Zobrazeno 1 - 7
of 7
pro vyhledávání: '"Ahmed Yaaqoub"'
Autor:
Romano Clementucci, Paolo Ballato, Lionel Siame, Claudio Faccenna, Ahmed Yaaqoub, Abderrahim Essaifi, Laëtitia Leanni, Valery Guillou
Publikováno v:
EGU22
EGU22, 0000, à renseigner, Unknown Region. ⟨10.5194/egusphere-egu22-11675⟩
EGU General Zssembly
EGU General Zssembly, May 2022, Vienna, Austria
EGU22, 0000, à renseigner, Unknown Region. ⟨10.5194/egusphere-egu22-11675⟩
EGU General Zssembly
EGU General Zssembly, May 2022, Vienna, Austria
Topographic relief results from the complex interactions between tectonics and erosional surface processes. The efficiency of surface processes is a function of topographic slopes, bedrock erodibility and climatic conditions. Ancient orogens offers a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::73597fd33864a7f452f79f7dc99a5165
https://hal-insu.archives-ouvertes.fr/insu-03938066
https://hal-insu.archives-ouvertes.fr/insu-03938066
Autor:
Romano Clementucci, Paolo Ballato, Lionel Louis Siame, Matthew Fox, Riccardo Lanari, Andrea Sembroni, Claudio Faccenna, Ahmed Yaaqoub, Abderrahim Essaifi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5cc92b0cefe6e1999f5e71840dff10ea
https://doi.org/10.1002/essoar.10511350.1
https://doi.org/10.1002/essoar.10511350.1
In actively deforming regions, the geometry and evolution of fluvial systems are sensitive to surface uplift, style of deformation and erosion processes. The uplift influences drainages via base level changes, drainage reversals, and capture processe
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::27ceb2feca0e3e321dd92d170f901b7b
https://doi.org/10.5194/egusphere-egu22-6048
https://doi.org/10.5194/egusphere-egu22-6048
Autor:
Romano Clementucci, Paolo Ballato, Lionel L. Siame, Claudio Faccenna, Ahmed Yaaqoub, Abderrahim Essaifi, Laëtitia Leanni, Valery Guillou
Publikováno v:
Earth and Planetary Science Letters
Earth and Planetary Science Letters, 2022, 596, ⟨10.1016/j.epsl.2022.117788⟩
Earth and Planetary Science Letters, 2022, 596, ⟨10.1016/j.epsl.2022.117788⟩
International audience; Topographic relief results from the complex interactions between tectonics and erosional surface processes, which are primarily mediated by bedrock erodibility and climatic conditions. Ancient orogens offer a favourable settin
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::259104731a746e1e131ffca64175119f
https://doi.org/10.1016/j.epsl.2022.117788
https://doi.org/10.1016/j.epsl.2022.117788
The Middle Atlas mountain range represents the northeastern branch of the Atlas system, which spans approximately 2000 km from the Atlantic coast of Morocco to Tunisia. The Atlas system is a prominent example of active intracontinental mountain belts
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d8433ada94376f8a4be9f2938ddce5fe
https://doi.org/10.5194/egusphere-egu21-13646
https://doi.org/10.5194/egusphere-egu21-13646
Autor:
Abderrahim Essaifi, Claudio Faccenna, Romano Clementucci, Lionel Siame, Paolo Ballato, Laëtitia Léanni, Valery Guillou, Ahmed Yaaqoub
Publikováno v:
EGU General Assembly Conference Abstracts (EGU21-12424)
EGU General Assembly Conference Abstracts (EGU21-12424), 2021, Vienna, Austria
EGU General Assembly Conference Abstracts (EGU21-12424), 2021, Vienna, Austria
Rock erodibility plays a central role in setting topographic limits on relief development and is a key parameter in landscape evolution models. However, channel bed erodibility (K) is usually either fixed arbitrary or let varying over a wide range of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::32b71bec5b9d1d02da25c7db4521fbad
https://hal.science/hal-03543483
https://hal.science/hal-03543483
Autor:
Abderrahim Essaifi, Ahmed Yaaqoub, Valery Guillou, Paolo Ballato, Lionel Siame, Laëtitia Léanni, Romano Clementucci, Claudio Faccenna
The topography of the Atlas-Meseta system (Morocco) is the result of Late Cenozoic rejuvenation related to mantle-driven uplift. This recent, large-scale dynamic uplift is testified by the occurrence of uplifted shallow-water marine deposits in the M
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::25effeca374d3ae2b1790a5bd8a0629e
https://doi.org/10.5194/egusphere-egu2020-11770
https://doi.org/10.5194/egusphere-egu2020-11770