@article {Coleman2019,
	title = {{Along-strike consistency of an extensional detachment system, West Cyclades, Greece}},
	journal = {Terra Nova},
	volume = {31},
	number = {3},
	year = {2019},
	abstract = {{\textcopyright} 2019 John Wiley \& Sons Ltd The Lavrion district of the Attica Peninsula, Greece, exposes the West Cycladic Detachment System (WCDS), a low-angle crustal-scale extensional fault system separating tectonostratigraphic units of the Cycladic Blueschist Unit. New multiple single-grain fusion and step-heated white mica 40 Ar/ 39 Ar ages integrated with existing (U{\textendash}Th)/He ages and independent paleothermometry resolves a syn- to post-orogenic deformation history. A structurally higher unit records Oligocene greenschist facies deformation that evolved into brittle conditions by the middle Miocene, and shares a similar history to Serifos at the southern end of the detachment system. The structurally lowest unit remained ductile until the late Miocene, preserving pervasive post-orogenic structures, similar to along-strike structures at the centre, deepest part of the fault. The similarities of structural styles and the timing of deformation across >~150~km of strike length of the detachment system indicates tens of kilometers of offset and extraordinary potential for correlating observations along Cycladic-style detachment systems.},
	issn = {13653121},
	doi = {10.1111/ter.12388},
	author = {Coleman, M. and Dubosq, R. and Schneider, D.A. and Grasemann, B. and Soukis, K.}
}
