1. Pertinence of the seismic reprocessing using existing seismic profiles in the Paris Basin.
- Author
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Hanot, F., Quisel, N., Thomas, S., and Rampnoux, N.
- Subjects
CARBON sequestration ,SEISMIC refraction method ,SALINE waters ,AQUIFERS ,DATA analysis - Abstract
Abstract: This study is focused on the pertinence of the seismic reprocessing done in the North-East of Paris Basin in order to define the geometry of the Dogger and Trias reservoirs. The goal of this work was to evaluate the possibilities of storage of CO
2 in the deep saline aquifers of the Paris Basin. This paper presents a new updated vision of the structural map and geology of North-East of Paris Basin. The preliminary phase involved reprocessing of 343 oil seismic lines recorded between 1981 and 1988, adding up to 303 kilometres coming from 10 different surveys. The quality of the existing data was not always good and work was performed to digitize original bands. Data consistency at the different scale was also analysed and checked. Particular attention was applied to the faults of the Dogger and Trias reservoirs and all shallower structure and aquifers up to the surface. The whole set of available data was harmonized through the establishment of a model of static multi-layer correction of the tertiary cover and by the use of adapted deconvolution. The crossings are thus homogeneous knowing that in-depth quality and definition remain dependent on the parameters of recording on the ground and in particular the length of the maximum offset and the distance between traces. Interpretation made it possible to identify the reflectors from the establishment of synthetic seismograms on 3 representative wells. The tops of the following layers were picked: Cenomanian, Gault, Oxfordian, Dogger, Aalenian, medio liassic sandstones, Triassic sandstones, and the metamorphic basement. The structure issued by this interpretation is notably different from that presented by the public sources because of the different density of the profiles taken into account. Explanations of the different interpretations are discussed in the paper. The isochrone maps were converted in-depth on the basis of 38 calibrations per well to illustrate the interpretation. The different layers show smooth deformations but also some faults where continuity and density increases with the depth because of the character inherited from the fault in the basement. Accidents visible are not continuous from the top of Cenomanian and to the top of the Gault, rather they correspond to the fault of Pays de Bray oriented N130 ° and to a meridian accident located in the western part of the study. From the top of Oxfordian, the continuity increases for these accidents. In addition, some oriented North-South faults appear. All the major faults are visible from the Sandstones in Medio Liasic. In addition to antithetic faults in relation with the accidents previously described, other meridian faults appear in the North of the fault of Pays de Bray. It should be indicated uncertainties in the picking of reflectors between the Trias and the basement, many multiples resistant to the processing programs interfering with these events. This project is based on an appropriated density of existing seismic 2D lines. The unequal quality of these acquisitions makes it possible to define structural aspects of the deep layers but does not allow to image possible lateral variations of rock types of the reservoir. [Copyright &y& Elsevier]- Published
- 2011
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