Aborted propagation of the Ethiopian rift caused by linkage with the Kenyan rift

Autor: Corti G.[1], Cioni R.[2], Franceschini Z.[2], Sani F.[2], Scaillet S.[3], Molin P.[4], Isola I.[5], Mazzarini F.[5], Brune S.[6, Keir D.[2, Erbello A.[9], Muluneh A.[10], Illsley-Kemp F.[6, 11], Glerum A.[6]

Publikováno v: Nature Communications
Nature Communications, Vol 10, Iss 1, Pp 1-11 (2019)
Nature Communications, Nature Publishing Group, 2019, 10, pp.1309. ⟨10.1038/s41467-019-09335-2⟩
Nature communications 10 (2019). doi:10.1038/s41467-019-09335-2
info:cnr-pdr/source/autori:Corti G.[1], Cioni R.[2], Franceschini Z.[2], Sani F.[2], Scaillet S.[3], Molin P.[4], Isola I.[5], Mazzarini F.[5], Brune S.[6,7], Keir D.[2,8], Erbello A.[9], Muluneh A.[10], Illsley-Kemp F.[6,11], Glerum A.[6]/titolo:Aborted propagation of the Ethiopian rift caused by linkage with the Kenyan rift/doi:10.1038%2Fs41467-019-09335-2/rivista:Nature communications/anno:2019/pagina_da:/pagina_a:/intervallo_pagine:/volume:10

Continental rift systems form by propagation of isolated rift segments that interact, and eventually evolve into continuous zones of deformation. This process impacts many aspects of rifting including rift morphology at breakup, and eventual ocean-ri

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::25d351601ef80ab3481201627a5b4dd6
https://hdl.handle.net/11590/347932