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pro vyhledávání: '"David Essing"'
Autor:
Mechita C. Schmidt-Aursch, Vera Schlindwein, David Essing, Céline Hadziioannou, Simon Stähler
Publikováno v:
Seismological Research Letters. 92:3100-3112
Long-lasting harmonic tremor signals are frequently observed in spectrograms of seismological data. Natural sources, such as volcanoes and icebergs, or artificial sources, such as ships and helicopters, produce very similar harmonic tremor episodes.
The Alto Tiberina fault (ATF) system (Northern Apennines, Italy) is dominated by a low-angle normal fault with syn- and antithetic splay faults located in the hanging wall. Starting in August 2013 the hanging wall has been affected by a swarm-like se
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2331748508029f96f628baf92ba65df8
https://doi.org/10.5194/egusphere-egu21-10143
https://doi.org/10.5194/egusphere-egu21-10143
Publikováno v:
Seismological Research Letters
Seismological Research Letters, Seismological Society of America, In press, ⟨10.1785/0220200253⟩
Seismological Research Letters, Seismological Society of America, 2021, 92 (3), pp.1926-1936. ⟨10.1785/0220200253⟩
Seismological Research Letters, In press, ⟨10.1785/0220200253⟩
Seismological Research Letters, Seismological Society of America, In press, ⟨10.1785/0220200253⟩
Seismological Research Letters, Seismological Society of America, 2021, 92 (3), pp.1926-1936. ⟨10.1785/0220200253⟩
Seismological Research Letters, In press, ⟨10.1785/0220200253⟩
Foreshocks in the form of microseismicity are among the most powerful tools to study the physical processes that occur before main earthquakes. However, their detection and precise characterization is still sparse, especially for small-to-moderate-si
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b6d26d08cc6ce08b584c4d04ae3689a2
https://hal.univ-grenoble-alpes.fr/hal-03197363/document
https://hal.univ-grenoble-alpes.fr/hal-03197363/document
Our knowledge about the physics behind the initiation process of large or small earthquakes remains limited. The current understanding of this process suggests that an earthquake occurs when increasing stress causes a pre-existing fault to fail sudde
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b48e45d34fc521de939e166db141a509
Autor:
Franziska Mehrkens, Lucie Rolland, Claudia Haindl, Christoph Schröer, Andre Lamert, Ingrid Daubar, Jiaxuan Li, Katharina Grunert, David Ambrois, Marc S. Boxberg, Thomas Möller, Paul Neumann, Harriet Godwin, Mélanie Drilleau, Raphaël F. Garcia, Sarah Mader, Martin van Driel, Mark P. Panning, Sharon Kedar, Titus Casademont, Matthew P. Golombek, Domenico Giardini, Amir Allam, Bruce Banerdt, Jérôme Chèze, Diego Mercerat, Simon Stähler, Dirk Becker, Lorenz Marten, Hector Alemany, John Clinton, Philippe Lognonné, Eléonore Stutzmann, Savas Ceylan, Balthasar Kenda, Isabell Hochfeld, Kasra Hosseini, Hao Hu, Fabrice Peix, David Essing, Fabian Dethof, T. Garth, Benjamin Fernando, Aymeric Spiga, Robert Neurath, Fabian Euchner, Shane Zhang, Tabea Kilchling, Julien Balestra, Nienke Brinkman, Marcel Paffrath, Brigitte Knapmeyer-Endrun, Martin Schimmel, Maren Böse, Yingcai Zheng, Manuel Ditz, Cedric Twardzik, Alexandre Szenicer, Céline Hadziioannou, Naomi Murdoch, Renee Weber, Anne Deschamps, David Mimoun, René Steinmann, Noah Trumpik, Philipp Werdenbach‐Jarklowski, Maria Tsekhmistrenko, Amir Khan, Conny Hammer, Ludovic Perrin
Publikováno v:
Seismological Research Letters, 90 (4)
Seismological Research Letters
Seismological Research Letters, Seismological Society of America, 2019, 90 (4), pp.1518-1534. ⟨10.1785/0220180379⟩
Seismological Research Letters, 2019, 90 (4), pp.1518-1534. ⟨10.1785/0220180379⟩
Digital.CSIC. Repositorio Institucional del CSIC
instname
Seismological Research Letters
Seismological Research Letters, Seismological Society of America, 2019, 90 (4), pp.1518-1534. ⟨10.1785/0220180379⟩
Seismological Research Letters, 2019, 90 (4), pp.1518-1534. ⟨10.1785/0220180379⟩
Digital.CSIC. Repositorio Institucional del CSIC
instname
In December 2018, the National Aeronautics and Space Administration (NASA) Interior exploration using Seismic Investigations, Geodesy and Heat Transport (InSight) mission deployed a seismometer on the surface of Mars. In preparation for the data anal
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b169e4ece8147361dc29e93d81180caa
https://hdl.handle.net/20.500.11850/346386
https://hdl.handle.net/20.500.11850/346386
Autor:
David Essing, Piero Poli
Publikováno v:
Journal of Geophysical Research : Solid Earth
Journal of Geophysical Research : Solid Earth, 2022, 127, ⟨10.1029/2022JB024845⟩
JGR
Journal of Geophysical Research : Solid Earth, 2022, 127, ⟨10.1029/2022JB024845⟩
JGR
International audience; The Alto Tiberina Fault system, located in the Northern Apennines (Italy), consists of a low angle normal fault (LANF) which radiates micro-seismicity that can be explained by continuous creep. On top of the LANF, a network of