A New Azhdarchid Pterosaur from the Late Cretaceous of the Transylvanian Basin, Romania: Implications for Azhdarchid Diversity and Distribution (original) (raw)
Figure 2
Geological map of the Sebes area.
This map is re-drawn from [13], updated and modified: F- SbG/B vertebrate site -the type locality; 1- metamorphic basement (Getic-Supragetic nappe system); 2- Upper Cretaceous (Santonian-Latest Campanian) marine deposits referred to the Bozeş Formation in the base with locally developed coal-bearing fluvial-deltaic facieses referred to “Sebeşel strata”; 3- Transitional deltaic (a) or estuarian-paludal (b) facieses marking the top Bozeş Formation; 4- Upper Cretaceous (Latest Campanian-Maastrichtian/Paleocene?) continental units referred to the Sebeş or Şard (in part) Formations; 5- Undifferentiated Paleogene (Eocene-Oligocene) units referred to Şard (in part), Ighiu and Bărăbanţ Formations; 6- Undifferentiated Miocene and Pliocene marine units referred to the Sîntimbru, Dej and Lopadea Formations; 7- Quaternary cover; 8- Settlements; 9- Faults; 10- Anticlines; 11- Synclines; 12- Dip and strike; 13- Nappe Front.