochrouologic framework for hydrothermal and magmatic events in the Eocene Coroccohuayco porphyry-skarn Cu deposit, and the first robust dating of an ore system in the emerging Andahuaylas-Yauri batholith and metallogenic belt, southern Peru. This batholith and associated porphyry systems were emplaced during the Incaic orogeny, in a context of slab flattening, compression, exhumation, uplift, and the initiation of the bending of the Bolivian orocline.
机译:准确,准确地确定斑岩系统中成矿过程的时间和持续时间,是了解其成因并将其置于地区背景中的基本步骤。在这里,我们利用过去十年在地质年代学领域的重大改进,为始新世Coroccohuayco斑岩-矽卡岩型铜矿床的热液和岩浆事件提供了可靠的地质学框架,并为该系统中的矿石系统进行了首次可靠的定年。秘鲁南部新兴的Andahuaylas-Yauri基岩和成矿带。在印加造山运动中,该板岩层和相关的斑岩系统在平板展平,压缩,发掘,隆起和玻利奥海床斜线弯曲开始的背景下被放置。

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