In: Swiss Journal of Geosciences, 2017, vol. 110, no. 1, p. 233–251
For this pilot study we used recorded seismic events from the SED permanent network and data from a dedicated SNS network to improve the seismotectonic understanding of very weak seismicity in the vicinity of the Mont Terri underground laboratory. We combined field data on faults with microseismic events and modelling of stress and focal mechanisms. Eighty-six events with very low magnitudes...
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Neuchâtel : Aux Frais de l'auteur ; Soleure : En Commission chez Jent et Gassmann, 1840
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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: Geologica Carpathica, 2018, vol. 69, no. 2, p. 129–148
Sedimentary facies and cycles of the Triassic continental–marine transition of NW Bulgaria are documented in detail from reference sections along the Iskar river gorge between the villages of Tserovo and Opletnya. The depositional environments evolved from anastomosing and meandering river systems in the Petrohan Terrigenous Group to mixed fluvial and tidal settings in the Svidol Formation,...
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In: Chemical Geology, 2010, vol. 277, no. 1-2, p. 70-77
In this study, we present first results from an ongoing investigation on the stable barium (Ba) isotope fractionation in the natural barium cycle. Stable Ba isotope signatures of international IAEA reference materials (synthetic barium sulfate, IAEA-SO-5, -6, and barium carbonate, IAEA-CO-9), natural Ba minerals and experimental Ba precipitates have been analyzed as a first approach to evaluate...
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In: Tectonics, 2019, vol. 38, no. 12, p. 4399–4425
The western margin of the Caribbean Plate is a typical example where oceanic and continental terranes have amalgamated by subduction, collision, and strike‐slip processes. The boundaries between these blocks, as well as their tectonostratigraphic records, are generally covered by younger deposits and dense tropical vegetation, which may hamper reconstructing the accretionary evolution of...
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In: Vallesia : bulletin annuel de la Bibliothèque et des Archives cantonales du Valais, des Musées de Valère et de la Majorie = Jahrbuch der Walliser Kantonsbibliothek, des Staatsarchivs und der Museen von Valeria und Majoria, 1995, p. LIII-LV
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In: Bulletin de la Murithienne, 1980, no. 97, p. 101-170
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In: Acta Carsologica, 2007, vol. 36, no. 1, p. 53-68
Progress in the understanding of cave genesis processes, as well as the intensive research carried out in the Alps during the last decades, permit to summarize the latest knowledge about Alpine caves. The phreatic parts of cave systems develop close to the karst water table, which depends on the spring position, which in turn is generally related to the valley bottom. Thus, caves are directly...
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In: Zubía, 2003, vol. 21, p. 175-186
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