Zobrazeno 1 - 4
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pro vyhledávání: '"Gilio M.[1"'
Autor:
Gilio M.[1, Scambelluri M.[1], Agostini S.[3], Godard M.[4], Pettke T.[5], Agard P.[6], Locatelli M.[6], Angiboust S.[7]
Publikováno v:
Lithos
Lithos, Elsevier, 2020, 352-353, pp.105308. ⟨10.1016/j.lithos.2019.105308⟩
Lithos (Oslo. Print) 352-353 (2020). doi:10.1016/j.lithos.2019.105308
info:cnr-pdr/source/autori:Gilio M.[1,2], Scambelluri M.[1], Agostini S.[3], Godard M.[4], Pettke T.[5], Agard P.[6], Locatelli M.[6], Angiboust S.[7]/titolo:Fingerprinting and relocating tectonic slices along the plate interface: Evidence from the Lago Superiore unit at Monviso (Western Alps)/doi:10.1016%2Fj.lithos.2019.105308/rivista:Lithos (Oslo. Print)/anno:2020/pagina_da:/pagina_a:/intervallo_pagine:/volume:352-353
Lithos, Elsevier, 2020, 352-353, pp.105308. ⟨10.1016/j.lithos.2019.105308⟩
Lithos (Oslo. Print) 352-353 (2020). doi:10.1016/j.lithos.2019.105308
info:cnr-pdr/source/autori:Gilio M.[1,2], Scambelluri M.[1], Agostini S.[3], Godard M.[4], Pettke T.[5], Agard P.[6], Locatelli M.[6], Angiboust S.[7]/titolo:Fingerprinting and relocating tectonic slices along the plate interface: Evidence from the Lago Superiore unit at Monviso (Western Alps)/doi:10.1016%2Fj.lithos.2019.105308/rivista:Lithos (Oslo. Print)/anno:2020/pagina_da:/pagina_a:/intervallo_pagine:/volume:352-353
International audience; The Lago Superiore Unit (LSU, Monviso Massif, Italian Western Alps) is a section of fossil oceanic lithosphere equilibrated to eclogite facies conditions (550 °C – 2.8 GPa) during Alpine subduction (45–40 Ma). It is cut b
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a43c5b9bcda29c70fbe58e10967a3c8f
https://hal.umontpellier.fr/hal-02510337
https://hal.umontpellier.fr/hal-02510337
Publikováno v:
Journal of petrology
60 (2019): 1229–1262. doi:10.1093/petrology/egz030
info:cnr-pdr/source/autori:Gilio M.[1,2], Scambelluri M.[1,3], Agostini S.[3], Godard M.[4], Peters D.[5,6], Pettke T.[5]/titolo:Petrology and geochemistry of serpentinites associated with the ultra-high pressure Lago di Cignana unit (Italian Western Alps)/doi:10.1093%2Fpetrology%2Fegz030/rivista:Journal of petrology (Print)/anno:2019/pagina_da:1229/pagina_a:1262/intervallo_pagine:1229–1262/volume:60
Gilio, M.; Scambelluri, M.; Agostini, S.; Godard, M.; Peters, Daniel; Pettke, Thomas (2019). Petrology and Geochemistry of Serpentinites Associated with the Ultra-High Pressure Lago di Cignana Unit (ItalianWestern Alps). Journal of petrology, 60(6), pp. 1229-1262. Oxford University Press 10.1093/petrology/egz030
60 (2019): 1229–1262. doi:10.1093/petrology/egz030
info:cnr-pdr/source/autori:Gilio M.[1,2], Scambelluri M.[1,3], Agostini S.[3], Godard M.[4], Peters D.[5,6], Pettke T.[5]/titolo:Petrology and geochemistry of serpentinites associated with the ultra-high pressure Lago di Cignana unit (Italian Western Alps)/doi:10.1093%2Fpetrology%2Fegz030/rivista:Journal of petrology (Print)/anno:2019/pagina_da:1229/pagina_a:1262/intervallo_pagine:1229–1262/volume:60
Gilio, M.; Scambelluri, M.; Agostini, S.; Godard, M.; Peters, Daniel; Pettke, Thomas (2019). Petrology and Geochemistry of Serpentinites Associated with the Ultra-High Pressure Lago di Cignana Unit (ItalianWestern Alps). Journal of petrology, 60(6), pp. 1229-1262. Oxford University Press 10.1093/petrology/egz030
In the Western Alps, the ophiolitic Zermatt–Saas Zone (ZSZ) and the Lago di Cignana Unit (LCU) record oceanic lithosphere subduction to high (540°C, 2·3GPa) and ultra-high pressure (600°C, 3·2GPa), respectively. The top of the Zermatt–Saas Zo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::613242a4b73a4d722be13c6faf498b37
https://publications.cnr.it/doc/465143
https://publications.cnr.it/doc/465143
Autor:
Scambelluri M.[1, Bebout G.E.[2], Belmonte D.[1], Gilio M.[1], Campomenosi N.[1], Collins N.[3], Crispini L.[1]
Publikováno v:
Earth and planetary science letters 441 (2016): 155–166. doi:10.1016/j.epsl.2016.02.034
info:cnr-pdr/source/autori:Scambelluri M.[1,2], Bebout G.E.[2], Belmonte D.[1], Gilio M.[1], Campomenosi N.[1], Collins N.[3], Crispini L.[1]/titolo:Carbonation of subduction-zone serpentinite (high-pressure ophicarbonate; Ligurian Western Alps) and implications for the deep carbon cycling./doi:10.1016%2Fj.epsl.2016.02.034/rivista:Earth and planetary science letters/anno:2016/pagina_da:155/pagina_a:166/intervallo_pagine:155–166/volume:441
info:cnr-pdr/source/autori:Scambelluri M.[1,2], Bebout G.E.[2], Belmonte D.[1], Gilio M.[1], Campomenosi N.[1], Collins N.[3], Crispini L.[1]/titolo:Carbonation of subduction-zone serpentinite (high-pressure ophicarbonate; Ligurian Western Alps) and implications for the deep carbon cycling./doi:10.1016%2Fj.epsl.2016.02.034/rivista:Earth and planetary science letters/anno:2016/pagina_da:155/pagina_a:166/intervallo_pagine:155–166/volume:441
Much of the long-term carbon cycle in solid earth occurs in subduction zones, where processes of devolatilization, partial melting of carbonated rocks, and dissolution of carbonate minerals lead to the return of CO2 to the atmosphere via volcanic deg
Publikováno v:
Rendiconti online Società Geologica Italiana 37 (2015): 61–64.
info:cnr-pdr/source/autori:Scambelluri M.[1], Cannaò E.[1,2], Gilio M.[1], Godard M.[3]/titolo:Petrologic and geochemical role of serpentinite in subduction zones and plate interface domains/doi:/rivista:Rendiconti online Società Geologica Italiana/anno:2015/pagina_da:61/pagina_a:64/intervallo_pagine:61–64/volume:37
info:cnr-pdr/source/autori:Scambelluri M.[1], Cannaò E.[1,2], Gilio M.[1], Godard M.[3]/titolo:Petrologic and geochemical role of serpentinite in subduction zones and plate interface domains/doi:/rivista:Rendiconti online Società Geologica Italiana/anno:2015/pagina_da:61/pagina_a:64/intervallo_pagine:61–64/volume:37
We discuss geochemical tracers in serpentinite for assessing the fluidrock interactions and the element exchange processes experienced by these rocks during subduction. This enables to define the timing of serpentinite accretion to plate interface do
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::a8c936d967ec17775fff7744eaa8de10
https://publications.cnr.it/doc/468028
https://publications.cnr.it/doc/468028