The development of late-stage continental breackup: Seismic reflection and borehole evidence from the Danakil depression, Ethiopia

Autor: Bastow I.[1], Booth A.[2], Corti G.[3], Keir D.[4, Magee C.[1], Jackson C.[1], Warren J.[6], Wilkinson J.[7], Lascialfari M.[2]

Publikováno v: Tectonics (Online) 37 (2018): 2848–2862.
info:cnr-pdr/source/autori:Bastow I.[1], Booth A.[2], Corti G.[3], Keir D.[4,5], Magee C.[1], Jackson C.[1], Warren J.[6], Wilkinson J.[7], Lascialfari M.[2]/titolo:The development of late-stage continental breackup: Seismic reflection and borehole evidence from the Danakil depression, Ethiopia/doi:/rivista:Tectonics (Online)/anno:2018/pagina_da:2848/pagina_a:2862/intervallo_pagine:2848–2862/volume:37

During continental breakup, the locus of strain shifts from a broad region of border faulting and ductile plate stretching to a narrow zone of magma intrusion in a young ocean basin. Recent studies of volcanic rifts and margins worldwide suggest this

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http://www.cnr.it/prodotto/i/393526