Zobrazeno 1 - 10
of 16
pro vyhledávání: '"Rheology of the Lithosphere and Mantle"'
Publikováno v:
Journal of Geophysical Research: Solid Earth, 126(3), 1
Journal of Geophysical Research. Solid Earth
Journal of Geophysical Research. Solid Earth
Laboratory studies suggest that seismogenic rupture on faults in carbonate terrains can be explained by a transition from high friction, at low sliding velocities (V), to low friction due to rapid dynamic weakening as seismic slip velocities are appr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e9ecef5c5027da320d2e8c311b69091a
https://dspace.library.uu.nl/handle/1874/412595
https://dspace.library.uu.nl/handle/1874/412595
Since the launch of the GRACE satellites in 2002, followed by GRACE-FO in 2018, the determination of seasonal hydrological variations has been significantly improved. These surface mass variations also induce crustal deformation which can be measured
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______166::811c8fad11c377493b28e96475660cba
https://hal-insu.archives-ouvertes.fr/insu-03669372
https://hal-insu.archives-ouvertes.fr/insu-03669372
Autor:
Catherine A, Rychert, Nicholas, Harmon
Publikováno v:
Geochemistry, Geophysics, Geosystems : G(3)
Strong, sharp, negative seismic discontinuities, velocity decreases with depth, are observed beneath the Pacific seafloor at ∼60 km depth. It has been suggested that these are caused by an increase in radial anisotropy with depth, which occurs in g
Publikováno v:
Geophysical Journal International
Geophysical Journal International, Oxford University Press (OUP), 2014, 198 (1), pp.285-297. ⟨10.1093/GJI/GGU134⟩
Geophysical Journal International, Oxford University Press (OUP), 2014, 198 (1), pp. 285-297. ⟨10.1093/gji/ggu134⟩
Geophysical Journal International, Oxford University Press (OUP), 2014, 198 (1), pp.285-297. ⟨10.1093/gji/ggu134⟩
Geophysical Journal International, Oxford University Press (OUP), 2014, 198 (1), pp.285-297. ⟨10.1093/GJI/GGU134⟩
Geophysical Journal International, Oxford University Press (OUP), 2014, 198 (1), pp. 285-297. ⟨10.1093/gji/ggu134⟩
Geophysical Journal International, Oxford University Press (OUP), 2014, 198 (1), pp.285-297. ⟨10.1093/gji/ggu134⟩
The geodetic rates for the gravity variation and vertical uplift in polar regions subject to past and present-day ice-mass changes (PDIMCs) provide important insight into the rheological structure of the Earth. We provide an update of the rates obser
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::47c8642770cb95aef7936625341d4305
https://hal.archives-ouvertes.fr/hal-03038091
https://hal.archives-ouvertes.fr/hal-03038091
Publikováno v:
Geophysical Research Letters
Geophysical Research Letters, American Geophysical Union, 2004, 31, pp.L23607. ⟨10.1029/2004GL021006⟩
Geophysical Research Letters, American Geophysical Union, 2004, 31, pp.L23607. ⟨10.1029/2004GL021006⟩
International audience; Coupling between erosion and tectonics is thought to play a determinant role in orogenic evolution. Here, we investigate the interplay in this coupling between the assumed erosion law and the crustal rheology at the margin of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::b1299157b5de989517f35cbb96e7f48f
https://hal.archives-ouvertes.fr/hal-00079361/document
https://hal.archives-ouvertes.fr/hal-00079361/document
Autor:
Sigmundsson, Freysteinn, Erik, Sturkell, Virginie, Pinel, Pall, Einarsson, Rikke, Pedersen, Halldor, Geirsson, Magnus Tumi Gudmundsson, Helgi, Bjornsson, Pagli, Carolina
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______3728::f6cf3011f01f64645a40fb8f29332af0
http://hdl.handle.net/11568/1076481
http://hdl.handle.net/11568/1076481
Autor:
Milne, G. A., Mitrovica, J. X., Davis, J. L., Scherneck, H. G., Johansson, J. M., Koivula, H., Vermeer, M.
Publikováno v:
Journal of geophysical research : solid earth, 2004, Vol.109, pp.B02412 [Peer Reviewed Journal]
Data collected under the auspices of the BIFROST GPS project yield a geographically dense suite of estimates of present-day, three-dimensional (3-D) crustal deformation rates in Fennoscandia [ Johansson et al., 2002 ]. A preliminary forward analysis
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od_______328::cb4db8af1c0481ba508bbe5b2525609f
http://dro.dur.ac.uk/2098/
http://dro.dur.ac.uk/2098/
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