Tectono-magmatic Interplay and Related Metasomatism in Gabbros of the Chenaillet Ophiolite (Western Alps)

Autor: Tribuzio R.[1, Manatschal G. [3], Renna M. R.[4], Ottolini L.[2], Zanetti A.[2]

Publikováno v: Journal of petrology
60 (2019): 2483–2508. doi:10.1016/j.gca.2017.07.034
info:cnr-pdr/source/autori:Tribuzio R.[1,2], Manatschal G. [3], Renna M. R.[4], Ottolini L.[2], Zanetti A.[2]/titolo:Tectono-magmatic Interplay and Related Metasomatism in Gabbros of the Chenaillet Ophiolite (Western Alps)/doi:10.1016%2Fj.gca.2017.07.034/rivista:Journal of petrology (Print)/anno:2019/pagina_da:2483/pagina_a:2508/intervallo_pagine:2483–2508/volume:60

The Jurassic Chenaillet ophiolite in the Western Alps consists of a gabbro-mantle association exhumed to the seafloor through detachment faulting and partly covered by basaltic lavas. One of the Chenaillet gabbroic bodies includes mylonites that are

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http://www.cnr.it/prodotto/i/436087