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Location: 51 km NE from Tacna, Peru
Jirón Giovanni Batista Lorenzo Bernini 149, Office 501 – A, San BorjaLimaPeru
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The Pucamarca mineralization is considered to be high sulphidation epithermal gold hosted in brecciated volcanics with associated vuggy silica alteration or silica – alunite alteration. The hydrothermal breccias at surface are characterized by abundant iron oxide cement within zones of silica – alunite alteration.
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