Zobrazeno 1 - 10
of 40
pro vyhledávání: '"Pauline Souloumiac"'
Publikováno v:
Geosciences, Vol 9, Iss 6, p 257 (2019)
Knowledge of the paleo-stress distribution is crucial to understand the fracture set up and orientations during the tectonic evolution of a basin, and thus the corresponding fluid flow patterns in a reservoir. This study aims to predict the main stre
Externí odkaz:
https://doaj.org/article/54430b621c8a4569b563d240a552e3b6
Large continental strike-slip earthquakes produce spectacular surface deformations. However, ground displacements are only partially measured in comparison with the amount of slip inferred at depth. Relatively few estimates of the proportion of surfa
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::410050a5ca33b93595cefa2c7b5ce831
https://doi.org/10.5194/egusphere-egu23-13616
https://doi.org/10.5194/egusphere-egu23-13616
During large strike-slip earthquakes, the surface displacement can be measured from correlation of satellite images acquired before and after the event. These measurements allow quantifying the total surface displacement and knowing how it distribute
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6e8c2d32fbd2c2b6f5bbfd44c4ab567b
https://doi.org/10.5194/egusphere-egu22-9868
https://doi.org/10.5194/egusphere-egu22-9868
Autor:
Matthias Rosenau, Fabio Corbi, Nadaya Cubas, Francesca Funiciello, Ehsan Kosari, Bertrand Maillot, Giacomo Mastella, Onno Oncken, Michael Rudolf, Pauline Souloumiac, Sarah Visage
Tectonic faults display a range of slip behaviours including continuous and episodic slip covering rates of more than 10 orders of magnitude. To gain insight into the slip behaviour of brittle faults, we performed laboratory stick-slip experiments at
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::78e9df8cae6b51e7b9c97da321de9506
https://doi.org/10.5194/egusphere-egu22-4533
https://doi.org/10.5194/egusphere-egu22-4533
Knowledge of the in-situ stress state is a key factor for any subsurface site characterization and for safe underground geotechnical exploitations. Despite the huge progress in estimating the stress field, understanding the state of stress is still a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::79a1b93f89e3b39ae6c2a97dacf3a077
https://doi.org/10.5194/egusphere-egu22-1324
https://doi.org/10.5194/egusphere-egu22-1324
Publikováno v:
Geology
Geology, Geological Society of America, 2020, 48 (8), pp.844-848. ⟨10.1130/G47115.1⟩
Geology, Geological Society of America, 2020, 48 (8), pp.844-848. ⟨10.1130/G47115.1⟩
Strike-slip faults are generally described as continuous structures, while they are actually formed of successive segments separated by geometrical complexities. Although this along-strike segmentation is known to affect the overall dynamics of earth
Autor:
Sarah Visage, Pauline Souloumiac, Nadaya Cubas, Bertrand Maillot, Solène Antoine, Arthur Delorme, Yann Klinger
Publikováno v:
SSRN Electronic Journal.
Publikováno v:
BSGF - Earth Sciences Bulletin. 194:5
Field observations and seismic interpretations testify that the front of the Jura fold-and-thrust belt is still submitted to compressive deformation, but whether the basement is deforming (thick-skinned) or not (thin-skinned) is an active question. W
Autor:
Sarah Visage, Pauline Souloumiac, Nadaya Cubas, Bertrand Maillot, Solene Antoine, Arthur Delorme, Yann Klinger
Publikováno v:
Tectonophysics. 847:229704
Autor:
Sarah Visage, Arthur Delorme, Bertrand Maillot, Pauline Souloumiac, Nadaya Cubas, Yann Klinger
During large strike-slip earthquakes, the displacement at the ground surface, only partially measured, is often under-estimated in comparison with the amount of slip inferred at depth. The resulting concept of shallow slip deficit is challenged by th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5fd037fd522cd292a2c2b8df25835bf1
https://doi.org/10.5194/egusphere-egu21-13297
https://doi.org/10.5194/egusphere-egu21-13297