Geochemistry and Sr-Nd-Pb isotopes of Monte Amiata volcano, central Italy: evidence for magma mixing between high-K calc-alkaline and leucititic mantle-derivd magmas

Autor: Conticelli S.[1], Boari E.[1], Burlamacchi L.[3], Cifelli F.[4], Moscardi F.[1], Laurenzi M.[5], Ferrari Pedraglio L.[6], Francalanci L.[1, Benvenuti M.[1, Braschi E., 2

Publikováno v: Italian Journal of Geosciences (Online) 134 (2015): 266–290.
info:cnr-pdr/source/autori:Conticelli S.[1], Boari E.[1], Burlamacchi L.[3], Cifelli F.[4], Moscardi F.[1], Laurenzi M.[5], Ferrari Pedraglio L.[6], Francalanci L.[1,2], Benvenuti M.[1,2], Braschi E.,[2] Manetti P. [3]/titolo:Geochemistry and Sr-Nd-Pb isotopes of Monte Amiata volcano, central Italy: evidence for magma mixing between high-K calc-alkaline and leucititic mantle-derivd magmas/doi:/rivista:Italian Journal of Geosciences (Online)/anno:2015/pagina_da:266/pagina_a:290/intervallo_pagine:266–290/volume:134

Monte Amiata is a small volcano composed by trachytic to olivine latitic lava flows and domes emplaced in a very short time between 305 and 231 ka. The main petrographic features are represented by the occurrence of i) abundant rounded magmatic encla

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