RT Journal Article
T1 Petrografía, geoquímica y posible origen del plutón de Salvatierra de los Barros (Zona de Ossa Morena, Badajoz)
T1 Petrography, geochemistry and possible origin of the Salvatierra de los Barros pluton (Ossa Morena Zone, Badajoz)
A1 Carracedo Sánchez, Manuel
A1 Sarrionandia Eguidazu, Fernando
A1 Eguiluz, Luis
A1 Apalategui, Octavio
AB The Salvatierra de los Barros pluton is mainly composed by medium grain biotite monzogranites andgranodiorites, with common monazite and apatite, and lesser cordierite and allanite. These rocks showmassive structure and apparent isotropic fabric, but have a solid state, brittle to brittle – ductilemicrostructural deformation. These rocks are peraluminous, with variable amounts in potassium, highcontents in calcium and low contents in ferromagnesian minerals; they have also normative corundum.Radiometric data obtained by different authors are in agreement with our geochemical data, and indicatean hibrid origin from mixing of pelitic melts and basaltic melts, in a Cadomian post-collisional settling
YR 2006
FD 2006
LK http://hdl.handle.net/10272/8506
UL http://hdl.handle.net/10272/8506
LA spa
DS Repositorio Institucional de la Universidad de Huelva
RD 30 may 2026