Carbonation of subduction-zone serpentinite (high-pressure ophicarbonate; Ligurian Western Alps) and implications for the deep carbon cycling

Autor: Scambelluri M.[1, Bebout G.E.[2], Belmonte D.[1], Gilio M.[1], Campomenosi N.[1], Collins N.[3], Crispini L.[1]

Publikováno v: Earth and planetary science letters 441 (2016): 155–166. doi:10.1016/j.epsl.2016.02.034
info:cnr-pdr/source/autori:Scambelluri M.[1,2], Bebout G.E.[2], Belmonte D.[1], Gilio M.[1], Campomenosi N.[1], Collins N.[3], Crispini L.[1]/titolo:Carbonation of subduction-zone serpentinite (high-pressure ophicarbonate; Ligurian Western Alps) and implications for the deep carbon cycling./doi:10.1016%2Fj.epsl.2016.02.034/rivista:Earth and planetary science letters/anno:2016/pagina_da:155/pagina_a:166/intervallo_pagine:155–166/volume:441

Much of the long-term carbon cycle in solid earth occurs in subduction zones, where processes of devolatilization, partial melting of carbonated rocks, and dissolution of carbonate minerals lead to the return of CO2 to the atmosphere via volcanic deg

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::912b9fbb07ebf12619e26aac61b01ce3
https://doi.org/10.1016/j.epsl.2016.02.034