Porosity Development Controlled by Deep-Burial Diagenetic Process in Lacustrine Sandstones Deposited in a Back-Arc Basin (Makó Trough, Pannonian Basin, Hungary)

<div>Seismic section of studied wells and core intervals (colored and empty squares) [<a href="/journals/geofluids/2020/9020684/#B41">41</a>] along the line shown in Figure <a href="../fig1/">1</a>. Porosity and permeability ranges were measured on core samples from the Makó Trough (TXM interim report).</div>

Geofluids

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Figure 4

Figure 4: Porosity Development Controlled by Deep-Burial Diagenetic Process in Lacustrine Sandstones Deposited in a Back-Arc Basin (Makó Trough, Pannonian Basin, Hungary) 

Figure 4 | Porosity Development Controlled by Deep-Burial Diagenetic Process in Lacustrine Sandstones Deposited in a Back-Arc Basin (Makó Trough, Pannonian Basin, Hungary) 