id	author	title	date	pages	extension	mime	words	sentence	flesch	summary	cache	txt
gc-1003	Radonjić, Miloš	Hyperpycnites within the Devonian-Carboniferous flysch of the Carpatho-Balkanides (Kostadinovica, eastern Serbia)	2020	12	.pdf	application/pdf	8481	448	53	(b) Upper part of unit B near the transi- tion into unit C. Two massive sandstone beds are marked as B23 and B25 and are truncated by normal faults (Fn). The onset of unit D is marked by a sharp change in facies association compared to unit C. Aside from the general similari- ties described above, differences within units A and D are most notably the rare occurrence of S3 facies (fine-grained sandstones with climbing ripples) within unit D. In terms of the lateral geometry of the proposed system at the Kostadinovica section, the change to more fine-grained litho- logies should mark the shift away from the central zone of super- imposed channel axes towards lobes of the system (from unit A towards unit C), while the opposite shift would mark migration G eologia C roatica Radonjić Miloš: Hyperpycnites within the Devonian-Carboniferous flysch of the Carpatho-Balkanides (Kostadinovica, eastern Serbia) 141 and plants could indicate repetitive hyperpycnal events trigger- ing (or coinciding with) turbiditic transport of the sediment rep- resenting several dozen events reflected as distinct sequences (at least within units A and D).	cache/gc-1003.pdf	txt/gc-1003.txt