Zobrazeno 1 - 10
of 70
pro vyhledávání: '"PHILIPPE VERNANT"'
Autor:
SEMİH ERGİNTAV, MICHAEL FLOYD, DEMITRIS PARADISSIS, HAYRULLAH KARABULUT, PHILIPPE VERNANT, FREDERIC MASSON, IVAN GEORGIEV, ALİ ÖZGÜN KONCA, UĞUR DOĞAN, ROBERT KING, ROBERT REILINGER
Publikováno v:
Turkish Journal of Earth Sciences. 32:248-261
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c911f142ecf468603167bcd88a209426
https://doi.org/10.55730/1300-0985.1842
https://doi.org/10.55730/1300-0985.1842
Publikováno v:
Geology.
The causes of seismicity in stable continental regions (SCRs) remain an open question, in particular with respect to (1) the transient or steady-state nature of the forcing mechanisms and (2) the bias toward shallow seismicity. In this study, we test
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2acf675336318bb969cf99b0a4a8aaf8
https://doi.org/10.1130/g51327.1
https://doi.org/10.1130/g51327.1
Autor:
Marianne Metois, Axel Periollat, Stéphane Mazzotti, Frédéric Masson, Mathilde Vergnolle, Anne Socquet, Philippe Vernant, Alexis Rigo, Stéphane Baize, Jesús Piña-Valdés, Juliette Grosset
Analysis of lithospheric deformation is key to understanding current tectonics and other active deformation processes. The Alceste project, conducted in the framework of the Résif Seismicity Transverse Action, aims at proposing an updated seismic ha
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6cbe960445f15768c4d622a0bb246d1d
https://doi.org/10.5194/egusphere-egu23-17273
https://doi.org/10.5194/egusphere-egu23-17273
Publikováno v:
eISSN
In regions formerly glaciated during the Last Glacial Maximum (LGM), Glacial Isostatic Adjustment (GIA) explains most of the measured uplift and deformation rates. GIA is also proposed as a key process contributing to fault activity and seismicity sh
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5d5e4819687e0b84f0b4db9b22fd65df
https://doi.org/10.5194/egusphere-2023-538
https://doi.org/10.5194/egusphere-2023-538
Publikováno v:
Solid Earth, Vol 12, Pp 15-34 (2021)
The salt mining industrial exploitation located in Vauvert (France) has been injecting water at high pressure into wells to dissolve salt layers at depth. The extracted brine has been used in the chemical industry for more than 30 years, inducing a s
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a0bcd747c9b3ab748d3a7e0a1d5a2ea4
https://doi.org/10.5194/se-12-15-2021
https://doi.org/10.5194/se-12-15-2021
Publikováno v:
Géomorphologie : relief, processus, environnement. 26:255-264
De nouveaux âges d'enfouissement par mesure des rapports isotopiques 26Al/10Be au sein de trois cavités proches du canyon de la Vis (sud de la France, limite sud-est des Grands-Causses) remettent en question le modèle de karstogenèse classiquemen
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::df7255e3d36b188c1488be21d26de61f
https://doi.org/10.4000/geomorphologie.15043
https://doi.org/10.4000/geomorphologie.15043
Autor:
Adrien Damon, Stéphane Mazzotti, Philippe Vernant, Rémi Vachon, Juliette Grosset, Frédéric Ego, David Baumont
Publikováno v:
SSRN Electronic Journal.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7e2359fb9e3e217986f842074df02ae4
https://doi.org/10.2139/ssrn.4300077
https://doi.org/10.2139/ssrn.4300077
The understanding of the origins of seismicity in intraplate regions is crucial to better characterize seismic hazards. In formerly glaciated regions such as Fennoscandia North America or the Western Alps, stress perturbations from Glacial Isostatic
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e8f6d49a48e790877cc8af9d26bdeb4f
https://doi.org/10.5194/se-2021-141
https://doi.org/10.5194/se-2021-141
In the last decade, geodetic data has become fundamental in studies of active faults, seismicity and seismic hazard. In particular, GNSS strain rates and velocities are used to constrain fault-slip rates and seismicity parameters, on the premise that
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f0acceb46103f0714b4f9505722aa02c
https://doi.org/10.5194/egusphere-egu21-10839
https://doi.org/10.5194/egusphere-egu21-10839