Temperature measurements, gas chemistry, and gas hydrates of the Dvurechenskii mud volcano, supplement to: Feseker, Tomas; Pape, Thomas; Wallmann, Klaus; Klapp, Stephan A; Schmidt-Schierhorn, Friederike; Bohrmann, Gerhard (2009): The thermal structure of the Dvurechenskii mud volcano and its implications for gas hydrate stability and eruption dynamics. Marine and Petroleum Geology, 26(9), 1812-1823

Tomas Feseker, Thomas Pape, Klaus Wallmann, Stephan A Klapp, Friederike Schmidt-Schierhorn & Gerhard Bohrmann
The sediment temperature distribution at mud volcanoes provides insights into their activity and into the occurrence of gas hydrates. If ambient pressure and temperature conditions are close to the limits of the gas hydrate stability field, the sediment temperature distribution not only limits the occurrence of gas hydrates, but is itself influenced by heat production and consumption related to the formation and dissociation of gas hydrates. Located in the Sorokin Trough in the northern Black...
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