Zobrazeno 1 - 10
of 18
pro vyhledávání: '"Fadl Raad"'
Autor:
Philippe Pezard, Gilles Henry, Laurent Brun, Erwan Le Ber, Fadl Raad, Michel Séranne, Florian Widhen, Andrea Schleifer, Cinzia Bellezza, Fabio Meneghini, Nicolas Brillouet, Denis Neyens, Claudine Lamotte
The Balaruc hydrothermal system is fed both from surrounding karstic carbonates with fresh water outpouring in the nearby Thau lagoon with the Vise source, and at depth along deep regional faults with local springs up to 50°C. This hydrothermal syst
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::24ebbd27a5cbea78e33d2a66cae808d9
https://doi.org/10.5194/iahs2022-484
https://doi.org/10.5194/iahs2022-484
Autor:
Carine Lézin, Agnès Maillard, Francis Odonne, Francisco J. Sierro, Frank Chanier, Virginie Gaullier, Gary Colinet, Luis J. Chueca, Valérie Chavagnac, Fadl Raad
Publikováno v:
Marine and Petroleum Geology. 153:106254
Autor:
Fadl Raad, Philippe Pezard, Cesar Viseras, Francisco J. Sierro, Luis M. Yeste, Javier J. Aguila, Paula Jerez, Andrea Schleifer, Fabio Meneghini, Cinzia Bellezza, Johanna Lofi, Angelo Camerlenghi, Giovanni Aloisi
The Late Miocene deposits in the Sorbas Basin (Spain) have been of an extreme importance in the understanding of the Messinian Salinity Crisis (MSC) events (5.97-5.33 Ma). They consist of four formations. The pre-crisis Abad marls topped by the evapo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3f0245704c883bbddd560b96f7f773a8
https://doi.org/10.5194/egusphere-egu22-8952
https://doi.org/10.5194/egusphere-egu22-8952
Autor:
Agnès Maillard, Fadl Raad, Frank Chanier, Hanneke Heida, Johanna Lofi, Guillem Mas, Daniel Garcia-Castellanos
Publikováno v:
Digital.CSIC. Repositorio Institucional del CSIC
instname
Tectonophysics (0040-1951) (Elsevier BV), 2022-04, Vol. 829, P. 229295 (23p.)
instname
Tectonophysics (0040-1951) (Elsevier BV), 2022-04, Vol. 829, P. 229295 (23p.)
The Balearic Promontory (Spain) is of key importance to understand the tectonic kinematics of the westernmost Mediterranean, because its continued marine sedimentation has recorded the contrasting effects expected from competing geodynamic models pro
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::32ee5afd691f998eb9a7ee528cb28779
http://hdl.handle.net/10261/265603
http://hdl.handle.net/10261/265603
Autor:
Fadl Raad, Gaia Travan, Bruno C. Vendeville, Jacques Déverchère, Johanna Lofi, Virginie Gaullier
The Algerian margin, located in the Western Mediterranean basin, is reactivated in compression since 8 My due to the convergence between Africa and Eurasia, and is nowadays subjected to a N45W compression of several mm/y (Jolivet et al., 1995; Noquet
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::42739d3fd8049f4dbc60743b123d81d4
https://doi.org/10.5194/egusphere-egu21-11948
https://doi.org/10.5194/egusphere-egu21-11948
Autor:
Fadl Raad, Agnès Maillard, Hanneke Heida, Johanna Lofi, Ivone Jimenez-Munt, Daniel García-Castellanos
Publikováno v:
Basin Research
Basin Research, In press, ⟨10.1111/bre.12610⟩
Basin Research, Wiley, In press, ⟨10.1111/bre.12610⟩
Digital.CSIC. Repositorio Institucional del CSIC
instname
Basin research
Basin Research, In press, ⟨10.1111/bre.12610⟩
Basin Research, Wiley, In press, ⟨10.1111/bre.12610⟩
Digital.CSIC. Repositorio Institucional del CSIC
instname
Basin research
During the Messinian Salinity Crisis (MSC, 5.97–5.33 Ma), thick evaporites were deposited in the Mediterranean Sea associated with major margin erosion. This has been interpreted by most authors as resulting from water level drop by evaporation but
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f97e3b45ed81118f1965676e9e68e016
https://hal.science/hal-03402713/file/bre.12610.pdf
https://hal.science/hal-03402713/file/bre.12610.pdf
The Messinian Salinity Crisis (MSC) is a prominent and still misunderstood event that influenced the Mediterranean basin in the late Miocene leaving behind a Salt Giant (SG) widespread all over the Mediterranean basin. More than 90% of the Messinian
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6a44ebdc0dbf0abc7dd8d216ad89162d
https://doi.org/10.5194/egusphere-egu2020-7690
https://doi.org/10.5194/egusphere-egu2020-7690
This study intends to contribute to the understanding of the Mediterranean Salt Giant in the Western Mediterranean, formed about 6 Ma ago during the Messinian Salinity Crisis. It provides reprocessed multichannel seismic reflection data that aim at i
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c9d544b1adc7a2e0a3ad767af295a2da
https://doi.org/10.5194/egusphere-egu2020-13769
https://doi.org/10.5194/egusphere-egu2020-13769
Publikováno v:
Marine and Petroleum Geology
Marine and Petroleum Geology, Elsevier, In press, ⟨10.1016/j.marpetgeo.2020.104777⟩
Marine and Petroleum Geology, In press, ⟨10.1016/j.marpetgeo.2020.104777⟩
Marine and Petroleum Geology, Elsevier, In press, ⟨10.1016/j.marpetgeo.2020.104777⟩
Marine and Petroleum Geology, In press, ⟨10.1016/j.marpetgeo.2020.104777⟩
International audience; The Messinian Salinity Crisis (MSC) is a controversial geological event that influenced the Mediterranean Basin in the late Miocene leaving behind a widespread Salt Giant. Today, more than 90% of the Messinian evaporitic depos
Autor:
Massimo Bellucci, Romain Pellen, Estelle Leroux, François Bache, Marga Garcia, Damien DO COUTO, Fadl Raad, Marina Rabineau, Christian Gorini, Maryline Moulin, Agnès Maillard, Johanna Lofi, Anna del Ben, Angelo Camerlenghi, Jeffrey Poort, Danie Aslanian
Publikováno v:
HAL
Data Base compilation (Western Mediterranean Sea) (Seanoe)
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::e98fb1db144a8b9d07d6f77a1c8fef3b
https://hal.archives-ouvertes.fr/hal-03454460
https://hal.archives-ouvertes.fr/hal-03454460