Zobrazeno 1 - 5
of 5
pro vyhledávání: '"Colin Pagani"'
Publikováno v:
Journal of Geophysical Research : Solid Earth
Journal of Geophysical Research : Solid Earth, 2021, 126 (6), pp.e2021JB021905. ⟨10.1029/2021JB021905⟩
Journal of Geophysical Research : Solid Earth, American Geophysical Union, 2021, 126 (6), pp.e2021JB021905. ⟨10.1029/2021JB021905⟩
Journal of Geophysical Research : Solid Earth, 2021, 126 (6), pp.e2021JB021905. ⟨10.1029/2021JB021905⟩
Journal of Geophysical Research : Solid Earth, American Geophysical Union, 2021, 126 (6), pp.e2021JB021905. ⟨10.1029/2021JB021905⟩
International audience; Seismic hazard assessment in active fault zones can benefit of strain rate measurements derived from geodetic data. Producing a continuous strain rate map from discrete data is an inverse problem traditionally tackled with sta
Autor:
Christian Sue, Marguerite Mathey, Colin Pagani, Estelle Hannouz, Bertrand Potin, Andrea Walpersdorf, Stéphane Baize, Thomas Bodin, Laurent Husson
Due to the low to moderate seismicity of the European Western Alps, few focal mechanisms are available to date in this region, and the corresponding current seismic stress and strain fields remain partly elusive. The development of dense seismic netw
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8f8ec018893738dec3f839a21a961cbd
https://doi.org/10.5194/egusphere-egu21-14963
https://doi.org/10.5194/egusphere-egu21-14963
Autor:
Marguerite Mathey, Christian Sue, Colin Pagani, Stéphane Baize, Andrea Walpersdorf, Thomas Bodin, Laurent Husson, Estelle Hannouz, Bertrand Potin
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4b918a60d99ee4a3dc7a012403fcc96e
https://doi.org/10.5194/se-2020-196-supplement
https://doi.org/10.5194/se-2020-196-supplement
Autor:
Marguerite Mathey, Christian Sue, Bertrand Potin, Colin Pagani, Thomas Bodin, Laurent Husson, Estelle Hannouz, Stéphane Baize, Andrea Walpersdorf
In the Western Alpine arc, GNSS measurements indicate that the far field convergence responsible for the Oligo-Miocene continental collision is now over. However, seismicity and slow deformation are still active. Former collisional tectonic features,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f280c0fc1b36703a6085626f03ccf915
https://doi.org/10.5194/egusphere-egu2020-7546
https://doi.org/10.5194/egusphere-egu2020-7546