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>Chromatograms of saturated fractions of extracts from Domanic rocks: Berezovskaya area before (a) and after (b) experiments; Zelenogorskaya area before (c) and after (d) experiments. Pr = pristane (i-C<sub>19</sub>); Ph = phytane (i-C<sub>20</sub>).</div>

Geofluids

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Figure 5

Figure 5: 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 5 | 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 