%0 Journal Article
%A Villaseca González, Carlos
%A Orejana García, David
%A Pérez-Soba Aguilar, Cecilia María
%A Reyes Andrés, Jesús
%T Estimación del régimen térmico y producción de calor de losniveles litosféricos del Sistema Central Español
%D 2005
%@ 0213-683X
%U https://hdl.handle.net/20.500.14352/49616
%X Heat production of outcropping metamorphic and granitic rocks from the Spanish Central System (SCS) issimilar to other surface heat production estimates in Paleozoic provinces (average A value 2.64 mWm-3).However, heat flow range in the SCS is higher than for Paleozoic terranes (70-90 mWm-2 instead of 45-70mWm-2). Contribution of mantle to the heat budget is estimated to be 27 mWm-2. Thus, a slightly highermantle heat flow combined with a lower crust with a markedly high heat production (average A value1.04 mWm-3) may explain the high estimated surface heat flow.
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