Zobrazeno 1 - 5
of 5
pro vyhledávání: '"Renaud Coueffe"'
Autor:
Jean-Yves Roig, Renaud Coueffe, Guillaume Morin, Cécile Gautheron, Beatrix Heller, Thierry Allard, Silvana Bressan Riffel
Publikováno v:
Goldschmidt2021 abstracts.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::613065e0ef6ea3a9628901e6369b1d34
https://doi.org/10.7185/gold2021.6310
https://doi.org/10.7185/gold2021.6310
Autor:
Frédéric Haurine, Cécile Gautheron, Caroline Sanchez, Renaud Coueffe, Jean-Yves Roig, Rosella Pinna-Jamme
Lateritic peofiles results from weathering processes involving coeval warm temperature and high precipitation seasons rates in intertropical context. Through geological times, the laterite will develop and an indurated duricrust iron oxide enriched h
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::37a4004cb36bf2ab19d7117c6b83bd97
https://doi.org/10.5194/egusphere-egu2020-12777
https://doi.org/10.5194/egusphere-egu2020-12777
Autor:
Damien Calmels, Renaud Coueffe, Cécile Quantin, Jean-Yves Roig, Claire Ansart, Cécile Gautheron, Gaël Monvoisin, Pierre Agrinier
Laterite formations are deep regoliths, up to one hundred of meters thick, that represent about 80% of the global soil volume. Formed under tropical conditions, laterites result from successive chemical weathering reactions over long periods up to te
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fc93da60be3e52a5532984f0a1fb0868
https://doi.org/10.5194/egusphere-egu2020-9521
https://doi.org/10.5194/egusphere-egu2020-9521
Autor:
Beatrix Heller, Renaud Coueffe, Thierry Allard, Silvana Bressan Riffel, Guillaume Morin, Jean-Yves Roig, Cécile Gautheron
Laterites are developing under intense chemical weathering and low physical erosion rates. Despite their large extension at the Earth’s surface, there is still a lack of time constraints for their formation, evolution and relation with climatic cha
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::94d936fa2fb2456abee4789651d62d1e
https://doi.org/10.5194/egusphere-egu2020-11900
https://doi.org/10.5194/egusphere-egu2020-11900
Autor:
Didier Néraudeau, Eric Lasseur, Renaud Coueffe, Denis Vaslet, Cécile Robin, François Guillocheau, Franck Hanot
Publikováno v:
Sedimentary Geology
Sedimentary Geology, Elsevier, 2009, 213 (1-2), pp.1-26. ⟨10.1016/j.sedgeo.2008.10.007⟩
Sedimentary Geology, 2009, 213 (1-2), pp.1-26. ⟨10.1016/j.sedgeo.2008.10.007⟩
Sedimentary Geology, Elsevier, 2009, 213 (1-2), pp.1-26. ⟨10.1016/j.sedgeo.2008.10.007⟩
Sedimentary Geology, 2009, 213 (1-2), pp.1-26. ⟨10.1016/j.sedgeo.2008.10.007⟩
A relative water-depth model for the Chalk of the Paris Basin is proposed, based on the lateral variations of the high-frequency metre-scale cycles, which are characteristic features easily identified in the field. The studied outcrops are the Cenoma
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e813213a729e3148315de42636a03c63
https://doi.org/10.1016/j.sedgeo.2008.10.007
https://doi.org/10.1016/j.sedgeo.2008.10.007