Zobrazeno 1 - 10
of 52
pro vyhledávání: '"Sylvain Calassou"'
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 24, Iss 11, Pp n/a-n/a (2023)
Abstract The rift‐to‐drift transition at rifted margins is an area of active investigation due to an incomplete understanding of the spatial and temporal evolution of physical and chemical processes at the ocean‐continent transition (OCT). Deep
Externí odkaz:
https://doaj.org/article/22c1e91d0bb3410890fc8cd611f6bb0e
Autor:
Nicolas Lefeuvre, Laurent Truche, Frédéric‐Victor Donzé, Maxime Ducoux, Guillaume Barré, Rose‐Adeline Fakoury, Sylvain Calassou, Eric C. Gaucher
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 22, Iss 8, Pp n/a-n/a (2021)
Abstract Native hydrogen (H2) may represent a new carbon free‐energy resource, but to date there is no specific exploration guide to target H2‐fertile geological settings. Here, we present the first soil gas survey specifically designed to explor
Externí odkaz:
https://doaj.org/article/a8d846dd1297474a9e89503085f713b8
Autor:
Bruno Leclere, Hannelore Derluyn, Eric C. Gaucher, Sylvain Calassou, Joseph Diaz, Jean-Paul Callot, David Grégoire
Publikováno v:
Geochimica et Cosmochimica Acta. 337:49-60
Autor:
Frédéric Mouthereau, Marine Larrey, Louise Boschetti, Nicolas Beaudoin, Stéphanie Brichau, Nick Roberts, Damien Huyghe, Matthieu Daëron, Véronique Miegebielle, Sylvain Calassou
The Alboran margin in the Betics formed as a result of backarc crustal thinning oblique to the direction of the slab retreat. The history of sediment infill, subsidence and faulting reveals extension at upper crustal levels operated from the Serraval
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::74f7276fe28451375dbcae6cd8644169
https://doi.org/10.5194/egusphere-egu23-13467
https://doi.org/10.5194/egusphere-egu23-13467
Autor:
Eric Lasseur, Alexandre Ortiz, Charlotte Fillon, Justine Briais, Francois Guillocheau, Jessica Uzel, Gianlucca Frasca, Jocelyn barbarand, Nicolas Loget, Sebastien Castellort, Sylvain Calassou
Publikováno v:
EGU General Assembly 2023
EGU General Assembly 2023, European Geosciences Union, Apr 2023, Vienna, Austria. pp.EGU23-12761, ⟨10.5194/egusphere-egu23-12761⟩
EGU General Assembly 2023, European Geosciences Union, Apr 2023, Vienna, Austria. pp.EGU23-12761, ⟨10.5194/egusphere-egu23-12761⟩
International audience; The knowledge acquired on the exhumation of the Pyrenean chain and the evolution of the adjacent foreland basins makes this Alpine-type domain a good laboratory to better constrain a full sediment routing system in a compressi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d67d9b986ce3ada26b064227ec30b440
https://doi.org/10.5194/egusphere-egu23-12761
https://doi.org/10.5194/egusphere-egu23-12761
The rift-to-drift transition at rifted margins is an area of active investigation due to unresolved issues of the ocean-continent transition (OCT). Deep structures that characterize modern OCTs are often difficult to identify by seismic observations,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8b323dcbaed4cc30cf99a4c147efeef4
Publikováno v:
GSA Bulletin. 134:941-964
Half grabens and supra-detachment basins correspond to end-member basin types of magma-poor rift settings, each of them showing a characteristic stratigraphic architecture. The occurrence of a basement-cover décollement has been shown to drastically
Autor:
Eric Lasseur, Charlotte Fillon, Justine Briais, Alexandre ORTIZ, François Guillocheau, Paul Bessin, Guillaume Baby, Julien Baptiste, Jessica Uzel, Cécile Robin, Sylvain Calassou, Gianluca Frasca, Sebastien Castelltort
Publikováno v:
ASF 2022-XVIIIème Congrès Français de Sédimentologie
ASF 2022-XVIIIème Congrès Français de Sédimentologie, Sep 2022, Brest, France
HAL
ASF 2022-XVIIIème Congrès Français de Sédimentologie, Sep 2022, Brest, France
HAL
International audience; L’ensemble des données et connaissances acquises sur la chaine Pyrénéenne et l’évolution de ces bassins d’avant-pays permettent à présent d’appréhender ce système orogénique et l’évolution des bassins dans
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::ab74ce5e57e66ea9e2516639048e3fa4
https://hal.science/hal-03781507
https://hal.science/hal-03781507
Autor:
Maxime Tremblin, Hassan Khozyem, Thierry Adatte, Jorge E. Spangenberg, Charlotte Fillon, Arnaud Grauls, Teodoro Hunger, Andres Nowak, Charlotte Läuchli, Eric Lasseur, Jean-Yves Roig, Olivier Serrano, Sylvain Calassou, François Guillocheau, Sébastien Castelltort
Publikováno v:
Global and Planetary Change
Global and Planetary Change, 2022, 212, pp.103794. ⟨10.1016/j.gloplacha.2022.103794⟩
Global and Planetary Change, Elsevier, 2022, 212, pp.103794. ⟨10.1016/j.gloplacha.2022.103794⟩
Global and Planetary Change, vol. 212, pp. 103794
Global and Planetary Change, 2022, 212, pp.103794. ⟨10.1016/j.gloplacha.2022.103794⟩
Global and Planetary Change, Elsevier, 2022, 212, pp.103794. ⟨10.1016/j.gloplacha.2022.103794⟩
Global and Planetary Change, vol. 212, pp. 103794
International audience; The Paleogene records the most prominent global climate change of the Cenozoic Era with a shift from a greenhouse to an icehouse world. Several transient hyperthermal events punctuated this long-term evolution. The most pronou
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8d85e05f012f9e54ec09bce99020b372
https://insu.hal.science/insu-03621183v2/file/1-s2.0-S0921818122000613-main.pdf
https://insu.hal.science/insu-03621183v2/file/1-s2.0-S0921818122000613-main.pdf
The Late Cretaceous Oman Mountains are generally assumed to result from obduction followed by the inversion of the mid-Permian- to Triassic Neotethyan rifted margin. However, the key rift-related crustal features, such as a necking zone or hyper-exte
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::835c8df4e60796a5997633bb365393b1
https://doi.org/10.5194/egusphere-egu22-11305
https://doi.org/10.5194/egusphere-egu22-11305