In: Tree Physiology, 2016, vol. 36, no. 5, p. 562-575
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In: Bulletin of Earthquake Engineering, 2015, vol. 13, no. 4, p. 1073-1095
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In: Contributions to Mineralogy and Petrology, 2015, vol. 170, no. 5-6, p. 1-16
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In: Swiss Journal of Geosciences, 2015, vol. 108, no. 2-3, p. 213-224
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In: Empirical Economics, 2015, vol. 48, no. 3, p. 1233-1266
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In: Swiss Journal of Geosciences, 2015, vol. 108, no. 2-3, p. 305-326
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In: Climatic Change, 2015, vol. 131, no. 2, p. 183-190
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In: Frontiers in Earth Science, 2021, vol. 9, p. 645596
The Opalinus Clay is notable in Switzerland as being the selected host rock for deep geological disposal of radioactive waste. Since the early 1990’s, this argillaceous mudstone formation of Jurassic age has been intensively studied within the framework of national and international projects to characterize its geological, hydrological, mechanical, thermal, chemical, and biological...
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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: Climate of the Past, 2020, vol. 16, no. 2, p. 743–756
The climate of the Southern Hemisphere (SH) is strongly influenced by variations in the El Niño–Southern Oscillation (ENSO) and the Southern Annular Mode (SAM). Because of the limited length of instrumental records in most parts of the SH, very little is known about the relationship between these two key modes of variability over time. Using proxy-based reconstructions and last-millennium...
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