RT info:eu-repo/semantics/article
T1 Geochemical characterization of serpentinites at Cabo Ortegal, Northwestern Spain
A1 Pereira Gómez, María Dolores
A1 Peinado Moreno, María Mercedes
A1 Blanco Sánchez, José Antonio
A1 Yenes Ortega, Mariano
K1 Serpentinitas
K1 Geoquímica
K1 Cabo Ortegal
K1 España
K1 Serpentinites
K1 Geochemistry
K1 Spain
AB Cabo Ortegal is one of the major ultramafic complexes outcropping in Iberia. Most rocks are variably serpentinized, and the characteristics of the process can be traced through the composition of the rocks. The major and trace elements change in the different units of the complex. Together with the wide range of oxygen isotope values (d18O from 3.9 up to 6.6 ), these changes lead to the conclusion that several stages of serpentinization took place at Cabo Ortegal. Each stage is characterized by the composition of the fluid that produced the serpentinization. Seawater does not have to be the main fluid in the process; an ultimate stage of serpentinization can mask the characteristics of a previous one.
PB Mineralogical Association of Canada (Toronto, Canadá)
YR 2008
FD 2008
LK http://hdl.handle.net/10366/19413
UL http://hdl.handle.net/10366/19413
UL http://hdl.handle.net/10366/19413
LA eng
NO PEREIRA, M.,D., PEINADO, M., BLANCO, J. A., YENES, M. (2008). Geochemical characterization of serpentinites at Cabo Ortegal, Northwestern Spain. "The Canadian Mineralogist", 46, 317-327.
DS Gestión del Repositorio Documental de la Universidad de Salamanca
RD 26-sep-2024