Reference : Westward propagation of the North Anatolian fault into the northern Aegean: Timing an...
Scientific journals : Article
Physical, chemical, mathematical & earth Sciences : Earth sciences & physical geography
http://hdl.handle.net/2268/77785
Westward propagation of the North Anatolian fault into the northern Aegean: Timing and kinematics
English
Armijo, R. [> >]
Meyer, B. [> >]
Hubert, Aurelia mailto [Université de Liège - ULg > Département de géographie > Géomorphologie >]
Barka, A. [> >]
1999
Geology
Geological Society of America
27
267-270
Yes (verified by ORBi)
International
0091-7613
Boulder
CO
[en] North Anatolian Fault ; Marmara Sea ; Tectonics
[en] We present new evidence for the propagation processes of the North Anatolian fault. Fold-
ing in the Dardanelles Straits region allows us to document the timing of the deformation pre- ceding, and the finite displacement after, the passage of the propagating tip of the fault. The accuracy of the observations is due to interplay between deformation and the sea-level changes in the Mediterranean (the well-known Messinian regression followed by the Pliocene transgres- sion). The long-term kinematics around the Sea of Marmara pull-apart (total displacement of about 85 km over the past 5 m.y.) is similar to the present-day kinematics deduced from space geodesy. At a larger scale, westward propagation of the North Anatolian fault over nearly 2000 km in the past 10 m.y. appears to be associated with strain recovery, suggesting that the continental lithosphere retains long-term elasticity.
http://hdl.handle.net/2268/77785

File(s) associated to this reference

Fulltext file(s):

FileCommentaryVersionSizeAccess
Open access
Geology99_Dardanelles.pdfPublisher postprint1.15 MBView/Open

Bookmark and Share SFX Query

All documents in ORBi are protected by a user license.