Thermodynamic analysis of HP-UHP fluid inclusions: The solute load and chemistry of metamorphic fluids

Autor: Maffeis A.[1], Ferrando S.[1], Connolly J.A.D.[2], Groppo C. [1, Frezzotti M.L.[4], Castelli D.[1]

Publikováno v: Geochimica et cosmochimica acta 315 (2021): 207–229. doi:10.1016/j.gca.2021.08.044
info:cnr-pdr/source/autori:Maffeis A.[1], Ferrando S.[1], Connolly J.A.D.[2], Groppo C. [1,3], Frezzotti M.L.[4], Castelli D.[1]/titolo:Thermodynamic analysis of HP-UHP fluid inclusions: The solute load and chemistry of metamorphic fluids/doi:10.1016%2Fj.gca.2021.08.044/rivista:Geochimica et cosmochimica acta/anno:2021/pagina_da:207/pagina_a:229/intervallo_pagine:207–229/volume:315

Subduction fluids play a crucial role in regulating long-term chemical cycles. Their characterisation is essential to understand the processes responsible for metasomatism, oxidation and melting of the mantle wedge. Both direct (fluid inclusion studi

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8c908c1ba98b19209924ae8c3f5af81c
http://www.cnr.it/prodotto/i/460048

Fe-rich antigorite: a rock-forming mineral from low-temperature/high-pressure meta-ophicarbonates

Autor: Di Pierro S.[1, 2, Groppo C.[1, Compagnoni R.[1], Capitani G.[4], Mellini M.[5]

Publikováno v: European journal of mineralogy
31 (2019): 775–784. doi:10.1127/ejm/2019/0031-2867
info:cnr-pdr/source/autori:Di Pierro S.[1,2,a], Groppo C.[1,3], Compagnoni R.[1], Capitani G.[4], Mellini M.[5]/titolo:Fe-rich antigorite: A rock-forming mineral from low-temperature%2Fhigh-pressure meta-ophicarbonates/doi:10.1127%2Fejm%2F2019%2F0031-2867/rivista:European journal of mineralogy (Print)/anno:2019/pagina_da:775/pagina_a:784/intervallo_pagine:775–784/volume:31

This study provides the first characterization of Fe-rich antigorite (FeOtot up to 12 wt%), a rock-forming mineral occurring in ophicarbonate rocks from different low-temperature/high-pressure meta-ophiolitic suites: Acceglio (Traversiera Valley, ext

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::bdc5eda20f3b5235ce343a075ef9d77f
http://hdl.handle.net/2318/1718941

The Monviso Massif and the Cottian Alps as Symbols of the Alpine Chain and Geological Heritage in Piemonte, Italy

Autor: Rolfo F.[1, Benna P.[1], Cadoppi P.[1], Castelli D.[1, Favero-Longo S.[3], Giardino M., Balestro G.[1], Belluso E.[1, Borghi A.[1], Camara F.[1], Compagnoni R.[1], Ferrando S.[1], Festa A.[1], Forno M.[1], Giacometti F.[4], Gianotti F.[1], Groppo C.[1], Lombardo B.[2], Mosca P.[2], Perrone G.[1], Piervittori R.[3], Rebay G.[4], Rossetti P. [1]

Publikováno v: Geoheritage (Berl., Print) 7 (2015): 65–84. doi:10.1007/s12371-014-0097-9
info:cnr-pdr/source/autori:Rolfo F.[1,2], Benna P.[1], Cadoppi P.[1], Castelli D.[1,2], Favero-Longo S.[3], Giardino M., Balestro G.[1], Belluso E.[1,2], Borghi A.[1], Camara F.[1], Compagnoni R.[1], Ferrando S.[1], Festa A.[1], Forno M.[1], Giacometti F.[4], Gianotti F.[1], Groppo C.[1], Lombardo B.[2], Mosca P.[2], Perrone G.[1], Piervittori R.[3], Rebay G.[4], Rossetti P. [1]/titolo:The Monviso Massif and the Cottian Alps as symbols of the Alpine chain and geological heritage in Piemonte, Italy/doi:10.1007%2Fs12371-014-0097-9/rivista:Geoheritage (Berl., Print)/anno:2015/pagina_da:65/pagina_a:84/intervallo_pagine:65–84/volume:7

In order to promote geosite conservation in the project entitled 'PROactive management of GEOlogical heritage in the PIEMONTE Region', we propose a comprehensive study involving the Monviso Massif (MM) geothematic area, one of the most outstanding sy

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1430ef6da074b1df8cb559b6032b15ff
https://doi.org/10.1007/s12371-014-0097-9

Metamorphic CO2 production in collisional orogens: Petrological constrains from phase diagram modeling of Himalayan, scapolite-bearing, calc-silicate rocks in the NKC(F)MAS(T)-HC system

Autor: Groppo C.[1, Rolfo F.[1, Castelli D.[1], Mosca P.[2]

Publikováno v: Journal of petrology
58 (2017): 53–83.
info:cnr-pdr/source/autori:Groppo C.[1,2], Rolfo F.[1,2], Castelli D.[1], Mosca P.[2]/titolo:Metamorphic CO2 production in collisional orogens: Petrological constrains from phase diagram modeling of Himalayan, scapolite-bearing, calc-silicate rocks in the NKC(F)MAS(T)-HC system/doi:/rivista:Journal of petrology (Print)/anno:2017/pagina_da:53/pagina_a:83/intervallo_pagine:53–83/volume:58

No abstract available

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=cnr_________::37f7b6ebf5b3e80d335a0809449859c3
http://www.cnr.it/prodotto/i/375568

Petrology of blueschist from the Western Himalaya (Ladakh, NW India): Exploring the complex behavior of a lawsonite-bearing system in a paleo-accretionary setting

Autor: Groppo C.[1, Rolfo F.[1, Sachan H.K.[3], Rai S.K.[3]

Publikováno v: Lithos (Oslo. Print) 252-253 (2016): 41–56. doi:10.1016/j.lithos.2016.02.014
info:cnr-pdr/source/autori:Groppo C.[1,2], Rolfo F.[1,2], Sachan H.K.[3], Rai S.K.[3]/titolo:Petrology of blueschist from the Western Himalaya (Ladakh, NW India): Exploring the complex behavior of a lawsonite-bearing system in a paleo-accretionary setting./doi:10.1016%2Fj.lithos.2016.02.014/rivista:Lithos (Oslo. Print)/anno:2016/pagina_da:41/pagina_a:56/intervallo_pagine:41–56/volume:252-253

Although the Himalaya is the archetype of collisional orogens, formed as a consequence of the closure of the Neo-Tethyan ocean separating India from Asia, high-pressure metamorphic rocks are rare. Beside few eclogites, corresponding to the metamorpho

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4fc5088e483d635815433a0289b09ebd
http://hdl.handle.net/2318/1565724