Mineralogy and geochemistry of the older (>40ka) ignimbrites on the Campanian Plain, Southern Italy.

dc.date.accessioned2020-03-11T20:26:59Z
dc.date.accessioned2022-10-18T22:42:03Z
dc.date.available2020-03-11T20:26:59Z
dc.date.available2022-10-18T22:42:03Z
dc.date.created2020-03-11T20:26:59Z
dc.date.issued2016
dc.identifierhttp://hdl.handle.net/10533/238170
dc.identifier15090013
dc.identifierWOS:000387197700001
dc.identifierno scielo
dc.identifiereid=2-s2.0-84968846704
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/4469509
dc.description.abstractThe Campanian Plain in southern Italy has been volcanically active for at least the last 300 ka. The Campanian Ignimbrite (CI) erupted at 39.3 ka, has a volume of ≥ 310 km3 and a great areal extent. However, significant, but scattered deposits of older ig
dc.languageeng
dc.relationhttps://doi.org/10.1016/j.jvolgeores.2016.05.002
dc.relation10.1016/j.jvolgeores.2016.05.002
dc.rightsinfo:eu-repo/semantics/openAccess
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 Chile
dc.rightshttp://creativecommons.org/licenses/by-nc-nd/3.0/cl/
dc.titleMineralogy and geochemistry of the older (>40ka) ignimbrites on the Campanian Plain, Southern Italy.
dc.typeArticulo


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