Subduction zone geometry: Mega-earthquake risk indicator

At the point where two tectonic plates converge, an area known as the subduction zone can form where one of the plates passes on top of the other. Rocks do not slide over one another easily and the movement of tectonic plates can be blocked along the entire length of such interaction zones for periods exceeding a thousand years. This 'slip deficit' results in an accumulation of energy, which is released abruptly during earthquakes.

A theory that held sway for many years suggested that mega-earthquakes mostly occurred in subduction zones where plates converged rapidly and those where the subducting plate was relatively young. However, the mega-earthquakes of Sumatra-Andaman in 2004 and Tohoku-Oki in 2011, which generated deadly tsunamis, go against this theory: in the first case, the speed of plate movement is relatively slow (3 to 4 cm per year) and in the second, the Pacific plate that subducts under Japan is more than 120 million years old. A new question therefore arose: can all subduction zones generate mega-earthquakes?

In this new study, the researchers examined another parameter: subduction zone geometry. By comparing the degree of curvature of the subducting plates in great historical earthquakes, they discovered that the maximum magnitude of earthquakes recorded in each subduction zone was inversely proportional to the degree of curvature of the fault. In other words, the flatter the contact between the two plates, the more likely it is that mega-earthquakes will occur.

Earthquakes take place once the energy accumulated as a result of the slip deficit exceeds a certain threshold. The researchers showed that the greater the curvature of the subduction fault, the more this threshold varies along the subduction zone. A heterogeneous threshold produces more frequent earthquakes, but these affect a smaller spatial area and are therefore of lower magnitude. In contrast, a homogeneous rupture threshold over a large portion of a fault has a greater chance of resulting in a simultaneous rupture of the whole blocked zone and, consequently, a greater chance of generating a mega-earthquake.

As a consequence, subduction zones such as the Philippines, Salomon Islands or Vanuatu do not appear likely to generate mega-earthquakes. Others, however, such as Peru, Java or Mexico, which have not seen very large earthquakes over the last 200-300 years, appear to have all the necessary characteristics for a mega-earthquake in the future.