Abstract:Jasperoid, a microcrystalline silica rock, occurs along the crest of the Magdalena Mountains and along the west-facing dip slope. It is the focus of this study because in similar settings in Nevada it is associated with economically important deposits of very fine grained gold. In the Magdalenas, jasperoid extensively replaces the Mississippian Kelly Limestone. Mineralogy displays strongly oxidized pyrite with internal zones of silver and copper sulfides; galena and sphalerite follow pyrite in the paragenesis.… Show more
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