WIP values are between 13.8 and 51.7 and show an increasing trend from Stage I to Stage III ( Figure 7 d).
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Geochemical Characteristics of the Middle Jurassic Coal-Bearing Mudstones in the Dameigou Area (Qaidam Basin, NW China): Implications for Paleoclimate, Paleoenvironment, and Organic Matter Accumulation.
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