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Page 1: Home | Earth-prints · reasonable travel-time residuals. The 1928 Sabukia valley earthquake is the earliest and laruest (M = 6.9) shock in the Gre- gory rift (Ambraseys, 1991b) to
Page 2: Home | Earth-prints · reasonable travel-time residuals. The 1928 Sabukia valley earthquake is the earliest and laruest (M = 6.9) shock in the Gre- gory rift (Ambraseys, 1991b) to
Page 3: Home | Earth-prints · reasonable travel-time residuals. The 1928 Sabukia valley earthquake is the earliest and laruest (M = 6.9) shock in the Gre- gory rift (Ambraseys, 1991b) to
Page 4: Home | Earth-prints · reasonable travel-time residuals. The 1928 Sabukia valley earthquake is the earliest and laruest (M = 6.9) shock in the Gre- gory rift (Ambraseys, 1991b) to
Page 5: Home | Earth-prints · reasonable travel-time residuals. The 1928 Sabukia valley earthquake is the earliest and laruest (M = 6.9) shock in the Gre- gory rift (Ambraseys, 1991b) to
Page 6: Home | Earth-prints · reasonable travel-time residuals. The 1928 Sabukia valley earthquake is the earliest and laruest (M = 6.9) shock in the Gre- gory rift (Ambraseys, 1991b) to
Page 7: Home | Earth-prints · reasonable travel-time residuals. The 1928 Sabukia valley earthquake is the earliest and laruest (M = 6.9) shock in the Gre- gory rift (Ambraseys, 1991b) to
Page 8: Home | Earth-prints · reasonable travel-time residuals. The 1928 Sabukia valley earthquake is the earliest and laruest (M = 6.9) shock in the Gre- gory rift (Ambraseys, 1991b) to
Page 9: Home | Earth-prints · reasonable travel-time residuals. The 1928 Sabukia valley earthquake is the earliest and laruest (M = 6.9) shock in the Gre- gory rift (Ambraseys, 1991b) to
Page 10: Home | Earth-prints · reasonable travel-time residuals. The 1928 Sabukia valley earthquake is the earliest and laruest (M = 6.9) shock in the Gre- gory rift (Ambraseys, 1991b) to
Page 11: Home | Earth-prints · reasonable travel-time residuals. The 1928 Sabukia valley earthquake is the earliest and laruest (M = 6.9) shock in the Gre- gory rift (Ambraseys, 1991b) to
Page 12: Home | Earth-prints · reasonable travel-time residuals. The 1928 Sabukia valley earthquake is the earliest and laruest (M = 6.9) shock in the Gre- gory rift (Ambraseys, 1991b) to
Page 13: Home | Earth-prints · reasonable travel-time residuals. The 1928 Sabukia valley earthquake is the earliest and laruest (M = 6.9) shock in the Gre- gory rift (Ambraseys, 1991b) to
Page 14: Home | Earth-prints · reasonable travel-time residuals. The 1928 Sabukia valley earthquake is the earliest and laruest (M = 6.9) shock in the Gre- gory rift (Ambraseys, 1991b) to