Morphology, Internal Architecture, Facies Model, and Emplacement Mechanisms of Lava Flows from the Central Atlantic Magmatic Province (CAMP) of the Hartford and Deerfield Basins (USA)

Autor: Abdelhak Moumou, Nasrrddine Youbi, Hind El Hachimi, Khalil El Kadiri, José Madeira, João Mata, Isma Amri, Abdelkarim Ait Baha

Publikováno v: Geosciences, Vol 14, Iss 8, p 204 (2024)

The morphology, internal architecture, and emplacement mechanisms of the Central Atlantic Magmatic Province (CAMP) lava flows of the Hartford and Deerfield basins (USA) are presented. The Talcott, Holyoke, and Hampden formations within the Hartford b

Externí odkaz: https://doaj.org/article/e85aa20819904de1ac360098dcee719c

Microstructural, Mineralogical and Geochemical Characterization of Au-Ag-Pb-Zn Mineralization from Moulay Bou Azza, Morocco

Autor: Mahjoubi, El Mahjoub, ADDI, Mohamed AIT, OULGOR, Ali, KHEBBI, Hicham, Hassane OUAZZANI, OUDY, Ammar, Isma AMRI, Abdelaziz ZERDANE, CHAIB, Mustapha

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::14b59f7678081e2c2d1bd105a480f3ce

The Geological Heritage of the Talassemtane National Park and the Ghomara coast Natural Area (NW of Morocco)

Autor: Soufian Maaté, Saïd Chakiri, Isma Amri, Ali Aoulad-Sidi-Mhend, Manuel Martín-Martín, Rachid Hlila, Ali Maate

The Talassemtane National Park and the Ghomara Coast (TNP-GC) natural area, registered in the list of the exceptional patrimony of Morocco by the UNESCO, are characterized by their great biodiversity integrated in the Intercontinental Biosphere Reser

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::eb1279969c62eda1d029be7da84ee4c9
https://hdl.handle.net/10045/95508

Spatial variability of pyroxenite layers in the Beni Bousera orogenic peridotite (Morocco) and implications for their origin

Autor: Isma Amri, Kamal Targuisti, Kamar Chetouani, Carlos J. Garrido, Jean-Louis Bodinier, Claudio Marchesi

Publikováno v: Comptes Rendus Géoscience
Comptes Rendus Géoscience, Elsevier, 2016, 348 (8), pp.619-629. ⟨10.1016/j.crte.2016.06.001⟩
Comptes Rendus Géoscience, 2016, 348 (8), pp.619-629. ⟨10.1016/j.crte.2016.06.001⟩

The Beni Bousera peridotite contains a diversity of pyroxenite layers. Several studies have postulated that at least some of them represent elongated strips of oceanic lithosphere recycled in the convective mantle. Some pyroxenites were, however, asc

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::db536cdef2bc6394af541abe8f696a38
https://hal.archives-ouvertes.fr/hal-01468018/file/chetouani.pdf

Thermal structure of a fossil mantle diapir inferred from the distribution of mafic cumulates

Autor: Marc Monnereau, Georges Ceuleneer, Isma Amri

Publikováno v: Nature
Nature, Nature Publishing Group, 1996, 379 (6561), pp.149-153. ⟨10.1038/379149a0⟩

MAFIC lithologies constitute a minor but ubiquitous component of the mantle section of ophiolites; they are currently viewed as cumulates left by basaltic melts travelling from the melting region to the surface. These features may be used to constrai

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ac5b8987ac2f5f357599976a63e8444a
https://doi.org/10.1038/379149a0