Abstract Self‐ignition during the explosive eruption of mud volcanoes can create flames that in some cases reach heights exceed hundreds meters. To study controls on electrical discharge natural mud, we performed laboratory experiments using a shock‐tube apparatus to simulate eruptions mud. We vary water content and proportions fine particles. measure electric within Faraday cage use high‐speed...

Mud volcanoes and other fluid seepage pathways usually transport sufficient gas for the formation of reservoirs are beneficial to accumulation hydrate. On hand, thermal effects mud can constrain occurrence hydrates. Current field measurements indicate that anomalies impact distribution hydrates associated with volcanoes. However, due lack quantitative analysis volcano flow evolution, it is diff...

Mud volcanoes and diapirs are geological structures formed due to arch piercing or diapiric intrusion of ductile sedimentary materials into the overlying strata along high permeability channels. A detailed study on processes controlling formation mud in northern continental margin South China Sea is vital importance exploration economically viable oil gas reservoirs can be helpful natural hydra...