40Ar/39Ar geochronology of Holocene basalts; examples from Stromboli, Italy

J.R. Wijbrans; B.S.H. Schneider; K.F. Kuiper; S. Calvari; S. Branca; E. De Beni; G. Norini; R.A. Corsaro; L. Miraglia

doi:10.1016/j.quageo.2010.10.003

40Ar/39Ar geochronology of Holocene basalts; examples from Stromboli, Italy

J.R. Wijbrans, B.S.H. Schneider, K.F. Kuiper, S. Calvari, S. Branca, E. De Beni, G. Norini, R.A. Corsaro, L. Miraglia

Research output: Contribution to Journal › Article › Academic › peer-review

Abstract

Absolute chronologies of active volcanoes and consequently timescales for eruptive behaviour and magma production form a quantitative basis for understanding the risk of volcanoes. Surprisingly, the youngest records in the geological timescale often prove to be the most elusive when it comes to isotopic dating. Absolute Holocene volcanic records almost exclusively rely on

Original language	English
Article number	109
Pages (from-to)	223-232
Journal	Quaternary Geochronology
Issue number	V6
DOIs	https://doi.org/10.1016/j.quageo.2010.10.003
Publication status	Published - 2011

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title = "40Ar/39Ar geochronology of Holocene basalts; examples from Stromboli, Italy",

abstract = "Absolute chronologies of active volcanoes and consequently timescales for eruptive behaviour and magma production form a quantitative basis for understanding the risk of volcanoes. Surprisingly, the youngest records in the geological timescale often prove to be the most elusive when it comes to isotopic dating. Absolute Holocene volcanic records almost exclusively rely on",

author = "J.R. Wijbrans and B.S.H. Schneider and K.F. Kuiper and S. Calvari and S. Branca and {De Beni}, E. and G. Norini and R.A. Corsaro and L. Miraglia",

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doi = "10.1016/j.quageo.2010.10.003",

language = "English",

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journal = "Quaternary Geochronology",

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AU - Wijbrans, J.R.

AU - Schneider, B.S.H.

AU - Kuiper, K.F.

AU - Calvari, S.

AU - Branca, S.

AU - De Beni, E.

AU - Norini, G.

AU - Corsaro, R.A.

AU - Miraglia, L.

PY - 2011

Y1 - 2011

N2 - Absolute chronologies of active volcanoes and consequently timescales for eruptive behaviour and magma production form a quantitative basis for understanding the risk of volcanoes. Surprisingly, the youngest records in the geological timescale often prove to be the most elusive when it comes to isotopic dating. Absolute Holocene volcanic records almost exclusively rely on

AB - Absolute chronologies of active volcanoes and consequently timescales for eruptive behaviour and magma production form a quantitative basis for understanding the risk of volcanoes. Surprisingly, the youngest records in the geological timescale often prove to be the most elusive when it comes to isotopic dating. Absolute Holocene volcanic records almost exclusively rely on

U2 - 10.1016/j.quageo.2010.10.003

DO - 10.1016/j.quageo.2010.10.003

M3 - Article

SN - 1871-1014

SP - 223

EP - 232

JO - Quaternary Geochronology

JF - Quaternary Geochronology

IS - V6

M1 - 109

ER -

40Ar/39Ar geochronology of Holocene basalts; examples from Stromboli, Italy

Abstract

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