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>Influence of Layered Structures of the Seabed on the Formation of Gas Hydrates in the Area Surrounding Deep-Sea Mud Volcanoes: A Mathematical Model
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Influence of Layered Structures of the Seabed on the Formation of Gas Hydrates in the Area Surrounding Deep-Sea Mud Volcanoes: A Mathematical Model
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机译：Influence of Layered Structures of the Seabed on the Formation of Gas Hydrates in the Area Surrounding Deep-Sea Mud Volcanoes: A Mathematical Model
The evolutionary processes of gas hydrate accumulations associated with deep-sea mud volcanoes are discussed. A mathematical model and the results of numerical modeling of gas hydrate accumulation in the seabed in the deep structures of underwater mud volcanoes are presented. The influence of permeability of various sediment layers on the evolution of gas hydrate accumulations associated with deep-sea mud volcanoes is analyzed quantitatively. Modeling has shown the rapid accumulation of significant volumes of gas hydrates in the layered structures of the seabed.
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