Revealing the Mineralogical and Petrographic Signs of Fluid-Related Processes in the Kelebia Basement Area (Szeged Basin, S Hungary): A Case Study of Alpine Prograde Metamorphism in a Permo-Triassic Succession

<div>Tentative time–temperature path of the Kelebia basement area. According to Worden and Burley [<a href="/journals/geofluids/2023/8600576/#B57">57</a>], three conceptual regimes of diagenesis are indicated: (i) eogenesis (early diagenesis), (ii) mesogenesis (burial diagenesis), and (iii) telogenesis (uplift-related diagenesis).</div>

Geofluids

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Figure 11

Figure 11: Revealing the Mineralogical and Petrographic Signs of Fluid-Related Processes in the Kelebia Basement Area (Szeged Basin, S Hungary): A Case Study of Alpine Prograde Metamorphism in a Permo-Triassic Succession 

Figure 11 | Revealing the Mineralogical and Petrographic Signs of Fluid-Related Processes in the Kelebia Basement Area (Szeged Basin, S Hungary): A Case Study of Alpine Prograde Metamorphism in a Permo-Triassic Succession 