Zobrazeno 1 - 3
of 3
pro vyhledávání: '"Mazzucchelli M.[2"'
Autor:
Giovanardi T.[1, Zanetti A.[3], Dallai L.[4], Morishita T.[5], Hemond C.[6], Mazzucchelli M[2
Publikováno v:
Lithos (Oslo. Print) 356-357 (2020): 1–16. doi:10.1016/j.lithos.2020.105366
info:cnr-pdr/source/autori:Giovanardi T.[1,2], Zanetti A.[3], Dallai L.[4], Morishita T.[5], Hemond C.[6], Mazzucchelli M[2,3]/titolo:Evidence of subduction-related components in sapphirine-bearing gabbroic dykes (Finero phlogopite-peridotite): Insights into the source of the Triassic-Jurassic magmatism at the Europe-Africa boundary/doi:10.1016%2Fj.lithos.2020.105366/rivista:Lithos (Oslo. Print)/anno:2020/pagina_da:1/pagina_a:16/intervallo_pagine:1–16/volume:356-357
info:cnr-pdr/source/autori:Giovanardi T.[1,2], Zanetti A.[3], Dallai L.[4], Morishita T.[5], Hemond C.[6], Mazzucchelli M[2,3]/titolo:Evidence of subduction-related components in sapphirine-bearing gabbroic dykes (Finero phlogopite-peridotite): Insights into the source of the Triassic-Jurassic magmatism at the Europe-Africa boundary/doi:10.1016%2Fj.lithos.2020.105366/rivista:Lithos (Oslo. Print)/anno:2020/pagina_da:1/pagina_a:16/intervallo_pagine:1–16/volume:356-357
A gabbroic dyke swarmcontaining magmatic sapphirine occurs in the Finero phlogopite-peridotite (FPP), one of themajor mantle massifs in the Ivrea-Verbano Zone (IVZ;western Southern Alps). Sapphirine is part of a particular mineral assemblage, includi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::bc37dd3f4e7acc8ec158bbf1a4613da1
https://hdl.handle.net/11380/1187194
https://hdl.handle.net/11380/1187194
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
Autor:
Ponce A.D.[1], Bertotto G.W.[1], Zanetti A.[2], Brunelli D.[3, Giovanardi T.[3, Aragon E. [6], Bernardi M.I.[1], Hemond C.[7] Mazzucchelli M.[2
Publikováno v:
Open Geosciences 7 (2015): 362–385. doi:10.1515/geo-2015-0023
info:cnr-pdr/source/autori:Ponce A.D.[1], Bertotto G.W.[1], Zanetti A.[2], Brunelli D.[3,4], Giovanardi T.[3,5], Aragon E. [6], Bernardi M.I.[1], Hemond C.[7] Mazzucchelli M.[2,3]/titolo:Short-scale variability of the SCLM beneath the extra-Andean back-arc (Paso de Indios, Argentina): Evidence from spinel-facies mantle xenoliths/doi:10.1515%2Fgeo-2015-0023/rivista:Open Geosciences/anno:2015/pagina_da:362/pagina_a:385/intervallo_pagine:362–385/volume:7
Open Geosciences, Vol 7, Iss 1 (2015)
Open Geosciences (2391-5447) (Sciendo), 2015-01, Vol. 7, N. 1, P. 362-385
CONICET Digital (CONICET)
Consejo Nacional de Investigaciones Científicas y Técnicas
instacron:CONICET
SEDICI (UNLP)
Universidad Nacional de La Plata
instacron:UNLP
info:cnr-pdr/source/autori:Ponce A.D.[1], Bertotto G.W.[1], Zanetti A.[2], Brunelli D.[3,4], Giovanardi T.[3,5], Aragon E. [6], Bernardi M.I.[1], Hemond C.[7] Mazzucchelli M.[2,3]/titolo:Short-scale variability of the SCLM beneath the extra-Andean back-arc (Paso de Indios, Argentina): Evidence from spinel-facies mantle xenoliths/doi:10.1515%2Fgeo-2015-0023/rivista:Open Geosciences/anno:2015/pagina_da:362/pagina_a:385/intervallo_pagine:362–385/volume:7
Open Geosciences, Vol 7, Iss 1 (2015)
Open Geosciences (2391-5447) (Sciendo), 2015-01, Vol. 7, N. 1, P. 362-385
CONICET Digital (CONICET)
Consejo Nacional de Investigaciones Científicas y Técnicas
instacron:CONICET
SEDICI (UNLP)
Universidad Nacional de La Plata
instacron:UNLP
Cenozoic basalts carrying ultramafic mantle xenoliths occur in the Matilde, León and Chenque hills in the Paso de Indios region, Argentina. The mantle xenoliths from the Chenque and León hills mainly present porphyroclastic textures, whereas the Ma
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::85e3369b82f0dbb41880ebee921aceb8
http://www.cnr.it/prodotto/i/345642
http://www.cnr.it/prodotto/i/345642