These predicted values show an increasing trend westward toward the Huianbao-Shajingzi thrust fault, with higher saturation levels of approximately 2 m 3 /t observed in wells HT-5 and QT-9.
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Geochemical Characterization and Paleo-Burial History Modeling of Unconventional Resources: A Case Study from the Ordovician Wulalike Formation (O<sub>2</sub>w) in the West Margin of the Ordos Basin (North China).
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