Pyroxenite Layers in the Northern Apennines’ Upper Mantle (Italy)—Generation by Pyroxenite Melting and Melt Infiltration

Autor: Borghini G.[1, 2, 3] Rampone E.[2], Zanetti A.[4], Class C.[3], Cipriani A.[3, Hofmann A.W.[3, Goldstein S.L.[3

Publikováno v: Journal of petrology
57 (2016): 625–653. doi:10.1093/petrology/egv074
info:cnr-pdr/source/autori:Borghini G.[1,2,3] Rampone E.[2], Zanetti A.[4], Class C.[3], Cipriani A.[3,5], Hofmann A.W.[3,6], Goldstein S.L.[3,7]/titolo:Pyroxenite layers in the northern apennines' upper mantle (Italy)-Generation by pyroxenite melting and melt infiltration/doi:10.1093%2Fpetrology%2Fegv074/rivista:Journal of petrology (Print)/anno:2016/pagina_da:625/pagina_a:653/intervallo_pagine:625–653/volume:57

Pyroxenite layers embedded within peridotite represent widespread lithological mantle heterogeneities and are potential components in the mantle source of many oceanic basalts. They can be generated by a variety of magmatic and metamorphic processes.

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::689f1be64981b531548157523195bc5e
https://doi.org/10.1093/petrology/egv074