The anticlinal core sample (RJG2-04) is 3.97%, which shows a decreasing trend to anticlinal right limb (2.1%, RJG2-01).
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Variations of Pore Structure and Methane Adsorption of Continental Deformed Shales from Small-Scale Anticline and Syncline: Two Cases Study of the Triassic Yanchang Formation, Ordos Basin and Jurassic Yaojie Formation, Minhe Basin.
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