In: Facies, 2015, vol. 61, no. 4, p. 1-27
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In: Contributions to Mineralogy and Petrology, 2015, vol. 169, no. 4, p. 1-22
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In: Swiss Journal of Geosciences, 2015, vol. 108, no. 2-3, p. 213-224
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In: Swiss Journal of Geosciences, 2015, vol. 108, no. 2-3, p. 327-343
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In: The Depositional Record, 2021, vol. 7, no. 1, p. 25-51
The Opalinus Clay is an argillaceous to silty mudstone formation, notable in Switzerland as the selected host rock for deep geological disposal of radioactive waste. Its upper bounding unit (Passwang Formation and eastern equivalents) is composed of successions of mudstone, sandy bioclastic marl and limestone separated by ooidal ironstone beds. The lithostratigraphic transition is diachronous...
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In: Geologica Carpathica, 2019, vol. 70, no. 4, p. 325–354
A cyclostratigraphic interpretation of peritidal to shallow-marine ramp deposits of the early Middle Triassic (Anisian) Opletnya Member exposed in outcrops along the Iskar River gorge, NW Bulgaria, is presented. Based on facies trends and bounding surfaces, depositional sequences of several orders can be identified. New biostratigraphic data provide a time frame of the studied succession with...
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In: International Journal of Earth Sciences, 2014, vol. 103, no. 4, p. 1059-1082
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In: Swiss Journal of Geosciences, 2014, vol. 107, no. 2-3, p. 349-357
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In: Stratigraphy & Timescales, 2018, vol. 3, p. 151–187
The sedimentary record of ancient shallow-marine carbonate platforms commonly displays a stacking of different facies, which reflects repetitive changes of depositional environments through time. These changes can be induced by external factors such as cyclical changes in climate and/or sea level, but also by internal factors such as lateral migration of sediment bodies and/or changes in the...
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In: Swiss Journal of Geosciences, 2007, vol. 100, no. 3, p. 443-455
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