Strongly SiO2-undersaturated, CaO-rich kamafugitic Pleistocene magmatism in Central Italy (San Venanzo volcanic complex) and the role of shallow

Autor: Lustrino .[1, Ronca S.[1], Caracausi A.[3], Ventura Bordenca C.[4], Agostini S.[5], Benedetto Faraone D.B.[1]

Publikováno v: Earth-science reviews 208 (2020). doi:10.1016/j.earscirev.2020.103256
info:cnr-pdr/source/autori:Lustrino .[1,2], Ronca S.[1], Caracausi A.[3], Ventura Bordenca C.[4], Agostini S.[5], Benedetto Faraone D.B.[1]/titolo:Strongly SiO2-undersaturated, CaO-rich kamafugitic Pleistocene magmatism in Central Italy (San Venanzo volcanic complex) and the role of shallow/doi:10.1016%2Fj.earscirev.2020.103256/rivista:Earth-science reviews/anno:2020/pagina_da:/pagina_a:/intervallo_pagine:/volume:208

The Pleistocene (~460-265 ka) San Venanzo volcanic complex belongs to the IAP (Intra-Apennine Province) in central Italy, which comprises at least four small Pleistocene monogenetic volcanoes plus several unrooted pyroclastic deposits with peculiar m

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