RT Journal Article
T1 Estimación del régimen térmico y producción de calor de losniveles litosféricos del Sistema Central Español
A1 Villaseca González, Carlos
A1 Orejana García, David
A1 Pérez-Soba Aguilar, Cecilia
A1 Reyes Andrés, Jesús
AB 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.
PB Sociedad Geológica de España
SN 0213-683X
YR 2005
FD 2005
LK https://hdl.handle.net/20.500.14352/49616
UL https://hdl.handle.net/20.500.14352/49616
LA spa
DS Docta Complutense
RD 29 abr 2024