Slip-rate variability and distributed deformation in the Marmara Sea fault system
Author:
Publisher
Springer Science and Business Media LLC
Subject
General Earth and Planetary Sciences
Link
http://www.nature.com/articles/ngeo739.pdf
Reference22 articles.
1. Scholz, C. H. The Mechanics of Earthquakes and Faulting 2nd edn (Cambridge Univ. Press, 2002).
2. Le Pichon, X. L., Chamot-Rooke, A., Rangin, C. & Şengör, A. M. C. The North Anatolian fault in the Sea of Marmara. J. Geophys. Res. 108, 2179 (2003).
3. Flerit, F., Armijo, R., King, G. & Meyer, B. The mechanical interaction between the propagating North Anatolian Fault and the back-arc extension in the Aegean. Earth Planet. Sci. Lett. 224, 347–362 (2004).
4. Meade, B. J. et al. Estimates of seismic potential in the Marmara Sea region from block models of secular deformation constrained by GPS measurements. Bull. Seism. Soc. Am. 92, 208–215 (2002).
5. Reilinger, R. et al. GPS constraints on continental deformation in the Africa–Arabia–Eurasia continental collision zone and implications for the dynamics of plate interaction. J. Geophys. Res. 111, B05411 (2006).
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