High-Nb hawaiite-mugearite and high-Mg calc-alkaline lavas from northeastern Iran: Oligo-Miocene melts from modified mantle wedge

Autor: Ahmadi P.[1], Ghorban M.R.[1], Coltorti M.[2], Kuritani T.[3], Cai Y.[4], Fioretti A.M.[5], Braschi E.[6], Giacomoni P.P.[2], Aghabazaz F.[1], Babazadeh S.[1], Conticelli S.[6

Publikováno v: International geology review 61 (2019): 150–174. doi:10.1080/00206814.2017.1416502
info:cnr-pdr/source/autori:Ahmadi P.[1], Ghorban M.R.[1], Coltorti M.[2], Kuritani T.[3], Cai Y.[4], Fioretti A.M.[5], Braschi E.[6], Giacomoni P.P.[2], Aghabazaz F.[1], Babazadeh S.[1], Conticelli S.[6,7]/titolo:High-Nb hawaiite-mugearite and high-Mg calc-alkaline lavas from northeastern Iran: Oligo-Miocene melts from modified mantle wedge/doi:10.1080%2F00206814.2017.1416502/rivista:International geology review/anno:2019/pagina_da:150/pagina_a:174/intervallo_pagine:150–174/volume:61

Tertiary volcanic rocks in northwestern Firoozeh, Iran (the Meshkan triangular structural unit), constitute vast outcrops (up to 250 km2) of high-Mg basaltic andesites to dacites that are associated with high-Nb hawaiites and mugearites. Whole-rock 4

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http://hdl.handle.net/11392/2383180