Zobrazeno 1 - 4
of 4
pro vyhledávání: '"Jean Verité"'
Autor:
Sabí Peris Cabré, Luis Valero, Jorge E. Spangenberg, Andreu Vinyoles, Jean Verité, Thierry Adatte, Maxime Tremblin, Stephen Watkins, Nikhil Sharma, Miguel Garcés, Cai Puigdefàbregas, Sébastien Castelltort
Publikováno v:
Climate of the Past
Climate of the Past, 2023, 19 (3), pp.533-554. ⟨10.5194/cp-19-533-2023⟩
eISSN
Climate of the Past, 2023, 19 (3), pp.533-554. ⟨10.5194/cp-19-533-2023⟩
eISSN
The early Cenozoic marine sedimentary record is punctuated by several brief episodes ( kyr) of abrupt global warming, called hyperthermals, that have disturbed ocean life and water physicochemistry. Moreover, recent studies of fluvial–deltaic syste
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::153fb3f9f4fd7a44ddd6f24da98ffa33
https://doi.org/10.5194/egusphere-2022-891
https://doi.org/10.5194/egusphere-2022-891
Autor:
Sabí Peris Cabré, Luis Valero, Jorge E. Spangenberg, Andreu Vinyoles, Jean Verité, Thierry Adatte, Maxime Tremblin, Stephen Watkins, Nikhil Sharma, Miguel Garcés, Cai Puigdefàbregas, Sébastien Castelltort
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d65d583872eb163def396f4b5a7dad94
https://doi.org/10.5194/egusphere-2022-891-supplement
https://doi.org/10.5194/egusphere-2022-891-supplement
Publikováno v:
Journal of Glaciology, Vol 69, Pp 860-878 (2023)
Surging and streaming of glaciers are modulated by meltwater availability and pressure which controls mechanical coupling at their beds. Using laboratory-scale experimental modelling and palaeoglaciological mapping, we explore how subglacial drainage
Externí odkaz:
https://doaj.org/article/49b291ac6b6b4f6884e2bda11c064a65
Autor:
Nikhil Sharma, Alexander C. Whittaker, Stephen E. Watkins, Luis Valero, Jean Vérité, Cai Puigdefabregas, Thierry Adatte, Miguel Garcés, François Guillocheau, Sébastien Castelltort
Publikováno v:
Scientific Reports, Vol 13, Iss 1, Pp 1-14 (2023)
Abstract Ancient fluvial deposits typically display repetitive changes in their depositional architecture such as alternating intervals of coarse-grained highly amalgamated (HA), laterally-stacked, channel bodies, and finer-grained less amalgamated (
Externí odkaz:
https://doaj.org/article/e3abd5efa5244fe98b90ca9019b8fc2e