Post-5 Ma rock deformation on Alonnisos (Greece) constrains the propagation of the North Anatolian Fault
Author:
Funder
European Commission
Horizon 2020
Publisher
Elsevier BV
Subject
Earth-Surface Processes,Geophysics
Reference46 articles.
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2. Westward propagation of the North Anatolian fault into the northern Aegean: timing and kinematics;Armijo;Geology,1999
3. The North Anatolian Fault Zone, Paper Presented at Annales Tectonicae;Barka,1992
4. Interaction between trench retreat and Anatolian escape as recorded by neogene basins in the northern Aegean Sea;Beniest;Mar. Pet. Geol.,2016
5. Structure and evolution of the Sporadhes basin of the North Aegean trough, northern Aegean Sea;Brooks;Tectonophysics,1980
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1. Late Quaternary deformation in the western extension of the North Anatolian Fault (North Evia, Greece): Insights from very high-resolution seismic data (WATER surveys);Tectonophysics;2024-01
2. The Development of Fault Networks at the Termination of Continental Transform Faults When Their Connecting Plate Boundary Is “Misaligned”;Tectonics;2023-10
3. Evolution of the North Anatolian Fault from a diffuse to a localized shear zone in the North Aegean Sea during the Plio-Pleistocene;Geophysical Journal International;2023-09-18
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