Zobrazeno 1 - 2
of 2
pro vyhledávání: '"Bonazzi M.[1"'
Publikováno v:
Ofioliti (Bologna) 46 (2021): 151–165. doi:10.4454/ofioliti.v46i2.544
info:cnr-pdr/source/autori:Simonetti M.[1], Langone A.[1], Corvò S.[1,2], Bonazzi M.[1,2]/titolo:Triassic-jurassic rift-related deformation and temperature-time evolution of the fossil Adriatic margin: A review from Ossola and Strona di Omegna valleys (Ivrea-Verbano zone)/doi:10.4454%2Fofioliti.v46i2.544/rivista:Ofioliti (Bologna)/anno:2021/pagina_da:151/pagina_a:165/intervallo_pagine:151–165/volume:46
info:cnr-pdr/source/autori:Simonetti M.[1], Langone A.[1], Corvò S.[1,2], Bonazzi M.[1,2]/titolo:Triassic-jurassic rift-related deformation and temperature-time evolution of the fossil Adriatic margin: A review from Ossola and Strona di Omegna valleys (Ivrea-Verbano zone)/doi:10.4454%2Fofioliti.v46i2.544/rivista:Ofioliti (Bologna)/anno:2021/pagina_da:151/pagina_a:165/intervallo_pagine:151–165/volume:46
The direct observation and investigation of rift-related structures at the mesoscale is uncommon. Hence, detailed constraints on the evolution of the main faults and shear zones developed during crustal extension are not always available. The Ivrea-V
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::090841ec098250cc22853d9875155cc5
Autor:
Bonazzi M.[1, Langone A.[2], Tumiati S.[3], Dellarole E.[4], Mazzucchelli M.[2, Giovanardi T.[5], Zanetti A.[2]
Publikováno v:
Geosciences (Basel) 10 (2020): 1–31. doi:10.3390/geosciences10080281
info:cnr-pdr/source/autori:Bonazzi M.[1,2], Langone A.[2], Tumiati S.[3], Dellarole E.[4], Mazzucchelli M.[2,5], Giovanardi T.[5], Zanetti A.[2]/titolo:Mantle-derived corundum-bearing felsic dykes may survive only within the lower (Refractory%2Finert) crust: Evidence from zircon geochemistry and geochronology (Ivrea-Verbano zone, southern Alps, Italy)/doi:10.3390%2Fgeosciences10080281/rivista:Geosciences (Basel)/anno:2020/pagina_da:1/pagina_a:31/intervallo_pagine:1–31/volume:10
Geosciences, Vol 10, Iss 281, p 281 (2020)
Geosciences
Volume 10
Issue 8
info:cnr-pdr/source/autori:Bonazzi M.[1,2], Langone A.[2], Tumiati S.[3], Dellarole E.[4], Mazzucchelli M.[2,5], Giovanardi T.[5], Zanetti A.[2]/titolo:Mantle-derived corundum-bearing felsic dykes may survive only within the lower (Refractory%2Finert) crust: Evidence from zircon geochemistry and geochronology (Ivrea-Verbano zone, southern Alps, Italy)/doi:10.3390%2Fgeosciences10080281/rivista:Geosciences (Basel)/anno:2020/pagina_da:1/pagina_a:31/intervallo_pagine:1–31/volume:10
Geosciences, Vol 10, Iss 281, p 281 (2020)
Geosciences
Volume 10
Issue 8
Corundum-rich (up to 55 vol.%) felsic dykes formed with albite, ±
K-feldspar, ±
hercynite and ±
biotite-siderophyllite cut the lower crustal rocks exposed in the Ivrea&ndash
Verbano Zone (NW Italy). Zircon is an
K-feldspar, ±
hercynite and ±
biotite-siderophyllite cut the lower crustal rocks exposed in the Ivrea&ndash
Verbano Zone (NW Italy). Zircon is an
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::76ff6c5b91c4100019cc29b0d0982bb9
http://www.cnr.it/prodotto/i/459606
http://www.cnr.it/prodotto/i/459606