@article{10272/13278,
year = {1996},
url = {http://hdl.handle.net/10272/13278},
abstract = {The Mercedita chromite podiform deposit is genetically and spatially related to the Moa-Baracoa ophiolite complex (NW Cuba). The ore bodies are crosscuted by veins, filled up by uvarovite with variable amounts of chromiferous clinochlore , calcite, titanite and rutile. Garnets are zoned and display a broad composition comprised between uvarovite and grossular end members. Their andradite content is very low. These garnets were formed by hydrothermal circulation during late episodes of ophiolite emplacement.},
publisher = {Sociedad Geológica de España},
title = {Granates de la serie Grosularia-uvarovita en cromititas prodiformes del yacimiento Mercedita (Cuba)},
title = {Grossular-uvarovite garnets in podiform chromitite from Mercedita deposit (Cuba)},
author = {Proenza, Joaquín A. and Melgarejo i Draper, J. C.},
}