Zobrazeno 1 - 10
of 13
pro vyhledávání: '"Youssef Timoulali"'
Publikováno v:
Geodesy and Geodynamics, Vol 10, Iss 4, Pp 297-306 (2019)
We investigate attenuation scattering and loss properties in Souss basin (SW of High-Atlas) as a transition zone between the High and Anti Atlas ranges. This district consists in a thinned crustal patch with shallow seismicity and loose sedimentary t
Externí odkaz:
https://doaj.org/article/c6853971b2f246aeab96de0e3d939410
Publikováno v:
Geodesy and Geodynamics, Vol 6, Iss 6, Pp 397-408 (2015)
This study presents the outcomes of the local earthquake tomography applied in the Moroccan Atlas domains. A seismic data collected by 36 seismic and a linearized inversion technics are used for determination of local velocity structure. The interpre
Externí odkaz:
https://doaj.org/article/c9780ac69b614552a30bae06ed2af9a7
Autor:
Lahcen El Moudnib, Youssef Timoulali, Abderrahime Nouayti, Mohammed El Abbassi, Mustapha Bouka, Nordine Nouayti, Nadia Mhammdi
Publikováno v:
Modeling Earth Systems and Environment. 9:2407-2423
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e3a4dffd577b9f55c5484e8d7a9cbe1a
https://doi.org/10.1007/s40808-022-01630-0
https://doi.org/10.1007/s40808-022-01630-0
Autor:
Youssef Timoulali, Mohamed El Hilali, Ahmed Hosny, Lahcen El Moudnib, Mustapha Bouiflane, Mimoun Chourak, Said Badrane
Publikováno v:
Mediterranean Geoscience Reviews. 4:537-554
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1e59562bffd40274d95b7e9392309b13
https://doi.org/10.1007/s42990-022-00084-x
https://doi.org/10.1007/s42990-022-00084-x
In Northern Morocco, seismic site effects in general and liquefaction hazard in particular can occur in the event of a major earthquake due to the thick sedimentary cover characterizing the peripheral Neogene basins of the Alboran Sea. An example is
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b50138b34b06be4a46ccf3b2619f0af4
https://doi.org/10.21203/rs.3.rs-1811493/v1
https://doi.org/10.21203/rs.3.rs-1811493/v1
Publikováno v:
Geodesy and Geodynamics, Vol 10, Iss 3, Pp 241-255 (2019)
We investigate sedimentological and tectonic processes at the central High Atlas, in order to understand their functioning and to build a geodynamic model that placed the area in its current geological frame. The analysis used here is based on the nu
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f13d2cc170d03c515b17e57fac700af5
http://www.sciencedirect.com/science/article/pii/S1674984718300624
http://www.sciencedirect.com/science/article/pii/S1674984718300624
Autor:
Taj Benyounes, Rabie El Bardai, Mohamed El Hilali, Mohamed Ahniche, Youssef Timoulali, Sahel Yattara
Publikováno v:
E3S Web of Conferences, Vol 298, p 01002 (2021)
According to historical documents and Moroccan earthquakes catalogs, the coastal zone has suffered in the past from several earthquakes. Understanding how sedimentary basins respond to seismic-wave energy generated by earthquake events is a significa
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4555f1f7f4d0defb93f9a5e37ffd9c0e
https://www.e3s-conferences.org/articles/e3sconf/pdf/2021/74/e3sconf_iccr2021_01002.pdf
https://www.e3s-conferences.org/articles/e3sconf/pdf/2021/74/e3sconf_iccr2021_01002.pdf
Publikováno v:
Journal of African Earth Sciences. 129:195-201
The crustal and mantle structure of the north-eastern part of Egypt and the surrounding area is shown by means of S-velocity maps for depths ranging from zero to 45 km, determined by the regionalization and inversion of Rayleigh-wave dispersion. This
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3b672e06cb90af2cf1d09c10375ae0f9
https://doi.org/10.1016/j.jafrearsci.2017.01.011
https://doi.org/10.1016/j.jafrearsci.2017.01.011
Publikováno v:
Journal of African Earth Sciences. 120:198-207
The High Atlas is a 100 km wide zone defined by E-W to NE-SW trending folds nearly orthogonal to the Atlantic coastline. The major compressional structures in the High Atlas consist of large-scale fold systems which affect Mesozoic and Cainozoic form
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::060171b78edd157a3edbef76a83b6aa5
https://doi.org/10.1016/j.jafrearsci.2016.05.009
https://doi.org/10.1016/j.jafrearsci.2016.05.009
Publikováno v:
Geodesy and Geodynamics, Vol 6, Iss 6, Pp 397-408 (2015)
This study presents the outcomes of the local earthquake tomography applied in the Moroccan Atlas domains. A seismic data collected by 36 seismic and a linearized inversion technics are used for determination of local velocity structure. The interpre
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2b370859d0c4bcce241fb5fd1f606575
https://doi.org/10.1016/j.geog.2015.12.003
https://doi.org/10.1016/j.geog.2015.12.003