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Movement and Accumulation of Methane in Marine Sediments: Relation to Gas Hydrate Systems

  • Clennell M
  • Judd A
  • Hovland M
DOI: 10.1007/978-94-011-4387-5_9
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Abstract

Deep in the sediments, gases come predominantly from temperature-dependent reactions. These thermogenic gases may migrate long distances vertically and laterally before reaching the hydrate stability zone.

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Clennell, M. B., Judd, A., & Hovland, M. (2003). Movement and Accumulation of Methane in Marine Sediments: Relation to Gas Hydrate Systems (pp. 105–122). https://doi.org/10.1007/978-94-011-4387-5_9

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