Using the spatial distribution and lithology of ballistic blocks to interpret eruption sequence and dynamics: August 6 2012 Upper Te Maari eruption, New Zealand

Author:

Breard E.C.P.,Lube G.,Cronin S.J.,Fitzgerald R.,Kennedy B.,Scheu B.,Montanaro C.,White J.D.L.,Tost M.,Procter J.N.,Moebis A.

Funder

Ministry of Business, Innovation and Employment

Royal Society of New Zealand

FP7-MC-ITN project NEMOH

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geophysics

Reference36 articles.

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3. The 1968 andesitic lateral blast eruption at Arenal Volcano, Costa Rica;Alvarado;J. Volcanol. Geotherm. Res.,2006

4. Directed blasts and blast-generated pyroclastic density currents: a comparison of the Bezymianny 1956, Mount St Helens 1980, and Soufriere Hills, Montserrat 1997 eruptions and deposits;Belousov;Bull. Volcanol.,2007

5. Pyroclastic Density Currents and the Sedimentation of Ignimbrites;Branney,2002

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