Self and Rampino 1981
Self, S., and M.R. Rampino, 1981: The 1883 eruption of Krakatau. Nature, 294, 699-704, doi:10.1038/294699a0.
The 1883 eruption of Krakatau was a modest ignimbrite-forming event. The deposits are primarily coarse-grained dacitic, non-welded ignimbrite. Large explosions produced pyroclastic flows that entered the sea, generating destructuve tsunami. Grain-size studies of the ignimbrite suggest that these explosions were not driven by magma-seawater interaction. The total bulk volume of pyroclastic deposits, including co-ignimbrite ash, is estimated to be 18-21 km3.
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Self, S., and Rampino, M.R.: The 1883 eruption of Krakatau, Nature, 294, 699-704, doi:10.1038/294699a0, 1981.
Self, S., and M.R. Rampino (1981), The 1883 eruption of Krakatau, Nature, 294, 699-704, doi:10.1038/294699a0.
Self, S., and M.R. Rampino, 1981: The 1883 eruption of Krakatau. Nature, 294, 699-704, doi:10.1038/294699a0.
Self, S., & Rampino, M.R. 1981, Nature, 294, 699, doi:10.1038/294699a0.
Self S, Rampino MR. The 1883 eruption of Krakatau, Nature 1981;294:699-704. doi:10.1038/294699a0.
S. Self, M.R. Rampino, Nature 294, 699-704, doi:10.1038/294699a0 (1981).
