Zobrazeno 1 - 10
of 60
pro vyhledávání: '"Michel Sébrier"'
Weak Tectono-Magmatic Relationships along an Obliquely Convergent Plate Boundary: Sumatra, Indonesia
Publikováno v:
Frontiers in Earth Science, Vol 6 (2018)
The tectono-magmatic relationships along obliquely convergent plate boundaries, where strain partitioning promotes strike-slip structures along the volcanic arc, are poorly known. Here it is unclear if and, in case, how the strike-slip structures con
Externí odkaz:
https://doaj.org/article/241da683093347f5976ea23e51a65775
Publikováno v:
Comptes Rendus. Géoscience
Comptes Rendus. Géoscience, 2022, 353 (S1), pp.339-380. ⟨10.5802/crgeos.102⟩
Comptes Rendus. Géoscience, Académie des sciences (Paris), 2021, 353 (S1), pp.339-380. ⟨10.5802/crgeos.102⟩
Comptes Rendus. Géoscience, 2022, 353 (S1), pp.339-380. ⟨10.5802/crgeos.102⟩
Comptes Rendus. Géoscience, Académie des sciences (Paris), 2021, 353 (S1), pp.339-380. ⟨10.5802/crgeos.102⟩
International audience; A critical review is conducted of a selection of paleoseismic works published on, or close to, metropolitan France over the last 30 years. The evolution of these works may be subdivided into three periods: dawn of French paleo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b2074db6f9dc2cb13d0ca02240907ff6
https://hal.science/hal-03573850
https://hal.science/hal-03573850
Publikováno v:
Geological Magazine
Geological Magazine, 2016, 153 (5-6), pp.992-1012. ⟨10.1017/S0016756816000467⟩
Geological Magazine, Cambridge University Press (CUP), 2016, 153 (5-6), pp.992-1012. ⟨10.1017/S0016756816000467⟩
Geological Magazine, 2016, 153 (5-6), pp.992-1012. ⟨10.1017/S0016756816000467⟩
Geological Magazine, Cambridge University Press (CUP), 2016, 153 (5-6), pp.992-1012. ⟨10.1017/S0016756816000467⟩
The Sierras Pampeanas consist of basement uplifts that are mainly controlled by W-verging crustal thrusts. One of these, the Sierra Pie de Palo, is controlled by a blind thrust whose kinematics is debated. We analysed the reverse faults located along
Weak Tectono-Magmatic Relationships along an Obliquely Convergent Plate Boundary: Sumatra, Indonesia
Publikováno v:
Frontiers in Earth Science
Frontiers in Earth Science, Frontiers Media, 2018, 6, pp.3. 〈10.3389/feart.2018.00003〉
Frontiers in Earth Science, Frontiers Media, 2018, 6, pp.3. ⟨10.3389/feart.2018.00003⟩
Frontiers in Earth Science, 2018, 6, pp.3. ⟨10.3389/feart.2018.00003⟩
Frontiers in Earth Science, Vol 6 (2018)
Frontiers in Earth Science (6), 1-20. (2018)
Frontiers in Earth Science, Frontiers Media, 2018, 6, pp.3. 〈10.3389/feart.2018.00003〉
Frontiers in Earth Science, Frontiers Media, 2018, 6, pp.3. ⟨10.3389/feart.2018.00003⟩
Frontiers in Earth Science, 2018, 6, pp.3. ⟨10.3389/feart.2018.00003⟩
Frontiers in Earth Science, Vol 6 (2018)
Frontiers in Earth Science (6), 1-20. (2018)
International audience; The tectono-magmatic relationships along obliquely convergent plate boundaries, where strain partitioning promotes strike-slip structures along the volcanic arc, are poorly known. Here it is unclear if and, in case, how the st
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::969eeee1cb7219ab92a24a9bd69ab20e
https://hal.archives-ouvertes.fr/hal-01780318/document
https://hal.archives-ouvertes.fr/hal-01780318/document
Autor:
Carlos H. Costa, Didier Bourlès, Emilio A. Ahumada, Michel Sébrier, Lionel Siame, Olivier Bellier, Carlos E. Gardini, Hector Cisneros
Publikováno v:
Tectonics. 34:1129-1153
Quaternary tectonic and denudation rates are investigated for an actively growing basement anticline: the Sierra Pie de Palo range, which belongs to the Andean foreland of Northwestern Argentina (28°S–33°S). In this study, a detailed morphometric
Autor:
K. Le Dortz, Régis Braucher, M. Foroutan, Didier Bourlès, B. Meyer, Michel Sébrier, Lucilla Benedetti, H. Nazari
Publikováno v:
Quaternary Geochronology
Quaternary Geochronology, Elsevier, 2012, 11, pp.98-115. ⟨10.1016/j.quageo.2012.02.020⟩
Quaternary Geochronology, 2012, 11, pp.98-115. ⟨10.1016/j.quageo.2012.02.020⟩
Quaternary Geochronology, Elsevier, 2012, 11, pp.98-115. ⟨10.1016/j.quageo.2012.02.020⟩
Quaternary Geochronology, 2012, 11, pp.98-115. ⟨10.1016/j.quageo.2012.02.020⟩
Modelling the evolution of the concentration of in-situ produced cosmogenic nuclides as a function of depth (depth-profile) has been developed to allow determining both the exposure duration and the denudation rate affecting geomorphic features. Howe
Autor:
H. Nazari, Mark D. Bateman, A. Rashidi, M. Foroutan, K. Le Dortz, B. Meyer, Morteza Fattahi, Michel Sébrier
Publikováno v:
Geophysical Journal International. 189:6-18
SUMMARY The Central Iran plateau appears aseismic during the last few millenniums based on instrumental and historical seismic records. Nevertheless, it is sliced by several strike-slip faults that are hundreds of kilometres long. These faults displa
Autor:
A. Rashidi, K. Le Dortz, Morteza Fattahi, Régis Braucher, Didier Bourlès, Mark D. Bateman, Lucilla Benedetti, Michel Sébrier, M. Foroutan, Lionel Siame, B. Meyer, H. Nazari
Publikováno v:
Geophysical Journal International. 185:1147-1174
SUMMARY Be and 36 Cl cosmic ray exposure (CRE) and optically stimulated luminescence (OSL) dating of offset terraces have been performed to constrain the long-term slip rate of the Dehshir fault. Analysis of cosmogenic 10 Be and 36 Cl in 73 surface c
Autor:
M. Ghorashi, H. Nazari, K. Le Dortz, Morteza Fattahi, B. Meyer, Michel Sébrier, Morteza Talebian, M. Foroutan, Mark D. Bateman
Publikováno v:
Terra Nova. 21:417-426
Although sliced by several strike slip faults, a large part of Central Iran remained aseismic during the period of time covered by the instrumental and historical seismic records. Stating the existence of earthquakes in the Holocene is therefore impo
Publikováno v:
Bulletin de la Société Géologique de France. 174:305-317
francaisL'ile de Sulawesi se situe a l'ouest l'archipel indonesien, au niveau de la zone de connexion centre 3 plaque (Pacifique Philippines, Indo-Australie) et le bloc de Sunda, ce dernier ayant une cinematique independante de l'Euraise. La forme pa