@article {2176,
	title = {Αντιστοίχηση της γεωτεκτονικής θέσης των Κυθήρων και των Κυκλάδων στη γεωδυναμική εξέλιξη του ελληνικού τόξου},
	journal = {Δελτίο Ελληνικής Γεωλογικής Εταιρείας.Δελτίο Ελληνικής Γεωλογικής Εταιρείας.},
	volume = {XXV},
	number = {1},
	year = {1991},
	pages = {65-80},
	abstract = {The tectonic structure and evolution  of  Kythira  is  in general  similar  to that of the Cyclades with a difference in the chronologic succession of the  alpine  and  post  alpine geodynaaic processes  which   have   ended in  the  Cyclades  in contrast  to Kythira  where  they  are still in evolution.  A basic distinction has to be lade between the  early  phase  of compressional  tectonism   which  built  up  the alpine nappe pile and the late phase of extensional  character   which   denudates  the   non   metamorphic units  froa the crests of the anticlinal domes of the underlying netanorphic units.  During  this  late phase the decollement  and  sliding  of  the  non metanorphic units along  their contact with the underlying metamorphic units is dominant under the important effect of gravity, the normal  faults  being limited above the main overthrusts.},
	keywords = {Cythere, Kythira, Cyclades, compression, extension, Gravitational collapse},
	author = {Παπανικολάου, Δ. and Δανάμος, Γ.}
}
