In: International Journal of Earth Sciences, 2010, vol. 99, no. 1, p. 139-163
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In: Swiss Journal of Geosciences, 2007, vol. 100, no. 3, p. 407-429
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In: International Journal of Earth Sciences, 2010, vol. 99, no. 1, p. 139-163
The Middle Berriasian deposits of the Jura platform in Switzerland and France have already been well studied in terms of high-resolution sequence stratigraphy and different orders of depositional sequences (large-, medium-, and small-scale) have been defined. The hierarchical stacking pattern of the sequences and the time span represented by the investigated interval imply that sea-level...
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In: Sedimentology, 2005, vol. 52(6), p. 1207
During the Late Jurassic, accelerated ocean-floor spreading and associated sea-level rise were responsible for a worldwide transgression, which reached its maximum in the Late Kimmeridgian. In many Western European basins, this major sea-level rise led to the formation of marly and condensed sections. In the Swiss Jura, however, a shallow carbonate platform kept growing and only subtle changes in...
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