In: Facies, 2005, vol. 51, no. 1-4, p. 264-274
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In: International Journal of Earth Sciences, 2010, vol. 99, no. 1, p. 139-163
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In: Swiss Journal of Geosciences, 2011, vol. 104, no. 2, p. 299-322
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In: Swiss Journal of Geosciences, 2011, vol. 104, no. 2, p. 299-322
Sediment production and accumulation on shallow carbonate platforms are controlled by allogenic, externally controlled processes (such as sea level, climate, and/or platform-wide subsidence patterns) as well as by autogenic factors that are inherent to the sedimentary system (such as lateral migration of sediment bodies). The challenge is to determine how and in which proportion these...
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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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Thèse de doctorat : Université de Fribourg, 2007 ; no 1550.
Le but de cette étude est de corréler et d’interpréter les dépôts transgressifs de trois différentes zones de dépôt avec haute résolution: les carbonates marginaux de la plate-forme du Jura (Suisse et France) et de la région du Dorset (Angleterre). En plus, une coupe hémipélagique du bassin Vocontien (France) a été intégrée dans le schéma de corrélation haute résolution. La...
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In: Facies, 2005, vol. 51, p. 264
Peloids are ubiquitous components in modern and fossil carbonates. The term peloid is non-genetic because the origin of these grains and the pathways of their formation are not fully understood. Based on Berriasian material originating from Dorset, southern England, we report here on peloids that result from the more or less in-place breakdown of previously micritized bivalve shells. The...
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