The response of bitumen-hosted pores to thermal maturity shows that as Ro increases from 0.7 to 2.0%, bitumen pore abundance shows an increasing trend ( Figure g–i).
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Development of Organic Pores in the Gufeng and Longmaxi Formation Shale, Sichuan Basin: Combined Effects of Bioprecursor, Pore Filling, and Mineral-Organic Interactions.
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