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Mineralization is present in quartz veins and stockwork or breccia with disseminated pyrite.
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The Tropico breccia is hosted within finely bedded siltstones and dirty limestones, interpreted to be part of the Proaño group which hosts the major Fresnillo deposits.
The upper zone of copper mineralization encountered within ST23-03 is a 48.6m thick interval of strong breccia and vein-style copper sulfides grading 3% Cu, with broad zones of semi-massive to massive sulfide from 34.4m downhole.