秘鲁东南部Andahuaylas-Yauri基岩斑岩-夕卡岩型铜-钼-金矿床的年代学和铅同位素新数据

Jorge Acosta, C. Heo, Eder Villarreal, Synthia Yauli, C. Salazar, Seok-Jun Yang, M. Ortega, Braulio Zorrilla
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引用次数: 1

摘要

报道了秘鲁东南部阿普里马克省附近的Trapiche和Constancia地区Cu-Mo-Au矿床的U-Pb、Re-Os年代学资料和铅同位素分析。测量的年龄是先前报道的成矿年龄在28 ~ 33 Ma之间的第一个区域脉冲。铅同位素结果表明,成矿有两个来源。第一种源被认为来自上地壳,第二种源被认为来自上地壳和下地壳的混合物。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
New Geochronological and Lead Isotopic Data for Porphyry-Skarn Cu-Mo-Au Deposits in the Andahuaylas-Yauri Batholith, Southeastern Part of Peru
New geochronological data of U-Pb, Re-Os and the lead isotope analysis of the Cu-Mo-Au mineral deposits are reported in the Trapiche and Constancia around Apurimac province, southeastern part of Peru. The measured ages were the first regional pulse of previously reported mineralization age between 28 and 33 Ma. The lead isotopic results indicate two sources of mineralization. The first source is thought to be derived from the upper crust and the second one is thought to be derived from a mixture of the upper crust and the lower crust.
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