Zobrazeno 1 - 8
of 8
pro vyhledávání: '"Mohamed Bouybaouene"'
Autor:
Domingo G. A. M. Aerden, Thomas P. Farrell, Ethan F. Baxter, Emily M. Stewart, Alejandro Ruiz‐Fuentes, Mohamed Bouybaouene
Acknowledgments The authors would like to thank Ángel Perandrés-Villegas for preparing the thin sections used for this study, Fátima Linares Ordóñez for X-ray computed micro-tomography scanning, Mike Tappa for assistance with thermal ionization
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::22691bf646ec2cbc905889c0956c369a
https://hdl.handle.net/10481/78255
https://hdl.handle.net/10481/78255
Publikováno v:
European Journal of Mineralogy
European Journal of Mineralogy, Copernicus, 2011, 23 (2), pp.157-168. ⟨10.1127/0935-1221/2011/0023-2094⟩
European Journal of Mineralogy, Copernicus, 2011, 23 (2), pp.157-168. ⟨10.1127/0935-1221/2011/0023-2094⟩
International audience; Over 30 graphite aggregates that represent pseudomorphs after diamond were manually extracted from a garnet pyroxenite layer in the Beni Bousera peridotite massif, northern Morocco. The inclusions present in the aggregates wer
Publikováno v:
Lithos. 87:214-234
REE mineralogy was characterized at the micrometer scale (using scanning electron microscopy) in the four tectono-metamorphic units of the Beni Mzala window, Sebtide Complex, Internal Rif, Morocco, which sample a HP-LT metamorphic gradient from subgr
Autor:
Ahmed Chalouan, Mohamed Bouybaouene, André Michard, Raymond Montigny, F. Negro, Bruno Goffé, Omar Saddiqi
Publikováno v:
Comptes Rendus Geoscience. 338:92-114
The internal = northern zones of the Maghrebide belt includes allochthonous massifs that define, together with those from the Betics, Sicily and Calabria, a disrupted ‘Alkapeca’ terrane. In the Rif transect, taking advantage of new thermobarometr
Publikováno v:
Lithos
Lithos, Elsevier, 2014, 208-209, pp.67-80. ⟨10.1016/j.lithos.2014.08.014⟩
Lithos, Elsevier, 2014, 208-209, pp.67-80. ⟨10.1016/j.lithos.2014.08.014⟩
International audience; The presence of variable amounts of amphibole +/- phlogopite in a garnet websterite and a garnet clinopyroxenite from the Beni Bousera peridotite massif provides evidence for post-formation metasomatism. Textural observations
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ec4e93f3b53cf5b5ce9b1a02cdd1b36e
https://hal-insu.archives-ouvertes.fr/insu-01096989
https://hal-insu.archives-ouvertes.fr/insu-01096989
Publikováno v:
Terra Nova. 9:171-174
In the Alboran domain, two crustal-thickening late-orogenic extension cycles are superposed. The importance of the late Alpine thinning of the Alpujarride-Sebtide crustal section on top of the Beni Bousera peridotites is discussed here in metamorphic
Publikováno v:
Lithos
Lithos, Elsevier, 2013, 179, pp.231-248. ⟨10.1016/J.LITHOS.2013.08.023⟩
Lithos, Elsevier, 2013, 179, pp.231-248. ⟨10.1016/J.LITHOS.2013.08.023⟩
A detailed mineralogical and textural study of two pyroxenites from the Beni Bousera massif, a garnet clinopyroxenite (GP) and a garnet clinopyroxenite containing graphite pseudomorphs after diamond (GGP), indicates a strong metamorphic overprint ass
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c2bd9043be4c4980ffe6465549d339c8
https://hal-insu.archives-ouvertes.fr/insu-00933753
https://hal-insu.archives-ouvertes.fr/insu-00933753
In the Rif (northern Morocco) and the Western Betics (southern Spain), the Alboran Domain forms a complex stack of metamorphic nappes including mantle peridotites (Beni Bousera and Ronda). We present in this paper new temperature data obtained in the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5b670f56ed28c51121885d924e8857e3
http://doc.rero.ch/record/32656/files/Negro_Fran_ois-Thermal_structure_of_the_Alboran_Domain-20130716161547-NX.pdf
http://doc.rero.ch/record/32656/files/Negro_Fran_ois-Thermal_structure_of_the_Alboran_Domain-20130716161547-NX.pdf