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La stratigraphie oligo-miocène et la surface d'érosion messinienne en mer Noire,stratigraphie sismique haute résolution
Authors:Hervé Gillet  Gilles Lericolais  Jean-Pierre Rehault  Corneliu Dinu
Institution:1. UMR 6538, Domaines océaniques, IUEM, Technopôle Brest-Iroise, 29280 Plouzané, France;2. Ifremer, Centre de Brest, DRO-GM, BP 70, 29280 Plouzané cedex, France;3. University of Bucharest, Faculty of Geology and Geophysics, Str. Traian Vuia nr. 6, sector 1, 70139 Bucharest, Roumanie
Abstract:The stratigraphy of the Black Sea western margin is revisited through seismic data acquired during two French-Romanian surveys. These data are calibrated by industrial and DSDP drillings; they display several major discontinuities regarded as Tertiary erosional surfaces. The major seismic discontinuity underlines the base of Miocene formations and corresponds to a composite surface including at least three erosional phases ranging from Oligocene to Pontian times. Moreover, a Messinian erosional surface is clearly identified. This is in agreement with the Hsü's proposition Palaeogeogr. Palaeoclimatol. Palaeoecol. 29 (1979) 75–93] suggesting a Messinian sea-level drop of Black Sea related to the Messinian Salinity Crisis described in the Mediterranean Sea. To cite this article: H. Gillet et al., C. R. Geoscience 335 (2003).
Keywords:surface d'érosion  Messinien  mer Noire  sismique haute résolution  stratigraphie sismique  erosional surface  Messinian  Black Sea  high-resolution seismic  seismic stratigraphy
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