Zobrazeno 1 - 5
of 5
pro vyhledávání: '"Mohamed Outhounjite"'
Publikováno v:
The Geological Society, London, Special Publications
The Geological Society, London, Special Publications, Geological Society of London, In press, pp.SP502-2019-65. ⟨10.1144/SP502-2019-65⟩
The Geological Society, London, Special Publications, Geological Society of London, 2020, 502, pp.SP502-2019-65. ⟨10.1144/SP502-2019-65⟩
The Geological Society, London, Special Publications, 2020, 502, pp.SP502-2019-65. ⟨10.1144/SP502-2019-65⟩
The Geological Society, London, Special Publications, Geological Society of London, In press, pp.SP502-2019-65. ⟨10.1144/SP502-2019-65⟩
The Geological Society, London, Special Publications, Geological Society of London, 2020, 502, pp.SP502-2019-65. ⟨10.1144/SP502-2019-65⟩
The Geological Society, London, Special Publications, 2020, 502, pp.SP502-2019-65. ⟨10.1144/SP502-2019-65⟩
International audience
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d2d9f6bd76d97eb71c1c16c09cc30eab
https://hal.archives-ouvertes.fr/hal-02471637/document
https://hal.archives-ouvertes.fr/hal-02471637/document
Autor:
Mohammed Jaffal, Abdelmajid Jarni, El Mostafa Aarab, Mohamed Outhounjite, Omar Guillou, Abdelmalek Ouadjou, El Mostafa Mouguina, Lhou Maacha
Publikováno v:
Arabian Journal of Geosciences. 12
The hercynian Kettara sill located at the central part of the central Jebilet is known for its differentiated mafic-ultramafic rocks. In the southwest part of this massif, there is a magnetic anomaly associated with the mafic-ultramafic rocks. Suscep
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::53db37d8b8f7c835c08b31737cdca897
https://doi.org/10.1007/s12517-018-4183-1
https://doi.org/10.1007/s12517-018-4183-1
Autor:
Mohamed Essaoudi, Larbi Rddad, Essaid El Bachari, Lhou Maacha, Mohamed Outhounjite, Laila Salama, Mohamed Zouhair, El Mostafa Mouguina
Publikováno v:
Arabian Journal of Geosciences. 11
Draa Sfar is a polymetallic (Zn–Pb–Cu) volcanogenic massive sulfide deposit with an actual resource of 13 Mt at 4.0% Zn and 1.3% Pb. It is part of the central Jbilets area known for its several Cu–Zn ore deposits. The ore is hosted in the upper
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d5e004f593dea9c25cf56ce458ef16ef
https://doi.org/10.1007/s12517-018-4126-x
https://doi.org/10.1007/s12517-018-4126-x
Autor:
Lhou Maacha, Abdelali Khalifa, Luc Barbanson, Mohamed Zouhair, Yannick Branquet, Safouane Admou, Mohamed Outhounjite, Lakhlifi Badra
Publikováno v:
Minerals
Minerals, 2018, 8 (10), pp.435. ⟨10.3390/min8100435⟩
Volume 8
Issue 10
Minerals, MDPI, 2018, 8 (10), pp.435. ⟨10.3390/min8100435⟩
Minerals, Vol 8, Iss 10, p 435 (2018)
Minerals, 2018, 8 (10), pp.435. ⟨10.3390/min8100435⟩
Volume 8
Issue 10
Minerals, MDPI, 2018, 8 (10), pp.435. ⟨10.3390/min8100435⟩
Minerals, Vol 8, Iss 10, p 435 (2018)
The genesis of the base-metal massive sulfide deposits hosted within the Moroccan Hercynian Jebilet and Guemassa Massifs is still under debate. No consensus currently exists between the two models that have been proposed to explain the deposits, i.e.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8184a76332a97c02e2c4bcbf8592aed8
https://insu.hal.science/insu-01892401
https://insu.hal.science/insu-01892401
Autor:
Hugo Moreira, Ahmed Touil, Mohamed Hibti, Mohamed Outhounjite, Said Ouirouane, Lhou Maacha, Salah Boukerrou, Hermínio Arias Nalini, Mohamed Zouhair
Publikováno v:
Arabian Journal of Geosciences. 11
The study performed on the host rocks of the Tighardine deposit allows proposing a new lithostratigraphic succession, mainly constituted of three volcanic and volcano–sedimentary units and dolomitic bed and lenses. Volcanic rocks consist mainly of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d9b88cf48e855684990f34dddb54cdff
https://doi.org/10.1007/s12517-017-3375-4
https://doi.org/10.1007/s12517-017-3375-4