Abstract ref. 2029:
Reef limestones of the Suva Planina region and similar organic limestones of eastern Serbia, Yugoslavia, represent continuous sedimentation from Tithonian (Jurassic) to Valanginian (Cretaceous) time. Two types can be distinguished--reef deposits and lateral equivalents formed in deeper waters. Transgression was widespread, and deposition of thick sequences of limestone was due to gradual subsidence of the depositional basin during epeirogenic crustal movements. 