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: PeerJ, 2020, vol. 8, p. e9931
Background: The large-headed turtle Solnhofia parsonsi is known by a handful of specimens from the Late Jurassic of Germany and Switzerland (maybe also France). Solnhofia parsonsi is traditionally regarded as a “eurysternid” Thalassochelydia, a group of small to medium sized, mostly lagoonal or marginal turtles found almost exclusively in the Late Jurassic of Europe. More recently,...
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In: Palaeontologia Electronica, 2017, vol. 20, no. 3, p. 1–14
A new trackway possibly made by a trotting theropod at the Las Hoyas fossil site (Early Cretaceous, Cuenca Province, Spain): Identification, bio-dynamics and palaeoenvironmental implications
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In: Journal of Sedimentary Research, 2015, vol. 85, no. 6, p. 660–682
Porous micritic facies, either primary chalks or resulting from secondary destructive micritization, can constitute important hydrocarbon or water reservoirs. Characterization of reservoir properties and the understanding of factors which controlled the distribution of porosity are of primary interest to evaluate the prospective reserves. Middle and late Oxfordian limestones of the eastern Paris...
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In: New Mexico Museum of Natural History & Science bulletin, 2003, no. 23, p. 1-72
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In: Journal of systematic palaeontology, 2013, p. 1-53
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In: Proceedings of the Yorkshire Geological Society, 2003, vol. 54, no. 3, p. 185-215
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In: Hayashibara Museum of Natural Sciences Research Bulletin, 2010, vol. 3, p. 133-141
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In: GeoResearch Forum, 2000, vol. 6, p. 203-210
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