The average values of T 2C1 and T 2C2 are 2.82 ms and 1.58 ms, 3.4 ms and 1.7 ms, and 4.35 ms and 2.25 ms from mudstone, silty mudstone to argillaceous sand, respectively, which presents an increasing trend.
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Investigation of the pore structure characteristics and fluid components of Quaternary mudstone biogas reservoirs: a case study of the Qaidam Basin in China.
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