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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
We have applied the analytic model of general triclinic transpression with oblique extrusion to an active shear zone in southeastern Spain. This study opens a new methodological approach in the study of active fault zones. We are able to constra[...]texto impreso
Fernández, Carlos ; Alonso Chaves, Francisco M. ; Anguita, Francisco | Asociación Española para la Enseñanza de las Ciencias de la Tierra | 2013Este artículo contiene una revisión de la historia y contenido actual de un concepto, el de astenosfera, clave en las modernas Ciencias de la Tierra. Definido por Barrell en 1914, cuando Wegener diseñaba su primer ataque a la Tierra inmóvil, fue[...]texto impreso
Ruiz Pérez, Javier ; Williams, Jean-Pierre ; Dohm, James M. ; Fernández, Carlos ; López, Valle | Elsevier Science B.V., Amsterdam | 2013Heat 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 t[...]texto impreso
It is well known that jointly measurable observables cannot lead to a violation of any Bell inequality-independent of the state and the measurements chosen at the other site. In this Letter we prove the converse: every pair of incompatible quant[...]texto impreso
This work shows the results of a structural study of the faults observed at the Tempe Rift (northeastern Tharsis region), Mars. A new, detailed map of faults and fault systems was used to geometrically characterize the fracture architecture of t[...]texto impreso
Amrán, Donna ; Sancho, Patricia ; Fernández, Carlos ; Esteban Fernández, Diego ; Ramos, Adrian M. ; Blas, Elena de ; Gómez Gómez, M.Milagros ; Palacios Corvillo, María A. ; Aller, Patricio | Elsevier | 2005It has been reported that inhibition of extracellular signal-regulated protein kinases (ERKs) attenuates the toxicity cisplatin (cisplatinum (II)-diammine dichloride) in some cell types. This response was here investigated using human myeloid le[...]texto impreso
Ruiz Pérez, Javier ; López, Valle ; Dohm, James M. ; Fernández, Carlos | Elsevier Science B.V., Amsterdam | 2012Lobate scarps, thought to be the surface expression of large thrust faults, are the most spectacular contractional tectonic features visible on Mercury. Most lobate scarps follow a general and relatively simple pattern, with a roughly arcuate or[...]texto impreso
Fernández, Carlos ; Anguita, Francisco ; Ruiz Pérez, Javier ; Romeo Briones, Ignacio ; Martín Herrero, Álvaro Ignacio ; Rodríguez, Alberto ; Pimentel, Carlos | Rosen Pub. Group | 2009This work shows the results of a detailed structural analysis of the deformation belts of Lavinia Planitia. Ridge belts and graben and groove belts can be observed at the studied area, while wrinkle ridges and large individual grooves predominat[...]
