The Onano eruption (Latera volcano, Central Italy): an example of magma mixing/mingling as dominant process in a caldera-forming eruption

Autor: Landi P.[1, D'Oriano C.[1]

Publikováno v: Contributions to mineralogy and petrology (Internet) 175 (2020): 1–24. doi:10.1007/s00410-020-01724-x
info:cnr-pdr/source/autori:Landi P.[1,2], D'Oriano C.[1]/titolo:The Onano eruption (Latera volcano, Central Italy): an example of magma mixing%2Fmingling as dominant process in a caldera-forming eruption/doi:10.1007%2Fs00410-020-01724-x/rivista:Contributions to mineralogy and petrology (Internet)/anno:2020/pagina_da:1/pagina_a:24/intervallo_pagine:1–24/volume:175

The Onano eruption (~ 0.17 Ma) is the second to last caldera-forming eruption of the Latera volcano, in the northernmost sector of the Roman Comagmatic Province (Latium, Italy). The stratigraphic sequence, from base to top, includes ash and pumice-ri

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