Fig. 9
From: Miocene syn-rift lacustrine sediments in the Mecsek Mts. (SW Hungary)
Structural features in the lacustrine deposits in the western Mecsek. a Vertically tilted conglomerate-sandstone succession of the Pécsvárad Limestone Mb. with syn-sedimentary tensional cracks (Abaliget). b Cracks (shown by arrows) only cut the conglomerate beds and do not continue into the sandstones. c Cracks (shown by arrows) in the bedding plane of a conglomerate bed running between the clasts. d Present orientation of cracks (green solid line) and bedding (yellow dashed line). e Original orientation of cracks acquired by backtilting with bedding. f, g Tensional fractures in Middle Triassic dolomite filled with the directly overlying Komló Claymarl (Abaliget)