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The North European Platform is a geological region characterized by relatively undeformed or weakly deformed sedimentary rocks dating from the beginning of the Paleozoic Era to the present. This contrasts with surrounding orogenic belts where similar sediments are heavily deformed.12

This platform includes the Russian Platform, where Paleozoic, Mesozoic, and Cenozoic sediments remain nearly horizontal. Further west, in areas like southeastern England and northern France, the North European Platform's Mesozoic and early Cenozoic sediments show weak deformation into anticlines and synclines due to the southern Alpine orogeny. These relatively undisturbed layers make the region valuable for finding well-preserved Phanerozoic fossils. The North Sea is a submarine sedimentary basin on this platform's continental margin, containing significant gas and oil reserves.12

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