Abstract
Most mud volcanoes are located along large tectonic zones within the Alpine and Central Asia folded regions, Pacific mobile belt, and rift zones of the Atlantic and Indian oceans. One of the main conditions of the functioning of mud volcanic processes in mobile belts of the Earth’s crust is dislocation and folding of sedimentary rocks. Precisely such geological conditions exist in the Taman mud volcanic province, where the well-known Shugo Volcano is located.
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