Research Article

Paleofluid Fingerprint as an Independent Paleogeographic Correlation Tool: An Example from Pennsylvanian Sandstones and Neighboring Crystalline Rocks (Tisia Composite Terrane, S Hungary)

Figure 1

Regional geology. Simplified map of Variscan basement areas in W and Central Europe [1, 8] and geologic framework of the Carpathian–Pannonian area [1, 4]. Late Variscan age granitoids known in the Hungarian part of the Tisia are also indicated [2]. 1: Mecsek Mountains (Mórágy Complex), monzonite; 2: Danube–Tisza Interfluve, Kecskemét basement area, monzonite; 3: Battonya basement area, tonalite. Box indicates area studied in detail (see Figure 3(a)). MS: Moravo–Silesian (Brunovistulian) Zone; ALCAPA: Alpine–West Carpathian–Pannonian Block; SDU: Slavonia–Drava Unit.