The Furongian to Lower Ordovician Alum Shale Formation in conventional and unconventional petroleum systems in the Baltic Basin – A review
Résumé
The organic carbon-and uranium-rich, marine Alum Shale Formation Formation in northwestern Europe (Middle Cambrian, Miaolingian to Early Ordovician) was deposited in the Baltic Basin and surrounding areas. It is a proven source rock for conventional oil either in sandstones of Cambrian age or Ordovician and Silurian carbonates, and also contains a potential for shale oil and for biogenic or thermogenic shale gas.
Domaines
Planète et Univers [physics]
Origine : Fichiers produits par l'(les) auteur(s)