detrital garnet

GARNET PROVENANCE IN MIXED FIRST-CYCLE AND POLY-CYCLE HEAVY-MINERAL ASSEMBLAGES OF THE ROPIANKA AND MENILITE FORMATIONS (SKOLE NAPPE, POLISH FLYSCH CARPATHIANS): CONSTRAINTS FROM CHEMICAL COMPOSITION AND GRAIN MORPHOLOGY

Dorota SALATA

Institute of Geological Sciences, Jagiellonian University, Oleandry 2a, 30-063 Kraków, Poland; -mail: dorota.salata at uj.edu.pl.

SOURCE ROCKS FOR HEAVY MINERALS IN LOWER PART OF MENILITE FORMATION OF SKOLE NAPPE (POLISH FLYSCH CARPATHIANS), BASED ON STUDY OF DETRITAL GARNET AND TOURMALINE

Dorota SALATA

Institute of Geological Sciences, Jagiellonian University, Oleandry 2a, 30-063 Kraków, Poland; e-mail: dorota.salata at uj.edu.pl

Salata, D., 2013. Source rocks for heavy minerals in lower part of Menilite Formation of Skole Nappe (Polish Flysch Carpathians), based on study of detrital garnet and tourmaline. Annales Societatis Geologorum Poloniae, 83: 1–17.

DETRITUS FROM VARISCAN LOWER CRUST IN ROTLIEGEND SANDSTONES OF THE INTRA-SUDETIC BASIN, SW POLAND, REVEALED BY DETRITAL HIGH-PYROPE GARNET

Julita BIERNACKA

Institute of Geology, University of Poznań, Maków Polnych 16, 61-606 Poznań, Poland, e-mail: julbier at amu.edu.pl

Biernacka, J., 2012. Detritus from Variscan lower crust in Rotliegend sandstones of the Intra-Sudetic Basin, SW Poland, revealed by detrital high-pyrope garnet. Annales Societatis Geologorum Poloniae, 82: 127–138.