RT Journal Article
T1 Sucesión de secuencias volcánicas félsicas en el Complejo Vulcanosedimentario de la Faja Pirítica Ibérica: discriminación entre modelos volcánicos y subvolcánicos
T1 Succession of felsic volcanic sequences in the Volcano-Sedimentary Complex in the Iberian Pyrite Belt:discrimination between volcanic and subvolcanic models
A1 Donaire Romero, Teodosio
A1 Pascual Martínez, Emilio
A1 Valenzuela Aznar, Alfonso
A1 González Roldán, Manuel Jesús
A1 Toscano Macías, Manuel
AB A field study is presented on two selected areas in the Volcano-Sedimentary Complex (VSC) of the IberianPyrite Belt (IPB), the Odiel River section and the Paymogo Volcanic lineament. Field evidence has allowedto distinguish two major groups of felsic rocks, which successively appear in the stratigraphic column.Probably, this conclusion can be extended to other areas in the IPB. In addition, field, petrographic andgeochemical evidence shows that at least the felsic rhyolitic succession in the Odiel River (and probablyalso in Paymogo) formed in a volcanic, environment, favouring a volcanic-pile model in the VSC
PB Sociedad Geológica de España
YR 2006
FD 2006
LK http://hdl.handle.net/10272/8635
UL http://hdl.handle.net/10272/8635
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 30 may 2026