Seismic models of a prograding carbonate platform: Vercors, south-east France

• Published in: Marine and petroleum geology Vol. 11; no. 5; pp. 514 - 527
• Main Authors: Stafleu, Jan, Everts, Arnout J.W., Kenter, Jeroen A.M.
• Format: Journal Article
• Language: English
• Published: Oxford Elsevier Ltd 01.10.1994; Elsevier Science
• Subjects: Applied geophysics; Earth sciences; Earth, ocean, space; Exact sciences and technology; Internal geophysics; Marine; seismic interpretation; seismic models; sequence stratigraphy; Stratigraphy; Drome; France; Europe; Western Europe; France, Rhone-Alpes, Vercors; seismic models; sequence stratigraphy; seismic interpretation; Mesozoic; outcrops; density; P-waves; velocity; seismic profiles; carbonates; seismic response; French Alps; Lower Cretaceous; Vercors; carbonate platforms; two-dimensional models; geometry; photography
• ISSN: 0264-8172; 1873-4073
• DOI: 10.1016/0264-8172(94)90065-5

The southern Vercors area (south-east France) displays superb exposures of a Lower Cretaceous prograding carbonate platform. These exposures allow a geometrical sequence analysis to be combined with detailed outcrop observations. Two-dimensional seismic modelling techniques were used to determine the seismic response of three of these exposures: the Montagnette, the Archiane Valley and the Rocher de Combau. The outcrops display prograding and retreating series of clinoforms interfingering with fine-grained basinal sediments. Photographs from different angles of view, combined with detailed field observations, were used to construct lithological profiles with a resolution of f few metres. P-wave velocities and bulk densities were measured from cored hand specimens and selected values were assigned to lithostratigraphic units in each profile. The vertical incidence modelling technique was then used to compute migrated time sections of reflectivity. These were convolved with source wavelets of different frequencies to produce the final synthetic seismic profiles. None of the modelled outcrop geometries is correctly portrayed seismically at 25–50 Hz frequencies. Not only do the synthetic seismic profiles show less detail, they also show misleading geometries. In most seismic models, for instance, pseudo-unconformities are present that correspond to rapid changes in dip and in facies in outcrop. Furthermore, the seismic tool is not able to resolve between stratal patterns punctuated by unconformities and those with gradual shifts in facies belts accompanied by complex interfingering relationships. This implies that an unconformity recognized on a real seismic line should not automatically be assumed to represent a true stratal unconformity. Large outcrops are often used to show the validity of sequence stratigraphy, a concept mainly based on the analysis of seismic lines. This study, however, shows that there is no one to one relationship between geometries observed in outcrop and in seismic lines. Seismic modelling of outcrops therefore provides a means for evaluating outcrop geometries in terms of seismic stratigraphy.