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Abstract
Sequential fragmentation/transport model was applied to ash deposits of 1723 eruption of Irazu volcano, Costa Rica. Some 25% of the sub-populations showed positive dispersion values, which were associated to a new fractal dimension,. With the help of Mandelbrot fractal relationship such cases were associated to a secondary fragmentation, similar to that proposed by Kaminski and Jaupart. Hence, explosive and effusive magma could be differentiated out of the granulometry
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