Zobrazeno 1 - 10
of 34
pro vyhledávání: '"Claude Froidevaux"'
Publikováno v:
Geophysical Monograph Series ISBN: 0875904688
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::53c15b4369941237fdf18fefa9d64fa0
https://doi.org/10.1029/gm082
https://doi.org/10.1029/gm082
Publikováno v:
Physics of the Earth and Planetary Interiors
Physics of the Earth and Planetary Interiors, 1994, 84 (1-4), pp.3-13
Physics of the Earth and Planetary Interiors, 1994, 84 (1-4), pp.3-13
cited By 43; In this study, several mantle tomography models are used as input to constrain the amplitude of mass anomalies and viscosity variations with depth in the mantle. For this purpose, we compute the dynamical state of an incompressible mantl
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::962d97e503fbdaa1a0a30f75a3409919
https://hal.archives-ouvertes.fr/hal-02046762
https://hal.archives-ouvertes.fr/hal-02046762
Publikováno v:
Tectonophysics
Tectonophysics, 1991, 187 (4), pp.345-360
Tectonophysics, 1991, 187 (4), pp.345-360
cited By 30; Plate velocities reflect the global mantle circulation which carries the heat from the deep part of the Earth to the surface. Three other measurable parameters put strong constraints on the physical processes involved in mantle dynamics:
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::55486473b64781bc07192e525577eb92
https://hal.archives-ouvertes.fr/hal-02046600
https://hal.archives-ouvertes.fr/hal-02046600
Autor:
Yanick Ricard, Claude Froidevaux
Publikováno v:
pp.553-569, 1990
Scopus-Elsevier
Glacial Isostasy, Sea-Level and Mantle Rheology ISBN: 9789401054928
Scopus-Elsevier
Glacial Isostasy, Sea-Level and Mantle Rheology ISBN: 9789401054928
The dynamics of the Earth’s mantle, which has a clear signature at the surface in the form of plate motion, can only be investigated indirectly. The geoid reflects the density heterogeneities driving this mantle circulation. Recent tomographic mode
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6a7b896c798529bd4bd010a782bba867
https://hal.archives-ouvertes.fr/hal-02046603
https://hal.archives-ouvertes.fr/hal-02046603
Publikováno v:
Geophysical Journal International. 54:93-119
Summary. Narrow zones of intense shear deformation, i.e. viscous slip zones, are studied analytically with a one-dimensional time-dependent model of two half-spaces of identical or contrasting rheologies and ambient temperatures in relative motion. T
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::96b1e3305efada1313925fbccb85975e
https://doi.org/10.1111/j.1365-246x.1978.tb06758.x
https://doi.org/10.1111/j.1365-246x.1978.tb06758.x
Publikováno v:
Rock Mechanics and Rock Engineering
Rock Mechanics and Rock Engineering, 1989, 22 (4), pp.289-297
Rock Mechanics and Rock Engineering, 1989, 22 (4), pp.289-297
cited By 2; Stresses in the Earth's crust are known to represent a key element of geodynamical processes at various spatial and temporal scales. Static stresses within lithospheric plates can be estimated on the basis of direct in situ measurements i
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8fa097d3cfa242e24b9b40a73642ec3e
https://doi.org/10.1007/bf01262284
https://doi.org/10.1007/bf01262284
Autor:
Claude Froidevaux, Luce Fleitout
Publikováno v:
Tectonics. 1:21-56
The purpose of this paper is to clarify the dynamic role of lithospheric density heterogeneities, in particular with respect to mountain building and other processes of intraplate deformation. Density anomalies within or just beneath the lithosphere
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::491dc9679234133b7655bba08aedcf4b
https://doi.org/10.1029/tc001i001p00021
https://doi.org/10.1029/tc001i001p00021
Autor:
Isabelle Moretti, Claude Froidevaux
Publikováno v:
Tectonics. 5:501-511
Geological and geophysical evidence (in particular thermal and gravity anomalies) suggests the presence of hot mantle material below the zones of continental rifting. Using a thermomechanical numerical model we quantify the lithospheric thinning caus
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a166aa94a9f26d38d13fbe31431986f8
https://doi.org/10.1029/tc005i004p00501
https://doi.org/10.1029/tc005i004p00501
Autor:
Claude Froidevaux, Yanick Ricard
Publikováno v:
Tectonophysics
Tectonophysics, 1987, 134 (1-3), pp.227-238
ResearcherID
Tectonophysics, 1987, 134 (1-3), pp.227-238
ResearcherID
The striking contrast in tectonic style between highlands like Tibet with its active grabens, and low altitude flanks, like the thrusting structures in the foothills of the Himalayas, shows that a disorder of the tectonic stresses correlates with the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::629e7295779e73bffae00e41c5df7326
https://doi.org/10.1016/0040-1951(87)90259-9
https://doi.org/10.1016/0040-1951(87)90259-9