**Tsunami Generation**

[9] Smith, G. L., McNeill, L.C., Wang, K., He, J., Henstock T.J., 2013. Thermal structure and megathrust seismogenic potential of the Makran subduction zone, Geophysical

[10] Byrne, D. E., Sykes, L. R., Davis, D. M., 1992. Great thrust earthquakes and aseismic slip along the plate boundary of the Makran subduction zone, Journal of Geophysical

[11] Mokhtari M, Abdollahie Far I, Hessami K., 2008. Structural elements of the Makran region, Oman Sea and their potential relevance to tsunamigenisis. Natural Hazards,

[12] Heidarzadeh, M., Pirooz, M.D., Zaker, N.H. and Synolakis, C.E., 2008b. Evaluating tsunami hazard in the northwestern Indian Ocean. Pure and Applied Geophysics,

[13] Scawthorn, C. and Porter, K. A. (2011) Reconnaissance Report Aspects of the 11 March 2011 Eastern Japan Earthquake and Tsunami, SPA Risk., http://www.sparisk.com/

[14] Plafker, G. 1972. Alaskan earthquake of 1964 and Chilean earthquake of 1960: Impli‐

[15] Mokhtari M, 2011. Tsunami in Makran Region and its effect on the Persian Gulf, In edited by Mokhtari M, Tsunami - a growing disaster, InTech Publication, Open book publication. http://www.intechopen.com/books/show/title/tsunami-a-growing-

[16] Heidarzadeh, M. and Satake, K., 2014a. Possible sources of the tsunami observed in the northwestern Indian Ocean following the 2013 September 24 Mw 7.7 Pakistan inland

cations for arc tectonics. Journal of Geophysical Research, 77(5), 901-925.

earthquake. Geophysical Journal International, 199(2), 752-766.

Research Letters, 40, 1–6.

Research, 97(B1), 449–478.

165(11-12), 2045-2058.

pubs/SPA-2011-Tohoku-Report.pdf

47, 185–199.

10 Tsunami

disaster
