Mesozoic and Cenozoic Sequence Stratigraphy of European Basins

Mesozoic and Cenozoic Sequence Stratrigraphy of European Basins - This project was designed to build a documented chronostratigraphic and outcrop record of depositional sequences calibrated across European Basins. Data on standard stages, magnetostratigraphy, and geochronology integrated with high resolution biostratigraphy calibrate the stratigraphic position of depositional sequence boundaries. Higher order eustatic sequences show a significant increase in the number identified. A good portion of the European Mesozoic and Cenozoic succession is set in a sequence stratigraphic context with a better stratigraphic record of its bonding surfaces.
Major Transgressive/Regressive Cycles: The Stratigraphic Signature of European Basin Development
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Published:January 01, 1999
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CiteCitation
Thierry Jacquin, Pierre-Charles de Graciansky, 1999. "Major Transgressive/Regressive Cycles: The Stratigraphic Signature of European Basin Development", Mesozoic and Cenozoic Sequence Stratigraphy of European Basins, Pierre-Charles de Graciansky, Jan Hardenbol, Thierry Jacquin, Peter R. Vail
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Abstract
Four Mesozoic major transgressive/regressive cycles have been recognized within Western European basins. They are named as: (1) Eastern Tethys Cycle, (2) Ligurian Cycle, (3) North Sea Cycle, and (4) North Atlantic Cycle, following the four main phases of rifting that affected the whole Western European Craton and its borders during Mesozoic times. Such cycles are bounded by major unconformities, whose names from oldest to youngest are: Hardegsen or Solling (Scythian), Early Cimmerian (Late Norian), Mid-Cimmerian (Aalenian), Late Cimmerian (Berriasian) and Laramide (Palaeocene). Major transgressive/regressive cycles record outpaces the area of every individual basin, which suggests that local tectonic features...