Carbonate degradation is very crucial thing to discuss about the occurring of diapiric and petroleum system.
Gas hydrate decomposition can provide
large amounts of gas-rich fl uids (generally
methane) that migrate upward through faults.
This process can induce shale diapirism and
mud volcanism, and can also cause sedimentary
instability through the reduction of the shear
strength of the overlying sediments (Henriet and
Meniert, 1998).
Similar process as above to carbonate decomposition.
would you like to inform me the title of book/journal which written by Henriet and Meniert?
Henriet, J.P., and Meniert, J., 1998, Gas hydrates: Relevance to world margin stability and climatic changes: Geological Society [London] Special Publication 137. 338 p.
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