Influence of Hydrothermal and Pyrolysis Processes on the Transformation of Organic Matter of Dense Low-Permeability Rocks from Domanic Formations of the Romashkino Oil Field

<div>EPR spectra of rock samples of Berezovskaya (a, c) and Zelenogorskaya (b, d) areas after pyrolytic heating at different temperatures.</div>

Geofluids

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Figure 7

Figure 7: Influence of Hydrothermal and Pyrolysis Processes on the Transformation of Organic Matter of Dense Low-Permeability Rocks from Domanic Formations of the Romashkino Oil Field 

Figure 7 | Influence of Hydrothermal and Pyrolysis Processes on the Transformation of Organic Matter of Dense Low-Permeability Rocks from Domanic Formations of the Romashkino Oil Field 