Abstract
The provenance of the Proč and Strihovce sandstones is crucial for understanding the relationship between the Pieniny Klippen (PKB) and Flysch (FB) belts in the easternmost part of the Western Carpathian realm. Detrital Cr-spinels in these tectonic units were assertively interpreted as sourced from the southern sources representing the Meliata mélange. In this study, we use the geochemistry of detrital chromian spinels to identify the mafic and ultramafic source of the sediments and to compare them each other. Simultaneously, we compare their chemical compositions with those from the different Western Carpathian geological units, which could feed the Proč and Krynica basins during the Paleogene, where the Proč and Strihovce formations (fms), respectively, were deposited. Chromian spinels from the Proč and Strihovce fms exhibit similar geochemical characteristics (Cr# = 0.44–0.88 and 0.29–0.89, Mg# = 0.17–0.68 and 0.2–0.72, TiO2 = 0.0–3.67 and 0.01–2.08 wt.%, respectively). The spinels show both supra-subduction zone (SSZ) peridotite signatures and volcanic origin. Whereas volcanic spinels from the Proč Formation (Fm.) were formed under an ocean island basalt (OIB) and back-arc basin basalt (BABB) geodynamic setting, those from the Strihovce Fm. suggest a predominantly mid-ocean ridge basalt (MORB) origin. To avoid mistakes in the provenance interpretations, the data from garnet geochemistry of both formations is supplied. The analysed Cr-spinels do not absolutely overlap with spinels reported from the Meliata Unit, and their composition indicates at least two independent sources.
Highlights
Heavy mineral (HM) analysis has remained a useful method in the study of sediments
Chromian spinel compositions were plotted in various discriminatory diagrams and compared with existing geochemical Cr-spinel data from Western Carpathian spinel-bearing rocks
Rounded spinels are very scarce in the Proč Fm., whereas these are more common in the Strihovce Fm. deposits
Summary
Heavy mineral (HM) analysis has remained a useful method in the study of sediments. Weathering, transport and diagenetic conditions at the depositional site significantly influence the composition of heavy mineral suites. These processes may modify the original sediment composition and complicate the provenance interpretations [5,6]. Suitable solutions seem to focus on the chemical composition of mineral species, such as garnet [7,8,9,10], tourmaline [11], rutile [12] or Cr-spinel [13,14,15], etc. We focused predominantly on Cr-spinel geochemistry and garnet composition. These detrital minerals seem to be appropriate for specifying the potential
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