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Barbero González, Luis C. ; Glasmacher, U. A. ; Villaseca González, Carlos ; López García, José Ángel ; Martín Romera, Cristina | Springer Science Business Media | 2005Abstract In the Montes de Toledo area, located in the axial part of the Central Hercynian zone, a long-term thermo-tectonic evolution can be deduced from apatite fission-track (AFT) data in conjunction with tight geological constraints derived f[...]texto impreso
Villaseca González, Carlos ; Martín Romera, Cristina ; Barbero González, Luis C. | Elsevier Sciences Ltd. | 2001Granulite terranes from Central Spain are Hercynian anatectic areas of mid-crustal levels (P-T conditions: 750-800 ° C and 4-6 kb), The granulite xenolith suite of the same sector comes from the lower crust as deduced from their P-T estimates (8[...]texto impreso
Villaseca González, Carlos ; Martín Romera, Cristina ; De la Rosa Díaz, Jesús Damián ; Barbero González, Luis C. | Elsevier Science B.V., Amsterdam. | 2003Accessory minerals are thought to play a key role in controlling the behaviour of certain trace elements such as REE, Y, Zr, Th and U during crustal melting processes under high-grade metamorphic conditions. Although this is probably the case at[...]texto impreso
Castiñeiras García, Pedro ; Villaseca González, Carlos ; Barbero González, Luis C. ; Martín Romera, Cristina | Springer Science Business Media | 2008U–Pb SHRIMP ages obtained in zircons from the Sotosalbos and Toledo anatectic complexes in Central Spain give new constraints to the evolution of the inner part of the Hercynian Iberian belt. Pre- Hercynian ages in zircons from the Sotosalbos co[...]
