Výsledky vyhledávání - "Coltorti M.[1]"

From the Middle Triassic Cima Pape complex (Dolomites; Southern Alps) to the feeding systems beneath active volcanoes: Clues from clinopyroxene textural and compositional zoning

Autor: Nardini N.[1], Casetta F.[1, Ickert R.B.[3, Mark D.F.[4, Ntaflos T.[2], Zanetti A.[6], Coltorti M.[1

Publikováno v: Journal of volcanology and geothermal research 422 (2022). doi:10.1016/j.jvolgeores.2021.107459
info:cnr-pdr/source/autori:Nardini N.[1], Casetta F.[1,2], Ickert R.B.[3,4], Mark D.F.[4,5], Ntaflos T.[2], Zanetti A.[6], Coltorti M.[1,7]/titolo:From the Middle Triassic Cima Pape complex (Dolomites; Southern Alps) to the feeding systems beneath active volcanoes: Clues from clinopyroxene textural and compositional zoning/doi:10.1016%2Fj.jvolgeores.2021.107459/rivista:Journal of volcanology and geothermal research/anno:2022/pagina_da:/pagina_a:/intervallo_pagine:/volume:422

Crystal zoning plays a fundamental role in modern volcanology as a key to unravel the geometry and the dynamics of plumbing systems. In this study, a detailed textural and compositional study of clinopyroxene crystals entrained in intrusive, hypabyss

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a70f2f660b8c6fbbb86636d20a102834
http://hdl.handle.net/11392/2478856

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The Variscan subduction inheritance in the Southern Alps Sub-Continental Lithospheric Mantle: Clues from the Middle Triassic shoshonitic magmatism of the Dolomites (NE Italy)

Autor: Casetta F.[1], Ickert R.B.[2, Mark D.F. [3, Giacomoni P.P.[1], Bonadiman C. [1], Ntaflos T.[5], Zanetti A. [6], Coltorti M. [1

Publikováno v: Lithos (Oslo. Print) 380-381 (2021). doi:10.1016/j.lithos.2020.105856 0024-4937
info:cnr-pdr/source/autori:Casetta F.[1], Ickert R.B.[2,3], Mark D.F. [3,4], Giacomoni P.P.[1], Bonadiman C. [1], Ntaflos T.[5], Zanetti A. [6], Coltorti M. [1,7]/titolo:The Variscan subduction inheritance in the Southern Alps Sub-Continental Lithospheric Mantle: Clues from the Middle Triassic shoshonitic magmatism of the Dolomites (NE Italy)/doi:10.1016%2Fj.lithos.2020.105856 0024-4937/rivista:Lithos (Oslo. Print)/anno:2021/pagina_da:/pagina_a:/intervallo_pagine:/volume:380-381

Although often speculated, the link between the Middle Triassic shoshonitic magmatism at the NE margin of the Adria plate and the subduction-related metasomatism of the Southern Alps Sub-Continental Lithospheric Mantle (SCLM) has never been constrain

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=cnr_________::8697cbe8d94e9bf288f57e24e27c81b6
https://publications.cnr.it/doc/443797

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Long-term storage of subduction-related volatiles in Northern Victoria Land lithospheric mantle: Insight from olivine-hosted melt inclusions from McMurdo basic lavas (Antarctica)

Autor: Giacomoni P.P.[1], Bonadiman C.[1], Casetta F.[1], Faccini B.[1], Ferlito C.[2], Ottolini L.[3], Zanetti A.[3], Coltorti M.[1

Publikováno v: Lithos (Oslo. Print) 378-379 (2020): 1–21. doi:10.1016/j.lithos.2020.105826
info:cnr-pdr/source/autori:Giacomoni P.P.[1], Bonadiman C.[1], Casetta F.[1], Faccini B.[1], Ferlito C.[2], Ottolini L.[3], Zanetti A.[3], Coltorti M.[1,4]/titolo:Long-term storage of subduction-related volatiles in Northern Victoria Land lithospheric mantle: Insight from olivine-hosted melt inclusions from McMurdo basic lavas (Antarctica)/doi:10.1016%2Fj.lithos.2020.105826/rivista:Lithos (Oslo. Print)/anno:2020/pagina_da:1/pagina_a:21/intervallo_pagine:1–21/volume:378-379

H2O, CO2, F, Cl and S concentrations in olivine-hosted melt inclusions (MI) from Cenozoic alkaline volcanics of Northern Victoria Land (NVL, Antarctica) were determined by Secondary Ion Mass Spectrometry (SIMS). The most undegassed H2O and CO2 values

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d5c0e078e8aa72c2792fcd1cf8c837b1
http://hdl.handle.net/11392/2426622

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Phlogopite-pargasite coexistence in an oxygen reduced spinel-peridotite ambient

Autor: Bonadiman C.[1, 2, Brombin V.[1, Andreozzi G.B.[4], Benna P.[5], Coltorti M.[1], Curetti N.[5], Faccini B.[1], Merli M.[6], Pelorosso B.[1], Stagno V.[4], Tesauro M.[7, Pavese A.[5]

Publikováno v: Scientific Reports, Vol 11, Iss 1, Pp 1-17 (2021)
Scientific reports (Nature Publishing Group) 11 (2021): 1–17. doi:10.1038/s41598-021-90844-w
info:cnr-pdr/source/autori:Bonadiman C.[1,2,3], Brombin V.[1,2], Andreozzi G.B.[4], Benna P.[5], Coltorti M.[1], Curetti N.[5], Faccini B.[1], Merli M.[6], Pelorosso B.[1], Stagno V.[4], Tesauro M.[7,8], Pavese A.[5]/titolo:Phlogopite-pargasite coexistence in an oxygen reduced spinel-peridotite ambient/doi:10.1038%2Fs41598-021-90844-w/rivista:Scientific reports (Nature Publishing Group)/anno:2021/pagina_da:1/pagina_a:17/intervallo_pagine:1–17/volume:11
Scientific Reports
'Scientific Reports ', vol: 11, pages: 11829-1-11829-17 (2021)
Scientific Reports, 11(1), 1. NLM (Medline)

The occurrence of phlogopite and amphibole in mantle ultramafic rocks is widely accepted as the modal effect of metasomatism in the upper mantle. However, their simultaneous formation during metasomatic events and the related sub-solidus equilibrium

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c74c3643032609092f9953a368315b16
https://hdl.handle.net/1874/412711

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Intraplate magmatism at a convergent plate boundary: The case of the Cenozoic northern Adria magmatism

Autor: Brombin V.[1], Bonadiman C.[1], Jourdan F.[2], Roghi G.[3], Coltorti M.[1], Webb L.E.[4], Callegaro S.[5], Bellieni G.[6], De Vecchi G.[6], Sede R.[1, Marzoli A.[3

Publikováno v: Earth-science reviews 192 (2019): 355–378. doi:10.1016/j.earscirev.2019.03.016
info:cnr-pdr/source/autori:Brombin V.[1], Bonadiman C.[1], Jourdan F.[2], Roghi G.[3], Coltorti M.[1], Webb L.E.[4], Callegaro S.[5], Bellieni G.[6], De Vecchi G.[6], Sede R.[1,6], Marzoli A.[3,6]/titolo:Intraplate magmatism at a convergent plate boundary: The case of the Cenozoic northern Adria magmatism/doi:10.1016%2Fj.earscirev.2019.03.016/rivista:Earth-science reviews/anno:2019/pagina_da:355/pagina_a:378/intervallo_pagine:355–378/volume:192

The complex European–Adria geodynamic framework, which led to the formation of the Alpine belt, is considered responsible for the orogenic magmatism that occurred in the Central Alps along the Periadriatic/Insubric Line (late Eocene–early Oligoce

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a6be5f0574f40f5fff99414592a1c027
https://publications.cnr.it/doc/463572

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