Multiple generations of tuffisite veins record repetitive ductile-brittle deformation of rhyolitic magma rising within an effusive vent: a source of flow banding in silicic lavas and repetitive seismic signals?

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ADS bibcode
2002AGUFM.V12A1416T
year
2002
Listed Authors
Tuffen, H.
Pinkerton, H.
Dingwell, D. B.
Davison, B.
Listed Institutions
Institut für Mineralogie, Petrologie und Geochemie, Theresienstrasse 41, München, 80333 Germany
Department of Environmental Science, Lancaster University, Bailrigg, Lancaster, LA1 4YQ United Kingdom
Institut für Mineralogie, Petrologie und Geochemie, Theresienstrasse 41, München, 80333 Germany
Department of Environmental Science, Lancaster University, Bailrigg, Lancaster, LA1 4YQ United Kingdom

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