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Intraplate main structural units of the Iberian Plate (Spanish Central System and Tertiary Basins) results from a mid-Tertiary compressive regime, caused by the convergence of African and European Plates. Crustal structure of this zone has been [...]texto impreso
Lobate scarps are the topographic expression of the largest thrust faults observed on the surfaces of terrestrial planets and their study provides information on the mechanical characteristics of the lithosphere at the time of formation. Here we[...]texto impreso
Analyses of the effective elastic thickness of the Martian lithosphere have been previously used to calculate surface heat flow on Mars at different places and times. In this work, I use elevation differences in a putative Late Hesperian shoreli[...]texto impreso
The proposed existence of magnetic lineations in the Terra Cimmeria and Terra Sirenum regions of Mars was initially explained by Earth-like sea-floor spreading. Here we argue instead that these lineations could have been formed at a convergent p[...]texto impreso
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Ruiz Pérez, Javier ; Williams, Jean-Pierre ; Dohm, James M. ; Fernández, Carlos ; López, Valle | Rosen Pub. Group | 2009Heat flow calculations based on geological and/or geophysical indicators can help to constrain the thickness, and potentially the geochemical stratification, of the martian crust. Here we analyze the Warrego rise region, part of the ancient moun[...]texto impreso
Ruiz Pérez, Javier ; Fernández, Carlos ; Gómez Ortiz, David ; Dohm, James M. ; López, Valle ; Tejero López, Rosa | Elsevier Science B.V., Amsterdam | 2008Surface heat flow calculations for the Amenthes region of Mars can be independently performed using the depth to the brittle–ductile transition and the effective elastic thickness of the lithosphere estimated for the Late Noachian/Early Hesperia[...]texto impreso
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Gómez Ortiz, David ; Tejero López, Rosa ; Ruiz Pérez, Javier ; Babín Vich, Rosa Blanca ; González Casado, José Manuel | Sociedad Geológica de España. | 2004Effective elastic thickness of the Iberian Peninsula lithosphere was estimated from a coherence analysis of topography and gravity spectra. A multitaper technique was used to estimate spectra. Coherence estimates provide an average Te value o f [...]texto impreso
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Dohm, James M. ; Anderson, Robert C. ; Williams, Jean-Pierre ; Ruiz Pérez, Javier ; McGuire, Patrick C. ; Buczkowski, Debra L. ; Wang, Ruye ; Scharenbroich, Lucas ; Hare, Trent M. ; Connerney, J.E.P. ; Baker, Victor R. ; Wheelock, Shawn J. ; Ferris, Justin C. ; Miyamoto, Hirdy | Elsevier Science Publishers | 2009Claritas rise is a prominent ancient (Noachian) center of tectonism identified through investigation of comprehensive paleotectonic information of the western hemisphere of Mars. This center is interpreted to be the result of magmatic-driven act[...]texto impreso
Ruiz Pérez, Javier ; Jiménez Díaz, Alberto ; Parro, Laura M. ; Egea González, Isabel ; Mansilla, Federico | Elsevier | 2019-04Two recent papers, by Karimi et al. (2016, Icarus 272, 102–113) and Karimi and Dombard (2017, Icarus 282, 34–39), tried to deduce paleo-heat flows for, respectively, Mars and Venus from modeling the viscoelastic relaxation of large impact crater[...]texto impreso
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Gómez Ortiz, D. ; Agarwal, B.N.P. ; Tejero López, Rosa ; Ruiz Pérez, Javier | Geological Society of America | 2011Through two-dimensional fi ltering and spectral analysis of gravity data, we infer the density structure of the Iberia Peninsula’s lithosphere (western Europe). The gravity anomaly map of the Iberian Peninsula displays long-wavelength anomaly mi[...]texto impreso
Depth of faulting and ancien theat flows in the Kuiper region of Mercuryfrom lobate scarp topography
Egea González, Isabel ; Ruiz Pérez, Javier ; Fernández Rodríguez, Carlos ; Williams, Jean-Pierre ; Márquez González, Álvaro ; Lara López, Luisa M. | Elsevier B.V. | 2012Mercurian lobate scarp sare interpreted to be the surface expressions of thrust faults formed by planetary cooling and contraction, which deformed the crust downto the brittle–ductile transition (BDT) dep that the time of faulting. In this work[...]
