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The AAPG/Datapages Combined Publications Database
AAPG Special Volumes
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The group of oil fields discovered in the Neocomian of the Paris basin in the Chateaurenard area represents accumulations of oil under conditions that are not entirely classical. These essentially stratigraphic fields are located in a small Neocomian basin. The sandstone reservoirs, 1-12 m thick, contain nearly fresh water (100 ppm NaCl), characteristic of the entire Paris basin. It seems probable that the oil originated in the underlying Dogger limestones rather than in the thin (60 m) marine layers of the Neocomian itself. Migration would have been by means of north-south faults. Trapping of oil in the lower sandstone reservoir (Griselles sandstone) apparently is in part stratigraphic and in part hydrodynamic.
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