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Publikováno v:
Geothermics 89 (2021): 1–15. doi:10.1016/j.geothermics.2020.101961
info:cnr-pdr/source/autori:Taussi M.[1], Nisi B.[2], Vaselli O.[2,3,4], Maza S.[5,6], Morata D.[5,6], Renzulli A.[1,7]/titolo:SOIL CO2 FLUX AND TEMPERATURE FROM A NEW GEOTHERMAL AREA IN THE CORDÓN DE INACALIRI VOLCANIC COMPLEX (NORTHERN CHILE)/doi:10.1016%2Fj.geothermics.2020.101961/rivista:Geothermics/anno:2021/pagina_da:1/pagina_a:15/intervallo_pagine:1–15/volume:89
info:cnr-pdr/source/autori:Taussi M.[1], Nisi B.[2], Vaselli O.[2,3,4], Maza S.[5,6], Morata D.[5,6], Renzulli A.[1,7]/titolo:SOIL CO2 FLUX AND TEMPERATURE FROM A NEW GEOTHERMAL AREA IN THE CORDÓN DE INACALIRI VOLCANIC COMPLEX (NORTHERN CHILE)/doi:10.1016%2Fj.geothermics.2020.101961/rivista:Geothermics/anno:2021/pagina_da:1/pagina_a:15/intervallo_pagine:1–15/volume:89
This paper deals with the first geochemical data from an unexplored sector of the Cordon de Inacaliri Volcanic Complex (Central Andes, Chile). The site is located at ∼5,150-5,200 m a.s.l., inside the Pabelloncito graben where, at about 9 km NW of t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::54c242dfb2ae87ffa31c915ad6884fb4
https://hdl.handle.net/11576/2679700
https://hdl.handle.net/11576/2679700
