El placer lateral de playa Mejías (noreste de Cuba Oriental): un ejemplo de interacción de procesos aluviales y marinos en la concentración de minerales de elementos preciosos

Abstract

The playa Mejías lateral placer is the most important placer in Cuba. Its mineralogical composition (magnetite, chromite, rutile, ilmenite, orthopyroxene) reveals that the ophiolites of the Mayarí-Baracoa Belt are the main source area. However, other sources are demonstrated for by the presence of 4 different morphological types of zircon crystals, and minerals related to listvaenitic mineralizations (calcosilicates, carbonates). Also, precious metals have been recognized . Previous to their fluvial transport, electrum grains were depleted in gold in the lateritic environment, producing silve r-rich rims to the electrum grains. The gold particles were transported by rivers as fine-sized particles of electrum with various compositions, and as Au-amalgam. During their fluvial transport, the smaller gold grains coalesced to form larger grains, and a final generation of highly pure gold cemented the subgrains. Then, the particles were deposited in a beach lateral placer, where the grains were leached by sea water, giving rise to corrosion textures. The particles of EGP minerals found are grains of osmium-rich laurite replaced by laurite veins associated with symplectitic intergrowths of a third laurite generation (having intermediate compositions between the above laurite generation) and iridioarsenite, as a consequence of serpentinization at the source. Leaching by sea water produces a depletion in osmium in the particles.