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The aseismic Murray ridge (MR) is a continuation of the Owen fracture zone which marks the boundary between the Indian and Arabian plates. Due to large variation in morphology and structure within this NE–SW trending ridge in the Arabian Sea a large variation of the bathymetry from few hundred metres to about 4000m is seen. Observed seismicity on the ridge system is predominantly strike-slip. Tsu...

Effect of Murray ridge on the tsunami propagation from Makran subduction zone