RT Journal Article
T1 The thermal state and strength of the lithosphere in the Spanish Central Systemand Tajo Basin from crustal heat production and thermal isostasy
A1 Jiménez Díaz, Alberto
A1 Ruiz Pérez, Javier
A1 Villaseca González, Carlos
A1 Tejero López, Rosa
A1 Capote Del Villar, Ramón
AB In this work we have modeled the thermal structure of the lithosphere of the Spanish Central System and the Tajo Basin, and their implications for lithospheric strength. For  his, we have used refined heatproducing elements (HPE) values to obtain new estimates of heat production rates in the Spanish Central System and Tajo Basin areas, which have been used joined to the relation between topography and thermal structure of the lithosphere to calculate the best- it surface heat flows in the study area. Moreover, we have implemented a temperature-dependent thermal conductivity (appropriate for olivine) for the lithospheric mantle to improve the calculations of temperature profiles in the mantle. The geotherms so obtained, together with the implementation of a new rheological law for the upper lithospheric mantle, have been used to calculate refined estimations of the strength and effective elastic thickness of the lithosphere. We have obtained surface heat flow values of 84 mW m−2 and ∼82 mW m−2 for the Spanish Central System and the Tajo Basin, respectively. The thermal state of the lithosphere affects mantle temperatures, and hence may be playing an important role in the uplift and maintenance of the Spanish Central System.
PB Elsevier Science B.V
SN 0264-3707
YR 2012
FD 2012
LK https://hdl.handle.net/20.500.14352/42398
UL https://hdl.handle.net/20.500.14352/42398
LA eng
DS Docta Complutense
RD 6 abr 2025