¡Nos trasladamos! E-Prints cerrará el 7 de junio.

En las próximas semanas vamos a migrar nuestro repositorio a una nueva plataforma con muchas funcionalidades nuevas. En esta migración las fechas clave del proceso son las siguientes:

Es muy importante que cualquier depósito se realice en E-Prints Complutense antes del 7 de junio. En caso de urgencia para realizar un depósito, se puede comunicar a docta@ucm.es.

Is Earth-based scaling a valid procedure for calculating heat flows for Mars?



Downloads per month over past year

Ruiz Pérez, Javier and Williams, Jean-Pierre and Dohm, James M. and Fernández, Carlos and López, Valle (2013) Is Earth-based scaling a valid procedure for calculating heat flows for Mars? Icarus (New York, N.Y. 1962), 226 (1). pp. 536-540. ISSN 0019-1035

[thumbnail of 46-ICARUS-12593R1-1.pdf]

Official URL: http://www.sciencedirect.com/science/article/pii/S0019103513002686


Heat flow is a very important parameter for constraining the thermal evolution of a planetary body. Several procedures for calculating heat flows for Mars from geophysical or geological proxies have been used, which are valid for the time when the structures used as indicators were formed. The more common procedures are based on estimates of lithospheric strength (the effective elastic thickness of the lithosphere or the depth to the brittle–ductile transition). On the other hand, several works by Kargel and co-workers have estimated martian heat flows from scaling the present-day terrestrial heat flow to Mars, but the so-obtained values are much higher than those deduced from lithospheric strength. In order to explain the discrepancy, a recent paper by Rodriguez et al. (Rodriguez, J.A.P., Kargel, J.S., Tanaka, K.L., Crown, D.A., Berman, D.C., Fairén, A.G., Baker, V.R., Furfaro, R., Candelaria, P., Sasaki, S. [2011]. Icarus 213, 150–194) criticized the heat flow calculations for ancient Mars presented by Ruiz et al. (Ruiz, J., Williams, J.-P., Dohm, J.M., Fernández, C., López, V. [2009]. Icarus 207, 631–637) and other studies calculating ancient martian heat flows from lithospheric strength estimates, and casted doubts on the validity of the results obtained by these works. Here however we demonstrate that the discrepancy is due to computational and conceptual errors made by Kargel and co-workers, and we conclude that the scaling from terrestrial heat flow values is not a valid procedure for estimating reliable heat flows for Mars

Item Type:Article
Uncontrolled Keywords:Mars; Mars, Interior; Tectonics; Thermal histories
Subjects:Sciences > Geology > Geodynamics
ID Code:31395
Deposited On:10 Jul 2015 10:10
Last Modified:14 Jul 2015 07:29

Origin of downloads

Repository Staff Only: item control page