@article{10272/8713,
year = {2005},
url = {http://hdl.handle.net/10272/8713},
abstract = {Heat production of outcropping metamorphic and granitic rocks from the Spanish Central System (SCS) is
similar 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 45-70
mWm-2). Contribution of mantle to the heat budget is estimated to be 27 mWm-2. Thus, a slightly higher
mantle heat flow combined with a lower crust with a markedly high heat production (average A value
1.04 mWm-3) may explain the high estimated surface heat flow},
publisher = {Sociedad Geológica de España},
title = {Estimación del régimen térmico y producción de calor de los niveles litosféricos del Sistema Central Español},
title = {Thermal regime and heat production estimates for lithospheric levels of the Spanish Central System},
author = {Villaseca, Carlos and Orejana, David and Pérez Soba, C. and Reyes Abril, J.},
}