Zobrazeno 1 - 5
of 5
pro vyhledávání: '"Remi Vachon"'
Publikováno v:
Geophysical Journal International. 226:709-727
This article has been accepted for publication in Geophysical Journal International ©: 2021 Vachon, REC, Bazargan, Hieronymus, Ronchin, Almqvist B. Published by Oxford University Press on behalf of the Royal Astronomical Society. All rights reserved
Autor:
Andreia Plaza-Faverola, Frances Cooke, Remi Vachon, Kate Waghorn, Jean Baptiste Koehl, Stefan Beaussier, Stefan Bünz
The continent–ocean transition along the passive margin off western Svalbard is, in places, only a few kilometers away from the formerly glaciated continental shelf. Strong bottom currents in the Fram Strait have led to the deposition of several ki
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2c05d48b558268eb73916fc3655e3b67
https://doi.org/10.5194/egusphere-egu22-11917
https://doi.org/10.5194/egusphere-egu22-11917
Publikováno v:
Geophysical Journal International. 218:773-786
Magmas and other viscously deforming fluids in the Earth frequently contain embedded crystals or other solid inclusions. These inclusions generally rotate about their own axis and, under certain co ...
Autor:
Christoph F. Hieronymus, Remi Vachon
The dynamics of dyke emplacement are typically modelled by assuming an elastic rheology for the host rock. However, the resulting stress field predicts significant shear failure in the region surrounding the dyke tip. Here, we model the dyking proces
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::0fce681e2cca0f04a718af4527bece21
http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-400007
http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-400007
Autor:
Christoph F. Hieronymus, Remi Vachon
Publikováno v:
Geophysical Journal International. 208:1414-1429
The size and thickness of dykes is of fundamental importance for volcano dynamics because dykes are the primary path for magma transport, and because large numbers of dykes often comprise a major proportion of the volcanic edifice and of the underlyi