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Autor:
Lamberti M.C.[1], Vigide N.[1, Venturi S. [3, Agusto M.[1], Yagupsky D.[2], Winocur D.[4], Barcelona H.[4], Velez M.L.[1], Cardellini C.[5], Tassi F.[6]
Publikováno v:
Journal of volcanology and geothermal research 374 (2019): 131–141. doi:10.1016/j.jvolgeores.2019.02.004
info:cnr-pdr/source/autori:Lamberti M.C.[1], Vigide N.[1,2], Venturi S. [3,6], Agusto M.[1], Yagupsky D.[2], Winocur D.[4], Barcelona H.[4], Velez M.L.[1], Cardellini C.[5], Tassi F.[6]/titolo:Structural architecture releasing deep-sourced carbon dioxide diffuse degassing at the Caviahue-Copahue Volcanic Complex/doi:10.1016%2Fj.jvolgeores.2019.02.004/rivista:Journal of volcanology and geothermal research/anno:2019/pagina_da:131/pagina_a:141/intervallo_pagine:131–141/volume:374
info:cnr-pdr/source/autori:Lamberti M.C.[1], Vigide N.[1,2], Venturi S. [3,6], Agusto M.[1], Yagupsky D.[2], Winocur D.[4], Barcelona H.[4], Velez M.L.[1], Cardellini C.[5], Tassi F.[6]/titolo:Structural architecture releasing deep-sourced carbon dioxide diffuse degassing at the Caviahue-Copahue Volcanic Complex/doi:10.1016%2Fj.jvolgeores.2019.02.004/rivista:Journal of volcanology and geothermal research/anno:2019/pagina_da:131/pagina_a:141/intervallo_pagine:131–141/volume:374
The link between carbon dioxide diffuse degassing and its structural control was examined in the Caviahue – Copahue Volcanic Complex, over an area of approximately 10 km 2 that encompasses five hydrothermal sites, namely, Anfiteatro, Copahue town,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d337bec4548863745b015efb6a0e1505
http://hdl.handle.net/11391/1447968
http://hdl.handle.net/11391/1447968