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The American mineralogist (Online) 102 (2017): 42–60. doi:10.2138/am-2017-5761
info:cnr-pdr/source/autori:Ferrando S.[1], Groppo C.[1,2], Frezzotti M.L.[3], Castelli D.[1], Proyer A.[4]/titolo:Dissolving dolomite in a stable UHP mineral assemblage: Evidence from Cal-Dol marbles of the Dora-Maira Massif (Italian Western Alps)/doi:10.2138%2Fam-2017-5761/rivista:The American mineralogist (Online)/anno:2017/pagina_da:42/pagina_a:60/intervallo_pagine:42–60/volume:102
info:cnr-pdr/source/autori:Ferrando S.[1], Groppo C.[1,2], Frezzotti M.L.[3], Castelli D.[1], Proyer A.[4]/titolo:Dissolving dolomite in a stable UHP mineral assemblage: Evidence from Cal-Dol marbles of the Dora-Maira Massif (Italian Western Alps)/doi:10.2138%2Fam-2017-5761/rivista:The American mineralogist (Online)/anno:2017/pagina_da:42/pagina_a:60/intervallo_pagine:42–60/volume:102
In deep and cold subduction such as that experienced by the UHP Units of the Western Alps, carbon dissolution is a relevant mechanism for carbon transfer from the slab into the mantle. The UHP impure Cal-Dol-marbles from the Dora-Maira Massif are stu
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f238ed948fc40a47bcf7b50cb7a31f1d
http://hdl.handle.net/2318/1614587
http://hdl.handle.net/2318/1614587