RT Journal Article
T1 Granates de la serie Grosularia-uvarovita en cromititas prodiformes del yacimiento Mercedita (Cuba)
T1 Grossular-uvarovite garnets in podiform chromitite from Mercedita deposit (Cuba)
A1 Proenza, Joaquín A.
A1 Melgarejo i Draper, J. C.
AB 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.
PB Sociedad Geológica de España
YR 1996
FD 1996
LK http://hdl.handle.net/10272/13278
UL http://hdl.handle.net/10272/13278
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 30 may 2026