Zobrazeno 1 - 2
of 2
pro vyhledávání: '"Conticelli S. [3"'
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
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
http://link.springer.com/article/10.1038/s41598-019-45031-3
Publikováno v:
Lithos (Oslo. Print) 316-317 (2018): 304–322. doi:10.1016/j.lithos.2018.07.018
info:cnr-pdr/source/autori:Di Giuseppe P.[1,2], Agostini S.[2], Manetti P.[1,3], Savascin M.Y.[4] Conticelli S.[3,5]/titolo:Sub-lithospheric origin of Na-alkaline and calc-alkaline magmas in a post-collisional tectonic regime: Sr-Nd-Pb isotopes in recent monogenetic volcanism of Cappadocia, Central Turkey/doi:10.1016%2Fj.lithos.2018.07.018/rivista:Lithos (Oslo. Print)/anno:2018/pagina_da:304/pagina_a:322/intervallo_pagine:304–322/volume:316-317
info:cnr-pdr/source/autori:Di Giuseppe P.[1,2], Agostini S.[2], Manetti P.[1,3], Savascin M.Y.[4] Conticelli S.[3,5]/titolo:Sub-lithospheric origin of Na-alkaline and calc-alkaline magmas in a post-collisional tectonic regime: Sr-Nd-Pb isotopes in recent monogenetic volcanism of Cappadocia, Central Turkey/doi:10.1016%2Fj.lithos.2018.07.018/rivista:Lithos (Oslo. Print)/anno:2018/pagina_da:304/pagina_a:322/intervallo_pagine:304–322/volume:316-317
Intense Cenozoic magmatism accompanied the convergence and collision of the Eurasian, African and Arabian plates. In the Cappadocia Region of Central Anatolia, widespread and abundant volcanism developed from the late Miocene to the Quaternary. Calc-
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::93391b1f8c064bd51c67b1a1ac11227c
https://www.journals.elsevier.com/lithos
https://www.journals.elsevier.com/lithos
