The Magnitude of the 39.8 ka Campanian Ignimbrite Eruption, Italy: Method, Uncertainties and Errors-Reference-Cited by-同舟云学术

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The Magnitude of the 39.8 ka Campanian Ignimbrite Eruption, Italy: Method, Uncertainties and Errors

Published:2020-10-19 Issue: Volume:8 Page:
ISSN:2296-6463
Container-title:Frontiers in Earth Science
language:
Short-container-title:Front. Earth Sci.

Author:

Silleni Aurora,Giordano Guido,Isaia Roberto,Ort Michael H.

Funder

National Science Foundation

Ministero dell' Istruzione, dell'Università e della Ricerca

Publisher

Frontiers Media SA

Subject

General Earth and Planetary Sciences

Reference174 articles.

1. Activating and reactivating pairs of nested collapses during caldera-forming eruptions: Campi Flegrei (Italy);Acocella;Geophys. Res. Lett.,2008

2. Evidence for a large-magnitude eruption from Campi Flegrei caldera (Italy) at 29 ka;Albert;Geology,2019

3. The regional geology and evolution of the Toba volcano-tectonic depression, Indonesia;Aldiss;J. Geol. Soc. London.,1984

4. Transport of pyroclastic flows across the sea during the explosive, rhyolitic eruption of the Kos Plateau Tuff, Greece;Allen;Bull. Volcanol.,2001

5. Effects of topography on pyroclastic density current runout and formation of coignimbrites;Andrews;Geology,2011

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