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Departamento de Geodinámica, Facultad de Ciencias Geológicas, Universidad Complutense de Madrid, 28040 Madrid, Spain
Departamento de Geodinámica, Facultad de Ciencias Geológicas, Universidad Complutense de Madrid, 28040, Madrid, Spain
Departamento de Geodinámica, Facultad de Ciencias Geológicas, Universidad Complutense de Madrid, Madrid 28040, Spain
Departamento de Geodinámica, Facultad de Ciencias Geológicas, Universidad Complutense de Madrid, 28040 Madrid, Spain; Instituto de Geociencias, CSIC-UCM, 28040 Madrid, Spain
Departamento de Geodinámica, Universidad Complutense de Madrid, Antonio Novais s / n, Madrid, 28040, Spain
Department Geodinámica, Univ. Complutense Madrid, Spain
Universidad Complutense de Madrid, Departamento de Geodinámica, Madrid, Spain
Ancient heat flow, crustal thickness, and lithospheric mantle rheology in the Amenthes region, Mars
Estimating the effective elastic thickness of the lithosphere of the Iberian peninsula based on multitaper spectral analysis
Estimation of Heat Sources in Planetary Crusts from Isotherm Depth, Surface Heat Flow, and Crustal Thickness
Evidence for a differentiated crust in Solis Planum, Mars, from lithospheric strength and heat flow
Heat Flow and Brittle-Ductile Transition in the Ice Shell of Europa
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Profile ID: LFWR-SCP-P-424428