In: Cyclostratigraphy : approaches and case histories, 2004, p. 135
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In: Journal of sedimentary research : an international journal of SEPM, 2003, vol. 73, no. 5, p. 756
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In: Sedimentology : the journal of the International Association of Sedimentologists, 2001, vol. 48, p. 117
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In: Palaeogeography, palaeoclimatology, palaeoecology : an international journal for the geo-sciences, 2003, vol. 200, p. 43
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In: Cyclostratigraphy: Approaches and Case Histories, 2004, p. 135-151
The Berriasian Pierre-Châtel Formation in the Swiss and French Jura Mountains is dominated by shallow-marine carbonates that overlie lacustrine and marginal-marine sediments with a major transgressive surface. Detailed facies analysis of five sections allows the definition of elementary and small-scale depositional sequences, which commonly exhibit deepening–shallowing trends. Benthic...
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In: Terra Nova, 2000, vol. 12(6), p. 303
The origin of third-order depositional sequences remains debatable, and in many cases it is not clear whether they were controlled by tectonic activity and/or by eustatic sea-level changes. In Oxfordian and Berriasian-Valanginian carbonate-dominated sections of Switzerland, France, Germany and Spain, high-resolution sequence-stratigraphic and cyclostratigraphic analyses show that the sedimentary...
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In: Palaeogeography, Palaeoclimatology, Palaeoecology, 2003, vol. 200(1-4), p. 43
When quantifying sedimentary processes on shallow carbonate platforms, it is important to know the high-frequency accommodation changes through time. Accommodation changes in cyclic successions are often analysed by simply converting cycle thickness to Fischer plots. This approach is not satisfactory, because it does not account for differential compaction, possible erosion, sea-level fall below...
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