González Menéndez, LuisAzor, A.2014-10-302014-10-302003http://hdl.handle.net/10272/9033The Nisa-Alburquerque batholith (294 ±77 Ma) is composed of S-type granites and small stocks of l-type granitoids. The batholith was emplaced into a variety of country rocks (metasediments and metaigneous lithologies) of three different domains, namely, the southern Central Iberian zone, the Central Unit, and the northern Ossa-Morena Zone. Pressure and temperature during final emplacement is investigated by considering previous studies in the contact aureole and by comparing with P-T estimates based on the mineralogy, normative composition and geochemistry of the S-type granites. On this ground, we proposed pressures of —2,3-3 kbar, and temperatures of — 650 °C as the most plausible ones during final emplacement of this batholithspaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/Nisa-Alburquerque batholithEmplacementContact aureoleMuscoviteAndalusiteGranite solidusjournal articleopen access