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The University of Southampton
Ocean and Earth Science, National Oceanography Centre Southampton

Western Indian Ocean earthquake and tsunami hazard potential greater than previously thought

Published: 15 May 2013
Arabian Sea, Makran subduction zone

Earthquakes similar in magnitude to the 2004 Sumatra earthquake could occur in an area beneath the Arabian Sea at the Makran subduction zone, according to research involving Gemma Smith, a Geology and Geophysics PhD student at University of Southampton.

The research, published in the Geophysical Research Letters, was carried out by scientists from the University of Southampton based at the National Oceanography Centre Southampton (NOCS) and the Pacific Geoscience Centre, which is part of the Canadian government's Natural Resources Canada department.

The study suggests that the risk from undersea earthquakes and associated tsunami in this area of the Western Indian Ocean – which could threaten the coastlines of Pakistan, Iran, Oman, India and potentially further afield – has been previously underestimated. The results highlight the need for further investigation of pre-historic earthquakes and should be fed into hazard assessment and planning for the region.

Subduction zones are areas where two of the Earth’s tectonic plates collide and one is pushed beneath the other. When an earthquake occurs here, the seabed moves horizontally and vertically as the pressure is released, displacing large volumes of water that can result in a tsunami.

The Makran subduction zone has shown little earthquake activity since a magnitude 8.1 earthquake in 1945 and magnitude 7.3 in 1947. Because of its relatively low seismicity and limited recorded historic earthquakes it has often been considered incapable of generating major earthquakes.

Plate boundary faults at subduction zones are expected to be prone to rupture generating earthquakes at temperatures of between 150 and 450 °C. The scientists used this relationship to map out the area of the potential fault rupture zone beneath the Makran by calculating the temperatures where the plates meet. Larger fault rupture zones result in larger magnitude earthquakes.

Makran earthquakes

"Thermal modelling suggests that the potential earthquake rupture zone extends a long way northward, to a width of up to 350 kilometres which is unusually wide relative to most other subduction zones," says Gemma Smith, lead author and PhD student at University of Southampton School of Ocean and Earth Science, which is based at NOCS.

The team also found that the thickness of the sediment on the subducting plate could be a contributing factor to the magnitude of an earthquake and tsunami there.

“If the sediments between the plates are too weak then they might not be strong enough to allow the strain between the two plates to build up,” says Smith. “But here we see much thicker sediments than usual, which means the deeper sediments will be more compressed and warmer. The heat and pressure make the sediments stronger. This results in the shallowest part of the subduction zone fault being potentially capable of slipping during an earthquake.

“These combined factors mean the Makran subduction zone is potentially capable of producing major earthquakes, up to magnitude 8.7-9.2. Past assumptions may have significantly underestimated the earthquake and tsunami hazard in this region.”adds Gemma who is a PhD student at the Graduate School of the National Oceanography Centre Southampton (GSNOCS).

 

 

Gemma Smith

These combined factors mean the Makran subduction zone is potentially capable of producing major earthquakes, up to magnitude 8.7-9.2. Past assumptions may have significantly underestimated the earthquake and tsunami hazard in this region.

Gemma Smith - Geology and Geophysics PhD student, University of Southampton

Notes for editors

Notes for editors

1. Reference: Smith, G.L., McNeill, L.C., Wang, K., He, J., and Henstock, T.J., 2013, Thermal structure and megathrust seismogenic potential of the Makran subduction zone: Geophys. Res. Lett., 40, doi:10.1002/grl.50374.

2. Gemma Smith is a PhD student at the Graduate School of the National Oceanography Centre Southampton (GSNOCS).

3. Image 1 shows the primary tectonic plates and plate boundaries in the Arabian Sea region and the geographic context.

4. Image 2 shows the location of the Makran subduction zone of Pakistan and Iran and locations of recorded earthquakes including the 1945 magnitude 8.1 earthquake (red dot to the north indicates the 1947 magnitude 7.3 earthquake). The profile for the thermal modelling of this study is the north-south trending black line, with distance given along the profile from the shallowest part of the subduction zone in the south (0 kilometres) to the most northern potential earthquake rupture extent (350 kilometres).

5. The University of Southampton is a leading UK teaching and research institution with a global reputation for leading-edge research and scholarship across a wide range of subjects in engineering, science, social sciences, health and humanities.  www.southampton.ac.uk

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