Výsledky vyhledávání - "CLOCCHIATTI R."

IAB-type versus OIB-like magmas in the Marsili back-arc Basin (Southern Tyrrenhian): a melt inclusion approach

Autor: TRUA T. (1), MARANI M. (2), CLOCCHIATTI R. (3), OTTOLINI L. (4), GAMBERI F. (2)

Publikováno v: Rendiconti online Società Geologica Italiana 2 (2008).
info:cnr-pdr/source/autori:TRUA T. (1), MARANI M. (2), CLOCCHIATTI R. (3), OTTOLINI L. (4), GAMBERI F. (2)/titolo:IAB-type versus OIB-like magmas in the Marsili back-arc Basin (Southern Tyrrenhian): a melt inclusion approach/doi:/rivista:Rendiconti online Società Geologica Italiana/anno:2008/pagina_da:/pagina_a:/intervallo_pagine:/volume:2

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=cnr_________::dfb607f99c2726fb001722c28e81d77f
http://www.cnr.it/prodotto/i/196784

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Trace element and isotopic variations among Marsili seamount back-arc magmas: constraints for African mantle inflow beneath the Southern Tyrrhenian basin

Autor: TRUA T. (1), MARANI M. (2), SERRI G. (1), CLOCCHIATTI R. (3), OTTOLINI L. (4), GAMBERI F. (2)

Publikováno v: Geoitalia 2007, 6° Forum italiano di Scienze della Terra, pp. 145–145, Rimini, 12-14 settembre 2007
info:cnr-pdr/source/autori:TRUA T. (1), MARANI M. (2), SERRI G. (1), CLOCCHIATTI R. (3), OTTOLINI L. (4), GAMBERI F. (2)/congresso_nome:Geoitalia 2007, 6° Forum italiano di Scienze della Terra/congresso_luogo:Rimini/congresso_data:12-14 settembre 2007/anno:2007/pagina_da:145/pagina_a:145/intervallo_pagine:145–145

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=cnr_________::9bf172d3a98a03bc513e33e72054090b
http://www.cnr.it/prodotto/i/196797

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Environmental impact of the acid fumarole plume of a passively degassing volcano (Vulcano Island, Italy)

Autor: Fulignati, Paolo, Sbrana, Alessandro, Clocchiatti, R, Luperini, W.

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=od______3728::bbb43a8f7a73f46fc9076d46d21016eb
http://hdl.handle.net/11568/205197

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Snapshots fo the magma plumbing system from melt inclusions and residual peridotites of the Vema Lithospheric Section (MAR 11°N)

Autor: Brunelli, Daniele, Clocchiatti, R., Cipriani, Anna, Ligi, M., Paganelli, E., Ottolini, L., Bonatti, E.

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=od______3674::f017629a415c8f6db51f7e94eea61e0e
https://hdl.handle.net/11380/859707

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Transcrystalline melt migration driven by natural thermal gradients

Autor: Schiano, Pierre, Provost, Ariel, Clocchiatti, R., Faure, François

Publikováno v: Science
Science, 2006, 314, pp.970-974
Science, American Association for the Advancement of Science, 2006, 314, pp.970-974

International audience

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::06b926c5613780d1ab5235bd235bb763
https://hal.science/hal-00272281

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Boundary layers in plagio-hosted melt inclusion: temporal and thermal constraints on MORB genesis

Autor: Brunelli D., Clocchiatti R., Ottolini L.

Publikováno v: Geoitalia 2005, Spoleto, 21-23 settembre (2005)
info:cnr-pdr/source/autori:Brunelli D.; Clocchiatti R.; Ottolini L./congresso_nome:Geoitalia 2005/congresso_luogo:Spoleto/congresso_data:21-23 settembre (2005)/anno:2005/pagina_da:/pagina_a:/intervallo_pagine

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=cnr_________::ce3961c861a047bc362686c40e22bbfb
http://www.cnr.it/prodotto/i/112111

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Primitive magmas of the Southern Tyrrhenian Sea: evidence from olivine-hosted melt inclusions at Marsili seamount

Autor: Clocchiatti R., Trua T., Serri G., Ottolini L.

Publikováno v: ECROFI XVIII, European Current Research on Fluid Inclusions., Siena, July 6-9 (2005)
info:cnr-pdr/source/autori:Clocchiatti R.; Trua T.; Serri G.; Ottolini L./congresso_nome:ECROFI XVIII, European Current Research on Fluid Inclusions./congresso_luogo:Siena/congresso_data:July 6-9 (2005)/anno:2005/pagina_da:/pagina_a:/intervallo_pagine

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=cnr_________::ed2e3f2eb1b9de47c375d0b5e90540b0
https://publications.cnr.it/doc/112106

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