@ARTICLE{Kotowski_Jakub_Detrital_2023,
 author={Kotowski, Jakub and Olszewska-Nejbert, Danuta and Nejbert, Krzysztof},
 volume={vol. 73},
 number={No 4},
 journal={Acta Geologica Polonica},
 pages={801-832},
 howpublished={online},
 year={2023},
 publisher={Komitet Nauk Geologicznych PAN},
 publisher={Wydział Geologii UW},
 abstract={The potential of heavy minerals as a provenance tracer in Albian arenites of extra-Carpathian Poland was assessed. Studies in this area have focused on various methods based on heavy mineral chemistry that provide an effective tool for reconstructing the provenance of quartz-rich sediments. The previously suggested division of the study area into two domains with different source areas: the western domain – the Miechów area, and the eastern domain – the Lublin area, was based on geochronological (monazite and muscovite dating) and rutile mineral chemical studies. The mineral chemistry of newly examined heavy minerals supports the previously suggested division. The mineral chemistry of detrital tourmaline suggests medium-grade metamorphic rocks as the main source in both domains. Detrital garnet in the western domain shows affiliation to the Góry Sowie Massif, while garnet in the eastern domain was most probably sourced from southern/central Norway. The western domain was most probably fed from rocks of the Bohemian Massif. The main source area for the eastern domain was most probably located in the Baltic Shield. The distinct division of the study area into two domains was caused by the palaeogeography of the region in the Albian and the action of longshore currents in south-eastward and eastward directions. Supplementary Material 1 Supplementary Online Material 2},
 type={Article},
 title={Detrital heavy minerals as guides to provenance of Albian arenites of southern extra-Carpathian Poland},
 URL={http://journals.pan.pl/Content/129849/PDF/13_Kotowski.pdf},
 doi={10.24425/agp.2023.148023},
 keywords={Detrital material, Mineral chemistry, Provenance, Stability of heavy minerals, Sand and sandstone, Lower Cretaceous},
}