Multistage Hydrocarbon Generation of Saline Lacustrine Source Rocks in Hydrous Pyrolysis: Insights from Clay Mineral-Organic Matter Interactions.

The isomerization ratio shows nonmonotonic changes with increasing temperature, including a decreasing trend at 25–250 and 300–350 °C and an increasing trend at 250–300 and 350–500 °C ( Figure 6 a–d). 3.3 Rock-Eval analysis The Rock-Eval parameters of original and residual solids are shown in Figure 7 .

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