The Variscan subduction inheritance in the Southern Alps Sub-Continental Lithospheric Mantle: Clues from the Middle Triassic shoshonitic magmatism of the Dolomites (NE Italy)

Autor: Casetta, F., Ickert, R.B., Mark, D.F., Giacomoni, P.P., Bonadiman, C., Ntaflos, T., Zanetti, A., Coltorti, M.

Publikováno v: In LITHOS January 2021 380-381

The 2011–2012 paroxysmal eruptions at Mt. Etna volcano: Insights on the vertically zoned plumbing system

Autor: Giacomoni, P.P., Coltorti, M., Mollo, S., Ferlito, C., Braiato, M., Scarlato, P.

Publikováno v: In Journal of Volcanology and Geothermal Research 1 January 2018 349:370-391

Clinopyroxene and titanomagnetite cation redistributions at Mt. Etna volcano (Sicily, Italy): Footprints of the final solidification history of lava fountains and lava flows

Autor: Mollo, S., Giacomoni, P.P., Andronico, D., Scarlato, P.

Publikováno v: In Chemical Geology 16 June 2015 406:45-54

Plagioclase as archive of magma ascent dynamics on “open conduit” volcanoes: The 2001–2006 eruptive period at Mt. Etna

Autor: Giacomoni, P.P., Ferlito, C., Coltorti, M., Bonadiman, C., Lanzafame, G.

Publikováno v: In Earth-Science Reviews November 2014 138:371-393

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

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c671264d12a1db044ae948aecb513fe8
http://hdl.handle.net/11392/2383180