Zobrazeno 1 - 10
of 183
pro vyhledávání: '"Rampone E"'
Autor:
Notini, L., Scambelluri, M., Tommasi, A., Zanetti, A., Ferri, F., Rodríguez-Vargas, A., Rampone, E.
Publikováno v:
In LITHOS January 2024 464-465
Autor:
Borghini, G., Rampone, E., Class, C., Goldstein, S., Cai, Y., Cipriani, A., Hofmann, A.W., Bolge, L.
Publikováno v:
In Chemical Geology 30 December 2021 586
Publikováno v:
In Chemical Geology 20 January 2020 532
Akademický článek
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Autor:
Rampone E.[1], Sanfilippo A.[2
Publikováno v:
Elements (Que. Online) 17 (2021): 23–28. doi:10.2138/GSELEMENTS.17.1.23
info:cnr-pdr/source/autori:Rampone E.[1], Sanfilippo A.[2,3]/titolo:The heterogeneous tethyan oceanic lithosphere of the alpine ophiolites/doi:10.2138%2FGSELEMENTS.17.1.23/rivista:Elements (Que. Online)/anno:2021/pagina_da:23/pagina_a:28/intervallo_pagine:23–28/volume:17
info:cnr-pdr/source/autori:Rampone E.[1], Sanfilippo A.[2,3]/titolo:The heterogeneous tethyan oceanic lithosphere of the alpine ophiolites/doi:10.2138%2FGSELEMENTS.17.1.23/rivista:Elements (Que. Online)/anno:2021/pagina_da:23/pagina_a:28/intervallo_pagine:23–28/volume:17
The Alpine–Apennine ophiolites are lithospheric remnants of the Jurassic Alpine Tethys Ocean. They predominantly consist of exhumed mantle peridotites with lesser gabbroic and basaltic crust and are locally associated with continental crustal mater
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::29d23da8afab0fd69126e29d24e904fc
http://hdl.handle.net/11567/1050057
http://hdl.handle.net/11567/1050057
Akademický článek
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Publikováno v:
In Earth and Planetary Science Letters 2004 218(3):491-506
Autor:
Borghini G.[1, 2, 3] Rampone E.[2], Zanetti A.[4], Class C.[3], Cipriani A.[3, Hofmann A.W.[3, Goldstein S.L.[3
Publikováno v:
Journal of petrology
57 (2016): 625–653. doi:10.1093/petrology/egv074
info:cnr-pdr/source/autori:Borghini G.[1,2,3] Rampone E.[2], Zanetti A.[4], Class C.[3], Cipriani A.[3,5], Hofmann A.W.[3,6], Goldstein S.L.[3,7]/titolo:Pyroxenite layers in the northern apennines' upper mantle (Italy)-Generation by pyroxenite melting and melt infiltration/doi:10.1093%2Fpetrology%2Fegv074/rivista:Journal of petrology (Print)/anno:2016/pagina_da:625/pagina_a:653/intervallo_pagine:625–653/volume:57
57 (2016): 625–653. doi:10.1093/petrology/egv074
info:cnr-pdr/source/autori:Borghini G.[1,2,3] Rampone E.[2], Zanetti A.[4], Class C.[3], Cipriani A.[3,5], Hofmann A.W.[3,6], Goldstein S.L.[3,7]/titolo:Pyroxenite layers in the northern apennines' upper mantle (Italy)-Generation by pyroxenite melting and melt infiltration/doi:10.1093%2Fpetrology%2Fegv074/rivista:Journal of petrology (Print)/anno:2016/pagina_da:625/pagina_a:653/intervallo_pagine:625–653/volume:57
Pyroxenite layers embedded within peridotite represent widespread lithological mantle heterogeneities and are potential components in the mantle source of many oceanic basalts. They can be generated by a variety of magmatic and metamorphic processes.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::689f1be64981b531548157523195bc5e
https://doi.org/10.1093/petrology/egv074
https://doi.org/10.1093/petrology/egv074
Publikováno v:
J. Petrol.
At Cima di Gagnone garnet peridotite and chlorite harzburgite lenses within pelitic schists and gneisses correspond to eclogite facies breakdown products of hydrated peridotites and are suitable for studying dehydration of serpentinized mantle. Therm
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=snsf_p3_pubs::f3471a47bc403788c2712cf7571e1ad0