Reactive melt migration controls the trace element budget of the lower oceanic crust: Insights from the troctolite-olivine gabbro association of the Pineto ophiolite (Corsica, France)

Autor: Berno D.[1], Sanfilippo A.[1, Zanetti A.[2], Tribuzio R.[1

Publikováno v: Ofioliti (Bologna) 44 (2019): 71–82. doi:10.4454/ofioliti.v44i2.525
info:cnr-pdr/source/autori:Berno D.[1], Sanfilippo A.[1,2], Zanetti A.[2], Tribuzio R.[1,2]/titolo:Reactive melt migration controls the trace element budget of the lower oceanic crust: Insights from the troctolite-olivine gabbro association of the Pineto ophiolite (Corsica, France)/doi:10.4454%2Fofioliti.v44i2.525/rivista:Ofioliti (Bologna)/anno:2019/pagina_da:71/pagina_a:82/intervallo_pagine:71–82/volume:44

The Pineto gabbroic sequence is a ~ 1.5 km-thick crustal section similar to those forming the oceanic core complexes at modern slow-spreading ridges. The sequence is subdivided into two sectors displaying different bulk compositions. The deeper secto

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=cnr_________::7667da2eee293a9b09dd9a15399f95c3