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Fernández López, Sixto Rafael ; Henriques, María Helena Paiva ; Mangold, Charles | Taylor & Francis | 2006The Cabo Mondego outcrops exposed along the cliffs, on the western margin of the Iberian Plate, show an expanded stratigraphic section of Lower Bathonian deposits containing abundant ammonoids. Upper Bajocian deposits correspond to similar facie[...]texto impreso
Pavia, Giulio ; Fernández López, Sixto Rafael ; Mangold, Charles | Università degli studi di Milano. Dipartimento di Scienze della Terra "A. Desio" | 2008The uppermost Bajocian to lowermost Bathonian ammonoid succession has been studied in the Bas Auran area in view of choosing one of its sections as the Global Stratotype Section and Point (G.S.S.P.) of the Bathonian Stage. The Bas Auran ammonite[...]texto impreso
Fernández López, Sixto Rafael ; Pavia, Giulio ; Erba, Elisabetta ; Guiomar, Myette ; Henriques, María Helena Paiva ; Lanza, Roberto ; Mangold, Charles ; Olivero, Davide ; Tiraboschi, Daniele | Springer Verlag | 2009The Bathonian Global Stratotype Section and Point (GSSP) is proposed at the base of limestone bed RB071 (bed 23 in Sturani 1967) in the Ravin du Bès Section (43º 57' 38" N, 6º 18' 55" E), Bas-Auran area, “Alpes de Haute Provence” French departme[...]texto impreso
Fernández López, Sixto Rafael ; Pavia, Giulio ; Erba, Elisabetta ; Guiomar, Myette ; Henriques, María Helena Paiva ; Lanza, Roberto ; Mangold, Charles ; Olivero, Davide ; Tiraboschi, Daniele | 2007The Global Boundary Stratotype Section and Point (GSSP) for the base of the Bathonian Stage is proposed at the base of limestone bed RB071 (bed 23 in Sturani 1967) in the Ravin du Bès Section (43º57’38’’N, 6º18’55’’E), Bas-Auran area, in the Cha[...]texto impreso
Olivero, Davide ; Pavia, Giulio ; Fernández López, Sixto Rafael ; Mangold, Charles ; Guiomar, Myette | Bureau de recherches géologiques et minières (France) | 2010Le Bathonien est le troisième étage du Jurassique moyen. Son nom dérive de la « Bath Oolithe », une formation définie près de Bath (Somerset, Angleterre). Mais, dans cette région, les niveaux condensés ne sont pas favorables pour définir le stra[...]texto impreso
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Fernández López, Sixto Rafael ; Pavia, Giulio ; Erba, Elisabetta ; Guiomar, Myette ; Henriques, María Helena Paiva ; Lanza, Roberto ; Mangold, Charles ; Morton, Nicol ; Olivero, Davide ; Tiraboschi, Daniele | 2008The Global Boundary Stratotype Section and Point (GSSP) for the base of the Bathonian Stage is proposed at the base of limestone bed RB071 (bed 23 in Sturani 1967) in the Ravin du Bès Section (43º57’38’’N, 6º18’55’’E), Bas-Auran area, in the Cha[...]texto impreso
Fernández López, Sixto Rafael ; Pavia, Giulio ; Erba, Elisabetta ; Guiomar, Myette ; Henriques, María Helena Paiva ; Lanza, Roberto ; Mangold, Charles ; Morton, Nicol ; Olivero, Davide ; Tiraboschi, Daniele | International Union of Geological Sciences | 2009-12The Bathonian GSSP is defined at the base of limestone bed RB071 in the Ravin du Bès Section, Bas-Auran area, southern Subalpine Chains (France). This section satisfies most of the erquirements recommended by the International Commission on Stra[...]
