The upper crustal magma plumbing system of the Pleistocene Apacheta-Aguilucho Volcanic Complex area (Altiplano-Puna, northern Chile) as inferred from the erupted lavas and their enclaves

Autor: Taussi M.[1], Godoy B.[2], Piscaglia F.[3], Morata D.[2], Agostini A.[4], Le Roux P.[5], González-Maurel O.[5, Gallmeyer G.[6], Menzies A.[6], Renzulli A.[1

Publikováno v: Journal of volcanology and geothermal research 373 (2019): 179–198. doi:10.1016/j.jvolgeores.2019.01.021
info:cnr-pdr/source/autori:Taussi M.[1], Godoy B.[2], Piscaglia F.[3], Morata D.[2], Agostini A.[4], Le Roux P.[5], González-Maurel O.[5,6], Gallmeyer G.[6], Menzies A.[6], Renzulli A.[1,3]/titolo:The upper crustal magma plumbing system of the Pleistocene Apacheta-Aguilucho Volcanic Complex area (Altiplano-Puna, northern Chile) as inferred from the erupted lavas and their enclaves/doi:10.1016%2Fj.jvolgeores.2019.01.021/rivista:Journal of volcanology and geothermal research/anno:2019/pagina_da:179/pagina_a:198/intervallo_pagine:179–198/volume:373

The evolution of the magma plumbing system of the Pleistocene Apacheta-Aguilucho Volcanic Complex area (Altiplano-Puna Volcanic Complex, northern Chile) was investigated through petrographic, geochemical and isotopic studies of representative lavas a

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::182ba00063760c305b4e7c49b0043bea
https://hdl.handle.net/11576/2665116