id	author	title	date	pages	extension	mime	words	sentence	flesch	summary	cache	txt
gc-188	Diamantopoulos, Anastasios	Plio–Quaternary Geometry and Kinematics of Ptolemais Basin (Northern Greece): Implications for the Intra-Plate Tectonics in Western Macedonia	2010	12	.pdf	application/pdf	5196	206	44	A significant difference in deforma- tion style between the Vegoritis–Ptolemais and Ptol- emais–Kozani sub-basins is indicated by their different strike and internal morphology, and by the greater depth and width of the Vegoritis–Ptolemais sub-basin. Given this evi- dence, the following must be considered in a new inter- pretation of the structural evolution of the Ptolemais basin: a) a westward tilting of the sedimentary fill in the Ptole- mais–Kozani sub-basin and a west–northwestward tilting of the sedimentary fill in the Vegoritis–Ptole- mais sub-basin; b) a rhomb-like morphology of the Ptolemais–Kozani sub-basin (DIAMANTOPOULOS & DIMITRAKO- POULOS, 2004a); c) the left-lateral strike-slip fault in the western margin- al domain (DIAMANTOPOULOS, 2004); d) the co-existence of reverse and normal faults in all mines of the PPC; e) anticline structures with a NE–SW axis trend in the internal parts of the basin; f) the kinematics of the deformation of Pliocene lignites in the boundary between the Ptolemais–Kozani and Vegoritis–Ptolemais sub-basins (DIAMANTOPOU- LOS & DIMITRAKOPOULOS, 2004b); g) the deformation partitioning between the marginal zones of the basin (DIAMANTOPOULOS, 2004); h) the thickness variation of the Pliocene lignites and of the Plio–Quaternary sediments; i) the different stratigraphy and sub-surface morphol- ogy between the Ptolemais–Kozani and Vegoritis– Ptolemais sub-basins, making the stratigraphic cor- relations difficult (DIAMANTOPOULOS & DIMI- TRAKOPOULOS, 2004a), and j) the Quaternary ductile–brittle deformation of the basement-units in eastern Askion and the eastern Vernon mountains (DIAMANTOPOULOS, 2005).	cache/gc-188.pdf	txt/gc-188.txt