Scientists have created a new global map that identifies which subduction zones are most capable of generating giant earthquakes.
The project comes nine years after the giant earthquake and tsunami in Sumatra in December 2004, which devastated the region and killed more than 200,000 people.
Since then two other giant earthquakes have occurred at subduction zones, one in Chile in February 2010 and one in Japan in March 2011, which both caused massive destruction, killed many thousands of people, and resulted in billions of dollars of damage.
Most earthquakes occur at the boundaries between tectonic plates that cover the Earth’s surface. The largest earthquakes on Earth only occur at subduction zones, plate boundaries where one plate sinks (subducts) below the other into the Earth’s interior.
So far, seismologists have recorded giant earthquakes for only a limited number of subduction zone segments. But accurate seismological records go back to only about 1900, and the recurrence time of giant earthquakes can be many hundreds of years.
“The main question is, are all subduction segments capable of generating giant earthquakes, or only some of them? And if only a limited number of them, then how can we identify these,” says Wouter Schellart, an associate professor in the School of Geosciences at Monash University, who led the international team.
Schellart and Professor Nick Rawlinson from the University of Aberdeen in Scotland used earthquake data going back to 1900 and data from subduction zones to map the main characteristics of all active subduction zones on Earth. They investigated if those subduction segments that have experienced a giant earthquake share commonalities in their physical, geometrical, and geological properties.
Their findings, published in the journal Physics of the Earth and Planetary Interiors, show that the main indicators include the style of deformation in the plate overlying the subduction zone, the level of stress at the subduction zone, the dip angle of the subduction zone, as well as the curvature of the subduction zone plate boundary and the rate at which it moves.
Schellart has identified several subduction zone regions capable of generating giant earthquakes, including the Lesser Antilles, Mexico-Central America, Greece, the Makran, Sunda, North Sulawesi, and Hikurangi.
Source: Monash University