Resumen

OBANDO-ACUNA, Luis G.  y  MURILLO-MAIKUT, Stephanie. Yugawaralite (zeolite) occurrence in Copey de Dota, Costa Rica. Rev. Geol. Amér. Central [online]. 2019, n.61, pp.121-130. ISSN 0256-7024.  http://dx.doi.org/10.15517/rgac.v61i0.40091.

Yugawaralite (Ca(Al2Si6)O16·4H2O) is reported for the first time in Costa Rica in the area of Copey de Dota. Yugawaralite belongs to the zeolite group, and can be found in hot springs, geothermal fields, strongly altered basic volcanic complexes (including pyroclasts and lavas), it has also been reported to be found in contact metamorphism settings. The work method included petrographic microscopy and macroscopy and X-ray diffractometry (XRD), two of the samples collected have zeolites, from the outcrops CO89A and CO89C. The CO89A outcrop has a light gray, well rounded, medium to well sorted, brittle, non‐calcareous medium grained sandstones, with volcaniclastic fragments, in this outcrop the Yugawaralite occurs as cement surrounding the clasts. In the outcrop CO89C there is a severely weathered basaltic-andesitic lava, with abundant zeolites, which fill vesicles. The observed paragenesis is Yugawaralite, Laumontite, Montmorillonite and Calcite, all these minerals are mixed in white massive and brittle aggregates. The Yugawaralite + Laumontite paragenesis, the absence of thermal springs in the area, the presence of silicified rocks nearby due to contact metamorphism caused by mafic intrusions between Copey and Santa María de Dota, suggests a contact metamorphism origin for the zeolites, corresponding to the Zeolite Facies.

Palabras clave : Hot springs; basaltic volcanic complex; contact metamorphism; zeolite facies; X-ray diffraction.

        · resumen en Español     · texto en Español     · Español ( pdf )