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Heavy oxygen recycled into the lithospheric mantle

Autor: Dallai L.[1], Bianchini G.[2], Avanzinelli R.[3, Natali C.[2, Conticelli S. [3, 4

Publikováno v: Scientific Reports, Vol 9, Iss 1, Pp 1-7 (2019)
Scientific Reports
Scientific reports (Nature Publishing Group) 9 (2019). doi:10.1038/s41598-019-45031-3
info:cnr-pdr/source/autori:Dallai L.[1], Bianchini G.[2], Avanzinelli R.[3,4], Natali C.[2,3], Conticelli S. [3,4,5]/titolo:Heavy oxygen recycled into the lithospheric mantle/doi:10.1038%2Fs41598-019-45031-3/rivista:Scientific reports (Nature Publishing Group)/anno:2019/pagina_da:/pagina_a:/intervallo_pagine:/volume:9

Magmas in volcanic arcs have geochemical and isotopic signatures that can be related to mantle metasomatism due to fluids and melts released by the down-going oceanic crust and overlying sediments, which modify the chemistry and mineralogy of the man

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::85fc666aae2a771c25a483fe6d22ee04
http://link.springer.com/article/10.1038/s41598-019-45031-3

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Akademický článek

Enhanced CO 2-mineral sequestration by cyclic hydraulic fracturing and Si-rich fluid infiltration into serpentinites at Malentrata (Tuscany, Italy)

Autor: Boschi, C., Dini, A., Dallai, L., Ruggieri, G., Gianelli, G.

Publikováno v: In Chemical Geology 2009 265(1):209-226

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Forest maintenance residues as fuel to provide energy for a middle school in tuscany

Autor: Capotorto, M., Dallai, L., Maffezzoli, M., Romoli, L., Allesina, G., Pedrazzi, S.

The world interest in reducing CO2 emissions, producing energy by renewable sources and promoting the idea of a circular economy has been increasing during the last years. General public is aware about the importance of green biomass as a local renew

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::276558846cce9ac6645b544c654e9859
https://hdl.handle.net/11380/1265988

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Tight bounds on missing late veneer in early Archean peridotite from triple oxygen isotopes

Autor: Peters S.T.M.[1], Fischer M.B.[1, Pack A.[1], Szilas K.[3], Appel P.W.U.[4], Münker C.[5], Dallai L.[6], Marien C.S.[5]

Publikováno v: Peters, S T M, Fischer, M B, Pack, A, Szilas, K, Appel, P W U, Münker, C, Dallai, L & Marien, C S 2021, ' Tight bounds on missing late veneer in early Archean peridotite from triple oxygen isotopes ', Geochemical Perspectives Letters, vol. 18, pp. 27-31 . https://doi.org/10.7185/geochemlet.2120
Geochemical Perspectives Letters
18 (2021): 27–31. doi:10.7185/geochemlet.2120
info:cnr-pdr/source/autori:Peters S.T.M.[1], Fischer M.B.[1,2], Pack A.[1], Szilas K.[3], Appel P.W.U.[4], Münker C.[5], Dallai L.[6], Marien C.S.[5]/titolo:Tight bounds on missing late veneer in early Archean peridotite from triple oxygen isotopes/doi:10.7185%2Fgeochemlet.2120/rivista:Geochemical Perspectives Letters (Print)/anno:2021/pagina_da:27/pagina_a:31/intervallo_pagine:27–31/volume:18

Oxygen isotopes provide a unique possibility to study Earth's late accretion phase from a lithophile element perspective, because most carbonaceous chondrites - meteorites that likely resemble the composition of the terrestrial late veneer - have mar

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e9c09741a3a9e8f4a56a0ce3aedb5e18
https://curis.ku.dk/ws/files/280556179/GPL2120_noSI.pdf

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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

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

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

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Stable oxygen and carbon isotope composition of holocene mytilidae from the camarones coast (Chubut, argentina). Palaeoceanographic implications

Autor: Boretto G.[1], Zanchetta G.[2, 3, Consoloni I.[2], Baneschi I.[5], Guidi M.[5], Isola I.[6, Bini M.[2, Ragaini L.[2], Terrasi F.[8], Regattieri E.[5], Dallai L.[5, 6

Publikováno v: Water (Basel) 12 (2020). doi:10.3390/w12123464
info:cnr-pdr/source/autori:Boretto G.[1], Zanchetta G.[2,3,4], Consoloni I.[2], Baneschi I.[5], Guidi M.[5], Isola I.[6,7],Bini M.[2,3],Ragaini L.[2], Terrasi F.[8], Regattieri E.[5], Dallai L.[5,6,9]/titolo:Stable Oxygen and Carbon Isotope Composition of Holocene Mytilidae from the Camarones Coast (Chubut, Argentina): Palaeoceanographic Implications/doi:10.3390%2Fw12123464/rivista:Water (Basel)/anno:2020/pagina_da:/pagina_a:/intervallo_pagine:/volume:12
CONICET Digital (CONICET)
Consejo Nacional de Investigaciones Científicas y Técnicas
instacron:CONICET
Water
Volume 12
Issue 12
Water, Vol 12, Iss 3464, p 3464 (2020)

The stable isotope composition of living and of Holocene Mytilidae shells was measured in the area of Camarones (Chubut, Argentina). The most striking results were the high &delta
18O values measured in samples older than ca. 6.1 cal ka BP. In t

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a90dfc525daf971952792b56b6c01d34
http://hdl.handle.net/11573/1577049

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