A 400 Ma-long Nd-Hf isotopic evolution of melt-modified garnet-pyroxenites in an ancient subcontinental lithosphere (Lanzo North ophiolite, Western Alps)

Autor: Sanfilippo A.[1, Borghini G.[3], Guarnieri L.[4], Nakamura E.[5], Piccardo G.B.[4], Vannucci R.[1, Zanetti A.[2]

Publikováno v: Chemical geology 588 (2022). doi:10.1016/j.chemgeo.2021.120643
info:cnr-pdr/source/autori:Sanfilippo A.[1,2], Borghini G.[3], Guarnieri L.[4], Nakamura E.[5], Piccardo G.B.[4], Vannucci R.[1,2], Zanetti A.[2]/titolo:A 400 Ma-long Nd-Hf isotopic evolution of melt-modified garnet-pyroxenites in an ancient subcontinental lithosphere (Lanzo North ophiolite, Western Alps)/doi:10.1016%2Fj.chemgeo.2021.120643/rivista:Chemical geology/anno:2022/pagina_da:/pagina_a:/intervallo_pagine:/volume:588

Pyroxenite veining is widely preserved in peridotite massifs, and used to derive information on the origin and evolution of upper mantle domains. These lithospheric mantle sections can be isolated from the convecting mantle for >1 Ga or more, sufferi

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8faa5c82d8caa39eaf9eff08ed64c5b0
https://publications.cnr.it/doc/462365