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- W2012971533 abstract "Le contexte lithostratigraphique et structural, la chronologie et la géochimie du volcanisme andésitique tertiaire de Cap-d'Ail (Alpes-Maritimes, France) sont précisés grâce aux nouvelles données acquises pendant les travaux de mise en souterrain du réseau ferré entre Cap-d'Ail et Monaco. Deux événements magmatiques distincts sont mis en évidence sur le site, l'un paléogène, l'autre néogène. Pour citer cet article : J.-P. Ivaldi et al., C. R. Geoscience 335 (2003). Lithostratigraphic and structural framework, chronology and geochemistry of the Tertiary calc-alkaline volcanism of Cap-d'Ail (French Maritime Alps) are specified according to the new data collected during the earthworks of the recent railway tunnel built between Cap-d'Ail and Monaco. Two different magmatic events were dated: the first one, to Palaeogene, the other one, to Neogene. To cite this article: J.-P. Ivaldi et al., C. R. Geoscience 335 (2003)." @default.
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- W2012971533 date "2003-04-01" @default.
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- W2012971533 title "Contexte lithostructural, âges 40K40Ar et géochimie du volcanisme calco-alcalin tertiaire de Cap-d'Ail dans le tunnel ferroviaire de Monaco" @default.
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- W2012971533 doi "https://doi.org/10.1016/s1631-0713(03)00061-0" @default.
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