Zobrazeno 1 - 10
of 674
pro vyhledávání: '"VANNUCCI, R"'
Publikováno v:
In LITHOS February 2018 300-301:136-153
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
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
https://publications.cnr.it/doc/462365
Publikováno v:
In LITHOS 2009 107(1):121-133
Publikováno v:
In LITHOS 2007 99(1):25-44
Publikováno v:
In Chemical Geology 2002 191(1):105-119
Publikováno v:
In Earth and Planetary Science Letters 2000 176(2):185-201
Publikováno v:
In Earth and Planetary Science Letters 1999 168(3):287-299
Publikováno v:
In LITHOS 1 August 2015 230:184-188
Autor:
Neumann E.-R.[1], Abu El-Rus M. A.[2], Tiepolo M.[3], Ottolini L.[3], Vannucci R. [4]Whitehouse M.[5]
Publikováno v:
Journal of petrology
56 (2015): 3–31. doi:10.1093/petrology/egu069
info:cnr-pdr/source/autori:Neumann E.-R.[1], Abu El-Rus M. A.[2], Tiepolo M.[3], Ottolini L.[3],Vannucci R. [4]Whitehouse M.[5]/titolo:Serpentinization and Deserpentinization Reactions in the Upper Mantle beneath Fuerteventura Revealed by Peridotite Xenoliths ..../doi:10.1093%2Fpetrology%2Fegu069/rivista:Journal of petrology (Print)/anno:2015/pagina_da:3/pagina_a:31/intervallo_pagine:3–31/volume:56
56 (2015): 3–31. doi:10.1093/petrology/egu069
info:cnr-pdr/source/autori:Neumann E.-R.[1], Abu El-Rus M. A.[2], Tiepolo M.[3], Ottolini L.[3],Vannucci R. [4]Whitehouse M.[5]/titolo:Serpentinization and Deserpentinization Reactions in the Upper Mantle beneath Fuerteventura Revealed by Peridotite Xenoliths ..../doi:10.1093%2Fpetrology%2Fegu069/rivista:Journal of petrology (Print)/anno:2015/pagina_da:3/pagina_a:31/intervallo_pagine:3–31/volume:56
Mantle xenoliths collected from Fuerteventura, one of the easternmost Canary Islands, exhibit a complex evolutionary history comprising events of depletion, serpentinization, dehydration and melt metasomatism. Each of these events left imprints on bo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::f6ead88c6dc785e2ee6f9e59c5c0bfcf
https://publications.cnr.it/doc/300865
https://publications.cnr.it/doc/300865