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

<div>Chrono- and lithostratigraphy of the sedimentary rocks in the Makó Trough. The lithology is indicated by mirrored gamma logs [<a href="/journals/geofluids/2020/9020684/#B25">25</a>, <a href="/journals/geofluids/2020/9020684/#B35">35</a>].</div>

Geofluids

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Figure 3: Porosity Development Controlled by Deep-Burial Diagenetic Process in Lacustrine Sandstones Deposited in a Back-Arc Basin (Makó Trough, Pannonian Basin, Hungary) 

Figure 3 | Porosity Development Controlled by Deep-Burial Diagenetic Process in Lacustrine Sandstones Deposited in a Back-Arc Basin (Makó Trough, Pannonian Basin, Hungary) 