Flow of a fluid-saturated breccia in a mud feeding system of mud volcanoes

Category: 14-4
A.L. Sobisevich, R.A. Zhostkov

УДК 551.217.3+532.5


A.L. Sobisevich, R.A. Zhostkov 

Schmidt Institute of Physics of the Earth, Russian Academy of Sciences, Moscow, Russia



The results of low-frequency microseismic sounding of the Shugo mud volcano are used for theoretical modelling of the processes of hydrodynamic outflow under various possible mechanisms of eruptive activity.

Keywords: mud volcanoes, volcanic activity model, geophysical profile, two-phase flow.



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