FIRST OCCURRENCE OF SILVER, GOLD AND PLATINUM IN THE YUCATÁN
Powder X-ray diffraction (XRD) indicates the orange-red lithology is dominated by a matrix of poorly crystalline serpentine and boehmite. Discrete crystals of chromium-bearing magnetite and zircon occur in the orange-red lithology as well. Scanning Electron Microscope (SEM) investigation of the lithology indicates that silver (Ag) particles are common, and lesser amounts of gold (Au) and platinum (Pt) occur. Ag occurs both in the orange-red lithology and in the adjacent limestone. Ag particles are of high purity with a few analyses having trace amounts of sulfur. The Ag particles are commonly platy and crystals up to approximately 30 microns in diameters occur, but crystals 1-5 micrometers are more abundant. Au occurs in both diffuse textures and with crystals up to 15 microns. Pt crystals are commonly less than 0.1 micrometers in diameter.
The assemblage of serpentine minerals, boehmite, Cr-bearing magnetite and zircon are consistent with a hydrothermally altered mafic igneous source material for the orange-red lithology. The occurrence of Ag, Au, and Pt are also consistent with a mafic origin however, the age and origin of the igneous source material is unclear. The Ag in the limestone is interpreted as a result of a dissolution-reprecipitation process. Although not of economic grade, our results indicate there may be tentative cause for future exploration.