From: Formation of an intra-orogenic transtensional basin: the Neogene Wagrain basin in the Eastern Alps
 | Basal Breccia | Red Conglomerate | Base coarse Conglomerate | High coarse Conglomerate | Conglomerate/sandstone |
---|---|---|---|---|---|
Intraformational sandstone | – | 7 | – | – | 7 |
Quartz sandstone | 8 |  | – | – | – |
Dolomite | – | 2 | – | 4 | – |
Dark-grey phyllite | 29 | 12 | 7 | 2 | 7 |
Bright calcareous phyllite | 59 | – | 2 | – | – |
Dark quartzite | – | – | 4 | – | – |
Vein quartz | 4 | 20 | 26 | 36 | 38 |
Micaschist | – | 20 | 13 | 12 | 3 |
Quartzitic schist | – | 22 | 30 | 26 | 30 |
Orthogneiss | – | 12 | 17 | 19 | 15 |
Pegmatite gneiss | – | 5 | 1 | 1 | – |