Zobrazeno 1 - 10
of 39
pro vyhledávání: '"A. Manjón-Cabeza Córdoba"'
Publikováno v:
Solid Earth, Vol 13, Pp 1585-1605 (2022)
In the eastern Atlantic Ocean, several volcanic archipelagos are located close to the margin of the African continent. This configuration has inspired previous studies to suggest an important role of edge-driven convection (EDC) in the generation of
Externí odkaz:
https://doaj.org/article/5092946325be4ce6a582355b23c5e065
Publikováno v:
Solid Earth, Vol 12, Pp 613-632 (2021)
The origin of intraplate volcanism is not explained by plate tectonic theory, and several models have been put forward for explanation. One of these models involves edge-driven convection (EDC), in which cold and thick continental lithosphere is juxt
Externí odkaz:
https://doaj.org/article/ece32eb6fbc0474caf264f4989250ac3
Publikováno v:
Geophysical Research Letters, Vol 50, Iss 16, Pp n/a-n/a (2023)
Abstract Earth's upper mantle rheology controls lithosphere‐asthenosphere coupling and thus surface tectonics. Rock deformation experiments and seismic anisotropy measurements indicate that composite rheology (co‐existing diffusion and dislocatio
Externí odkaz:
https://doaj.org/article/8a7fb56ebb2941879548494fd213b412
Autor:
Manjón-Cabeza Córdoba, Antonio1,2,3 (AUTHOR) antonio.manjon@csic.es, Ballmer, Maxim D.3,4 (AUTHOR)
Publikováno v:
Solid Earth. 2022, Vol. 13 Issue 10, p1585-1605. 21p.
The origin of the observed differences between Earth and Venus remains a mystery. On Earth, surface deformation is focused at narrow plate margins resulting in plate tectonics (or a mobile-lid regime). On Venus, a global network of connected plate ma
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5bbaa8f85c5a89c252d57a2c7b5ddcbc
https://doi.org/10.5194/egusphere-egu23-9112
https://doi.org/10.5194/egusphere-egu23-9112
It is well-established that the mantle exerts a strong control on the geodynamic processes and their expressions observed at the surface. One of the key components in mantle-surface interaction is rheology, yet, the details of this rheological coupli
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::504be6a4b7be428c8db05e6827328b90
https://doi.org/10.5194/egusphere-egu23-6948
https://doi.org/10.5194/egusphere-egu23-6948
Publikováno v:
XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
Mantle plumes - or areas of focused upwelling of hot and possibly compositionally-heterogeneous material from the base of the mantle to the surface - are features that were first predicted by the physics of mantle convection. Although they have been
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4ea63520b2f4d2e0f1497fd316c658b8
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018707
https://gfzpublic.gfz-potsdam.de/pubman/item/item_5018707
Autor:
Manjón-Cabeza Córdoba, Antonio1 (AUTHOR) a.m.c.cordoba@geo.uio.no, Ballmer, Maxim D.1,2 (AUTHOR)
Publikováno v:
Solid Earth. 2021, Vol. 12 Issue 3, p613-632. 20p.
Autor:
Charitra Jain, Antoine B. Rozel, Jeroen van Hunen, Emily J. Chin, Antonio Manjón-Cabeza Córdoba
Publikováno v:
Frontiers in Earth Science, 2022, Vol.10 [Peer Reviewed Journal]
Frontiers in Earth Science
Frontiers in Earth Science, 10
Frontiers in Earth Science
Frontiers in Earth Science, 10
Geophysical, geochemical, and geological investigations have attributed the stable behaviour of Earth’s continents to the presence of their Archean cratonic roots. These roots are likely composed of melt-depleted, low density residual peridotite wi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6c5327a196e840a7ed2187dcf4f71509
https://doi.org/10.3389/feart.2022.966397
https://doi.org/10.3389/feart.2022.966397
In the eastern Atlantic Ocean, several volcanic archipelagos are located close to the margin of the African continent. This configuration has inspired previous studies to suggest an important role of edge-driven convection (EDC) in the generation of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=copernicuspu::b797127b765b65a4dbb9d5a4a0f0158e
https://se.copernicus.org/articles/13/1585/2022/
https://se.copernicus.org/articles/13/1585/2022/