Villaseca, CarlosOrejana, DavidPin, C.López García, José ÁngelAndonaegui, P.Encina, L.2014-11-172014-11-172002http://hdl.handle.net/10272/9311Basic magmatism in Central Spain occur sporadically during a long period of ca. 140 Ma. The scarce data set of incompatible trace element geochemistry and initial isotopic ratios (Sr, Nd) on mantle-derived basic magmatism show that subcontinental mantle in Central Spain is markedly heterogeneous. Depleted mantle compositions are not registered and basic magmatism fluctuate between OIB and BSE values, being crustal involvement (via recycling in mantle sources or by hybridization at emplacement levels) an important contribution to some basic derivatesspaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/Basic rocksSubcontinental mantleGeochemistry(Sr, Nd) isotopesSistema Central EspañolEstimación de la composición del manto subcontinental en el centro de España a partir de los materiales básicos hercínicos y post-hercinicos del Sistema Central EspañolComposition estimates of Central Spain subcontinental mantle: inferences from Hercynian and post-Hercynian basic rocks from the Sistema Central Españoljournal articleopen access