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Villaseca González, Carlos ; Barbero González, Luis C. ; Herreros Villanueva, Víctor Manuel | Royal Society of Edinburgh, 1980-2007. | 1998Conventional rock c1assifieation diagrams do not distinguish the variety of peraluminous rock series. Moreover, peraluminous granite types have not becn clearly discriminated in recent revisions. The study of several peraluminous series in diffe[...]texto impreso
Barbero González, Luis C. ; Villaseca González, Carlos | Royal Society of Edinburgh, 1980-2007. | 1992The Layos Granite forms elongated massifs within the Toledo Complex of central Spain. It is late-tectonic with respect to the F2 regional phase and simultaneous with the metamorphic peak of the region, which reached a maximum temperature of 800-[...]
