秘鲁斑岩铜矿带遥感构造解译与成矿特征
Remote Sensing Interpretation of Structures and Metallogenic Features of Porphyry Copper Belt in Peru
DOI: 10.12677/AG.2015.51001, PDF, HTML, XML, 下载: 2,775  浏览: 7,687 
作者: 苏学沛, 高明光：中南大学，地球科学与信息物理学院，湖南 长沙
关键词: 秘鲁；斑岩铜矿；矿床特征；成矿条件；遥感解译；构造；Peru； Porphyry Coppers； Deposit Features； Metallogenic Conditions； Remote Sensing Interpretation； Structures
摘要: 秘鲁地处南美安第斯山脉中段，由于受纳兹卡板块长期向南美板块下部俯冲作用的影响，成矿条件十分优越。秘鲁大型铜矿相对集中，本文通过收集和整理相关文献以及实地考察，结合遥感构造解译，探讨与总结该成矿带的典型斑岩矿床的矿床特征与成矿条件，并提出了找矿方向。
Abstract: Peru, located at the central Andes, have developed favorable minerogenetic condition, due to the subduction of Nazca plate beneath the South American plate. Large copper mine in Peru is rela-tively concentrated. In this paper, we first review related literatures. Then through remote sensing interpretation, we systematically discuss deposit features and metallogenic conditions of the typical porphyry deposits, and further provide new exploring direction.
文章引用：苏学沛, 高明光. 秘鲁斑岩铜矿带遥感构造解译与成矿特征[J]. 地球科学前沿, 2015, 5(1): 1-11. http://dx.doi.org/10.12677/AG.2015.51001

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