Zobrazeno 1 - 8
of 8
pro vyhledávání: '"Houssa Ouali"'
The Richat Dome is a huge circular, slightly elliptical depression (~ 40 km in diameter) in the Proterozoic to Cambro-Ordovician sedimentary series of the NE part of the Mauritanian Taoudeni basin. This structure consists of a central zone that corre
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fb6b8ded9ecdfbceade92970e114e148
https://doi.org/10.5194/egusphere-egu21-12995
https://doi.org/10.5194/egusphere-egu21-12995
Autor:
Khalid Amrouch, Otmane Raji, Youssef Ahechach, Muhammad Ouabid, Abderrahmane Soulaimani, Jean-Louis Bodinier, Houssa Ouali
Alkaline complexes are an important target for geological exploration, with both scientific and economic interests. They are host to different types of mineral deposits, such as Rare Earths, igneous phosphates, -and K-rich minerals and rocks. In Moro
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b21ee33a00c916a2e91177ba54d65a66
https://doi.org/10.5194/egusphere-egu21-5091
https://doi.org/10.5194/egusphere-egu21-5091
Autor:
Philippe Münch, Houssa Ouali, Hicham El Messbahi, Hervé Jourde, Olivier Alard, Jean-Louis Bodinier, Jean-Marie Dautria
Publikováno v:
Journal of African Earth Sciences
Journal of African Earth Sciences, Elsevier, 2020, 167, pp.103845. ⟨10.1016/j.jafrearsci.2020.103845⟩
Journal of African Earth Sciences, 2020, 167, pp.103845. ⟨10.1016/j.jafrearsci.2020.103845⟩
Journal of African Earth Sciences, Elsevier, 2020, 167, pp.103845. ⟨10.1016/j.jafrearsci.2020.103845⟩
Journal of African Earth Sciences, 2020, 167, pp.103845. ⟨10.1016/j.jafrearsci.2020.103845⟩
International audience; The small (≈500 km2) Azrou-Timahdite basaltic area (Middle Atlas Magmatic Province, Northern Morocco) lies on a Lias (200-180 Ma) karst plateau of medium altitude (between 1,750 and 1,950 m). This area includes 23 small-size
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::cf60485b642e8d4f5b4e20b7bfd23e99
https://hal.archives-ouvertes.fr/hal-03096077
https://hal.archives-ouvertes.fr/hal-03096077
Autor:
Muhammad Ouabid, Houssa Ouali, Károly Hidas, Hicham El Messbahi, Antonio Acosta-Vigil, Manuel Jesús Román-Alpiste, Carlos J. Garrido, Claudio Marchesi, Jean-Marie Dautria, Jason Harvey
Publikováno v:
Digital.CSIC. Repositorio Institucional del CSIC
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The Meseta Goaïda magmatism, which occurs as gabbro, dolerite and rhyolitic intrusions in the Neoproterozoic basement and Cambrian platform sedimentary series of the Moroccan Hercynian orogen, has been ascribed to the Variscan orogenesis in the late
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::0a81d87f231a08563fd63327938b479d
Autor:
Carlos J. Garrido, Jean-Marie Dautria, Houssa Ouali, Károly Hidas, Claudio Marchesi, Antonio Acosta-Vigil, Manuel Jesús Román-Alpiste, Muhammad Ouabid
Publikováno v:
Precambrian Research
Precambrian Research, Elsevier, 2017, 299, pp.34-57. ⟨10.1016/j.precamres.2017.07.007⟩
Precambrian Research, Elsevier, 2017, 299, pp.34-57. ⟨10.1016/j.precamres.2017.07.007⟩
International audience; Field observations and U–Pb LA–ICP–MS zircon ages of magmatic outcrops in the Goaïda area, south-eastern part of Moroccan Central Massif (Meseta domain), provide firm evidence of Neoproterozoic silicic magmatism in the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d8f5ce4c41c25fd6c8e88c57197f3b16
https://hal.archives-ouvertes.fr/hal-01768800
https://hal.archives-ouvertes.fr/hal-01768800
Publikováno v:
Comptes Rendus Geoscience. 335:425-433
Resume Au Maroc central, le complexe volcanique de Bou-Acila, attribue au Cambrien, se situe au-dessus des calcaires a traces d'Archeocyathides, d'âge Georgien. Malgre le metamorphisme de faible degre qui a affecte ces roches, la texture magmatique
Publikováno v:
Comptes Rendus de l'Académie des Sciences - Series IIA - Earth and Planetary Science. 330:611-616
In northwestern Meseta, the Sidi-Said Maâchou volcanic complex includes dykes, sills and basaltic flows. This volcanism is synchronous with a Paradoxides schist deposit. Most of the rocks have been affected by post-magmatic alteration processes, whi
Publikováno v:
Geological Magazine. 132:321-337
High-grade basic and acidic meta-igneous rocks are widespread in the bimodal amphibolitic—felsic gneiss complexes, which are characteristic formations of the ‘Middle Allochthonous Unit’ from eastern and southern French Massif Central. The metab