<?xml version="1.0" encoding="UTF-8"?><xml><records><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Coleman, M.</style></author><author><style face="normal" font="default" size="100%">Dubosq, R.</style></author><author><style face="normal" font="default" size="100%">Schneider, D.A.</style></author><author><style face="normal" font="default" size="100%">Grasemann, B.</style></author><author><style face="normal" font="default" size="100%">Soukis, K.</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">{Along-strike consistency of an extensional detachment system, West Cyclades, Greece}</style></title><secondary-title><style face="normal" font="default" size="100%">Terra Nova</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2019</style></year></dates><number><style face="normal" font="default" size="100%">3</style></number><volume><style face="normal" font="default" size="100%">31</style></volume><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">© 2019 John Wiley &amp; 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–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 &gt; 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.</style></abstract></record></records></xml>