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

<div>Subsidence curve of the Makó Trough by Balázs et al. (2017) [<a href="/journals/geofluids/2020/9020684/#B37">37</a>] shows a very short and rapid synrift subsidence of the basement during early Late Miocene.</div>

Geofluids

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Figure 2: Porosity Development Controlled by Deep-Burial Diagenetic Process in Lacustrine Sandstones Deposited in a Back-Arc Basin (Makó Trough, Pannonian Basin, Hungary) 

Figure 2 | Porosity Development Controlled by Deep-Burial Diagenetic Process in Lacustrine Sandstones Deposited in a Back-Arc Basin (Makó Trough, Pannonian Basin, Hungary) 