Vapour dynamics during magma–water interaction experiments: hydromagmatic origins of submarine volcaniclastic particles (limu o Pele)
CI Schipper, I Sonder, A Schmid… - Geophysical Journal …, 2013 - academic.oup.com
Recent observations have shattered the long-held theory that deep-sea (> 500 m) explosive
eruptions are impossible; however, determining the dynamics of unobserved eruptions …
eruptions are impossible; however, determining the dynamics of unobserved eruptions …
Vapour dynamics during magma-water interaction experiments: hydromagmatic origins of submarine volcaniclastic particles (limu o Pele)
CI Schipper, I Sonder, A Schmid, JDL White… - Geophysical Journal …, 2013 - hero.epa.gov
Recent observations have shattered the long-held theory that deep-sea (> 500 m) explosive
eruptions are impossible; however, determining the dynamics of unobserved eruptions …
eruptions are impossible; however, determining the dynamics of unobserved eruptions …
Vapour dynamics during magma-water interaction experiments: hydromagmatic origins of submarine volcaniclastic particles (limu o Pele)
CI Schipper, I Sonder, A Schmid… - Geophysical …, 2013 - ui.adsabs.harvard.edu
Recent observations have shattered the long-held theory that deep-sea (> 500 m) explosive
eruptions are impossible; however, determining the dynamics of unobserved eruptions …
eruptions are impossible; however, determining the dynamics of unobserved eruptions …
Vapour dynamics during magma–water interaction experiments: hydromagmatic origins of submarine volcaniclastic particles (limu o Pele)
CI Schipper, I Sonder, A Schmid… - Geophysical Journal …, 2012 - ieeexplore.ieee.org
Recent observations have shattered the long-held theory that deep-sea (> 500 m) explosive
eruptions are impossible; however, determining the dynamics of unobserved eruptions …
eruptions are impossible; however, determining the dynamics of unobserved eruptions …