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During this time in the named area along the Talas-Fergana fault minimum three strong earthquakes took place: about 6000 years, 4500 years and 400-500 years ago. , 2009). 3 Investigations in the Kara-Kasmak – Sary-Bulak interfluve In the interfluve of right inflows of the Karakuldzha-Chatkalskaya river (Dzhashilsai, Dzhosho and others) (Fig. 14A) there are no clear evidences of vertical differential displacements of the TFF walls. However in the south of the region the vertical component can be observed.

232-240, ISBN 0-12-440870-2, San Diego, USA Fliri, F. (1998). Naturchronik von Tirol, Wagner, ISBN 3-7030-0313-8, Innsbruck, Austria Fréchet, J. (2008). Past and Future of Historical Seismicity Studies in France. , M. Meghraoui & M. ; Molin, D. & Ciurletti, G. (2001). Searching for the source of the 1117 earthquake in northern Italy: A multidisciplinary approach. , Albini, P. and Francés, F. ), 3-27, Kluwer, ISBN 0792371542, Dordrecht, Netherlands Gießberger, H. (1922). Die Erdbeben Bayerns I.

Determining earthquake recurrence intervals from deformational structures in young lacustrine sediments. Tectonophysics, 29, 141-152. Şaroğlu, F. , 1986. Doğu Anadolu’da neotektonik dönemdeki jeolojik evrim ve havza modelleri. Bulletin of The Mineral Research and Exploration, 107, 73-94. C. , 1979. Post-collisional tectonics of the Turkish-Iranian Plateau and a comparison with Tibet. Tectonophysics, 55, 361–376. C. & Yılmaz, Y, 1981. Tethyan evolution of Turkey: a plate tectonic approach. Tectonophysics, 75, 181-241.

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Analysis of the Clinton Critical Experiment [declassified]

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