RT Journal Article
T1 Nota preliminar sobre la presencia de turmalinitas estratiformes en el Ordovícico Inferior de Latedo (NO de Zamora)
A1 Fernández Fernández, A.
A1 Moro Benito, M. C.
AB In this paper, the geological, texto-structural, mineralogical and chemical features of the stratiforme tourmalinites from the Lower Ordovician volcano-sedimentary Cabeza de las Viñas Formation (Alcañices Synforme), are given. According to these data, it is suggested that these tourmalinites has been originated by regional metamorphisme of the B-rich pelitic beds. The B were probably trought to the sediment by the hidrothermal solutions related with the underlayžng metabasaltic rocks existing in the studied area
PB Sociedad Geológica de España
YR 1991
FD 1991
LK http://hdl.handle.net/10272/18005
UL http://hdl.handle.net/10272/18005
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 30 may 2026