Zobrazeno 1 - 10
of 129
pro vyhledávání: '"Marco Herwegh"'
Autor:
Ismay Vénice Akker, Raphael Schneeberger, Marco Herwegh, Nathan Looser, Lukas Aschwanden, Martin Mazurek, Kurt Decker, Andreas Ebert, Marcel Guillong, Stefano M. Bernasconi, Christoph Schrank, Michael W. M. Jones, Andrew Langendam, Herfried Madritsch
Publikováno v:
Swiss Journal of Geosciences, Vol 116, Iss 1, Pp 1-28 (2023)
Abstract The Middle-Jurassic Opalinus Clay is the foreseen host rock for radioactive waste disposal in central northern Switzerland. An extensive drilling campaign aiming to characterize the argillaceous formation resulted in a comprehensive drill co
Externí odkaz:
https://doaj.org/article/fddec887cd82403385799dfd2ccc6769
Autor:
Ismay Vénice Akker, Christoph Schrank, Marco Herwegh, Alfons Berger, Michael Jones, Cameron M. Kewish
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 24, Iss 10, Pp n/a-n/a (2023)
Abstract The exhumed Infrahelvetic Flysch Units in the eastern central Alps in Switzerland are a field analog to modern accretionary wedges at active plate boundaries. In these seismically active convergent settings, water‐saturated sediments under
Externí odkaz:
https://doaj.org/article/73253d56d34f4082a82899a28284e31a
Publikováno v:
Swiss Journal of Geosciences, Vol 115, Iss 1, Pp 1-33 (2022)
Abstract We present a series of analogue models inspired by the geology of the Zürcher Weinland region in the Northern Alpine Foreland Basin of Switzerland to explore the influence of rheological weak, i.e. (partially) ductile layers on the 3D evolu
Externí odkaz:
https://doaj.org/article/4a909b8f194447ee9def5773ebd9eacc
Publikováno v:
Swiss Journal of Geosciences, Vol 114, Iss 1, Pp 1-43 (2021)
Abstract The thermo-kinematic evolution of the eastern Aar Massif, Swiss Alps, was investigated using peak temperature data estimated from Raman spectroscopy of carbonaceous material and detailed field analyses. New and compiled temperature-time cons
Externí odkaz:
https://doaj.org/article/b0518d9bb9624b7eb5daa0f3da8382a7
Autor:
Alfons Berger, Martin Engi, Silja Erne-Schmid, Christoph Glotzbach, Cornelia Spiegel, Rick de Goede, Marco Herwegh
Publikováno v:
Swiss Journal of Geosciences, Vol 113, Iss 1, Pp 1-18 (2020)
Abstract The maximum temperature (Tmax) and subsequent exhumation reflect the relations between advective and conductive heat transport, which in turn depend on the tectonic evolution. To unravel these relations in an orogen, precise Tmax data need t
Externí odkaz:
https://doaj.org/article/8a1aba9f48ed42e695cc90ddb85bb3c9
Publikováno v:
Scientific Reports, Vol 7, Iss 1, Pp 1-10 (2017)
Abstract The crustal-scale geometry of the European Alps has been explained by a classical subduction-scenario comprising thrust-and-fold-related compressional wedge tectonics and isostatic rebound. However, massive blocks of crystalline basement (Ex
Externí odkaz:
https://doaj.org/article/a0dfb31a2f0841e3a64f5f43a90182f3
Inversion and exhumation of crystalline basement units of passive margins is a critical stage of mountain-building processes. With a multi-methodological approach that combines 3D geological modelling and cross-section restoration at different time s
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3738514579e6ded9679334c6f2a1f15a
https://doi.org/10.5194/egusphere-egu23-11654
https://doi.org/10.5194/egusphere-egu23-11654
Fault gouges of granitoid composition represent the principal non-cohesive tectonites within fault zones in the continental crust. The spatial distribution and strength of granitoid fault gouges is therefore crucial for understanding how weak the upp
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::54350a6fc7420a6dc08ae3a4b0f8dbc8
https://doi.org/10.5194/egusphere-egu23-6615
https://doi.org/10.5194/egusphere-egu23-6615
Autor:
Veronica Peverelli, Alfons Berger, Martin Wille, Andreas Mulch, Benita Putlitz, Pierre Lanari, Thomas Pettke, Marco Herwegh
Crustal rocks involved in orogenic processes frequently bear evidence for widespread fluid circulation. The hydration history of the granitic continental crust in inverted passive continental margins is of particular interest, as granitoids experienc
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6c3ab77b50ff95f7413ea2c0334b8798
https://doi.org/10.5194/egusphere-egu23-732
https://doi.org/10.5194/egusphere-egu23-732
On October 05, 2021 an Mw4.0 earthquake struck 6 km south of the village of Arolla, near the tongue of the Arolla Glacier. Almost one year prior to this earthquake, an M3.5 event occurred on November 08, 2020 in the same location. Both earthquakes we
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e088e3a2f8c686bd794788a027c6af2d
https://doi.org/10.5194/egusphere-egu23-12362
https://doi.org/10.5194/egusphere-egu23-12362