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• W2274918009 abstract "Stratigraphic, sedimentological and palaeoenvironmental constraints on the rise of the Urgonian platform in the western Swiss Jura, correlation with the Helvetic Zone of the Alps and the Northern Subalpine Chains (Chartreuse, Vercors). T. Adatte, A. Godet, K.B. Follmi, S. Bodin, E. De Kaenel, A. Arnaud-Vanneau & H. Arnaud.. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . @@ Urgonian carbonate platform to Vocontian Basin correlation (France SE) by means of biostratigraphy. H. Arnaud, A. Arnaud-Vanneau, F. Bastide, G. Massonnat, J. Vermeulen & A. Virgone. . . . . . . . . . . .@@ Expression of the oceanic Anoxic Event 2 in carbonate platform and in hemipelagic basin, example from Mexico and Tibet. B. Bomou, T. Adatte, K.B. Follmi, A. Arnaud-Vanneau, M. Caron, A. Tantawy, D. Fleitmann, V. Matera & Y. Huang. . . . . . . . . . . . . . . . . . . . . . . . . .@@ Impact of meteoric diagenesis on microporous carbonates of the Middle-East. Example from the Mishrif Fm. (Cenomanian Lower Turonian) of Qatar. M. D. De Periere, C. Durlet, E. Vennin, B. Caline, L. Lambert, R. Bourillot, C. Maza, E. Poli & C. Pabian-Goyheneche. . . . . . . . . . . . . . . . . . . . . . . . . @@ The fluvial-marine transition in genetic sequences of the uppermost Albian (Vraconnian) of the Morocccan Atlantic Margin (Agadir area). B. Essafraoui, D. Grosheny, N. Icame, S. Ferry, M. Masrour, M. Aoutem, L. Bulot & C. Lecuyer. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .@@ Sequential organization of a fluvial to marine sedimentary wedge (Upper Hauterivian of the Moroccan Atlantic margin). S. Ferry, M. Masrour & O. Parize. . . . . . . . . . . . . . . . . . . . . . . . . . . @@ Facies partitioning in the prograding genetic sequences of the Subalpine Urgonian carbonate platform. Their relationship to the significance given the Urgonian Rudistid facies. S. Ferry, D. Quesne & M. Khaska. . @@ Stratigraphic ranges of some Tithonian-Berriasian benthic foraminifers and dasycladales. Re-evaluation of their use in identifying this stage boundary in carbonate platform settings. B. Granier & I.I. Bucur. . . @@ New data on the Hawar, Shu'aiba, Bab, and Sabsab regional stages of the Lower Cretaceous in the United Arab Emirates and in Oman. B. Granier, R. Busnardo & B. Pittet. . . . . . . . . @@ The Cenomanian-Turonian transition on a W-E transect of the Moroccan Atlantic margin (Agadir). Isotope geochemistry and sequence stratigraphy. M. Jati, D. Grosheny, S. Ferry & D. Desmares. . . . . .@@ The RGF program (Geologic Reference Map of France): A geodynamic geologic map. E. Lasseur, L. Beccaletto, Y. Callec, R. Coueffe, F. Paquet, J.-P. Platel, O. Serrano & I. Thinon. . . . . . . . @@ OAE1a: late Early or early Late Bedoulian event? M. Moullade, W. Kuhnt, G. Tronchetti, P. Ropolo & B. Granier. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . @@ The Cretaceous carbonate series of the Oman mountains. P. Razin & C. Grelaud. . . . . . @@ @ Grosheny, Granier & Sander Platform to basin correlations in Cretaceous times. STRATIGRAPHIC, SEDIMENTOLOGICAL AND PALAEOENVIRONMENTAL CONSTRAINTS ON THE RISE OF THE URGONIAN PLATFORM IN THE WESTERN SWISS JURA, CORRELATION WITH THE HELVETIC ZONE OF THE ALPS AND THE NORTHERN SUBALPINE CHAINS (CHARTREUSE, VERCORS) Thierry ADATTE, Alexis GODET, Karl B. FOLLMI, Stephane BODIN, Eric De KAENEL, Annie ARNAUD-VANNEAU & Hubert ARNAUD Urgonian-type carbonates are a characteristic feature of growth, a second drowning phase occurred during the latest many late Early Cretaceous shallow-marine, tropical and Hauterivian and Early Barremian, which was accompanied subtropical environments. The presence of typical by important platform erosion and sediment reworking. photozoan carbonate-producing communities including The Late Barremian witnessed the renewed installation of a corals and rudists indicates the prevalence of warm, carbonate platform, which initiated with a phase of oolite transparent and presumably oligotrophic conditions in a production, which progressively evolved into an Urgonianperiod otherwise characterised by the high density of type carbonate production under the inclusion of corals and globally occurring anoxic episodes. Of particular interest, rudists. This phase terminated at the latest in the middle therefore, is the exploration of relationships between Early Aptian, due to a further drowning event. The Urgonian platform growth and palaeoceanographic evolution of this particular platform segment is compatible change. In the French and Swiss Jura Mountains, the onset with that of more distal and well-dated segments of the and evolution of the Urgonian platform have been same northern Tethyan platform preserved in the Helvetic controversially dated, and a correlation with other, better zone of the Alps and in the northern subalpine chains dated successions is correspondingly difficult. It is for this (Chartreuse, Vercors). reason that a series of recently exposed sections were sampled (Eclepens, Vaumarcus, Neuchâtel), in addition to" @default.
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• W2274918009 date "2011-01-07" @default.
• W2274918009 modified "2023-09-25" @default.
• W2274918009 title "PLATFORM TO BASIN CORRELATIONS IN CRETACEOUS TIMES - ABSTRACTS -" @default.
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