Mantle dynamics and secular variations beneath the East African Rift: Insights from peridotite xenoliths (Mega, Ethiopia)

Autor: Bianchini G.[1, Bryce J.G.[3], Blichert-Toft J.[4], Beccaluva L.[1], Natali C.[1]

Publikováno v: Chemical Geology
Chemical Geology, Elsevier, 2014, 386, pp.49-58. ⟨10.1016/j.chemgeo.2014.07.024⟩
Chemical Geology, 2014, 386, pp.49-58. ⟨10.1016/j.chemgeo.2014.07.024⟩
Chemical geology 386 (2014): 49–58. doi:10.1016/j.chemgeo.2014.07.024
info:cnr-pdr/source/autori:Bianchini G.[1,2], Bryce J.G.[3], Blichert-Toft J.[4], Beccaluva L.[1], Natali C.[1]/titolo:Mantle dynamics and secular variations beneath the East African Rift: Insights from peridotite xenoliths (Mega, Ethiopia)/doi:10.1016%2Fj.chemgeo.2014.07.024/rivista:Chemical geology/anno:2014/pagina_da:49/pagina_a:58/intervallo_pagine:49–58/volume:386

Segments of the Main Ethiopian Rift (MER), a key sector of the East African Rift (EAR) linking the Afar and Turkana depressions, record different stages of lithospheric evolution from initiation to continental break- up and incipient oceanic spreadin

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1fcacaebb91a638365f131b2240350bd
https://hal.archives-ouvertes.fr/hal-02110410