A Nagoya University-led team reveals the mechanisms behind different earthquakes at a plate boundary on the west coast of South America, shedding light on historical seismic events and potentially aiding prediction of the future risk from these natural disasters.
press released on April 26, 2017
Figure: A comparison between the previous source model and our model of the large earthquakes along the Ecuador-Colombia subduction zone. (Left) The previous source model of the large earthquakes in this subduction zone. The 1906 earthquake has been interpreted as a megathrust event (Mw 8.8) ruptured all segments of 1942, 1958, and 1979 earthquakes. (Right) Our source model of the large earthquakes in this subduction zone. Our analysis of the 1906 earthquake indicated Mw 8.4 and the occurrence of the large slip near the trench (black triangles with line) off the source areas of the three earthquakes. ©Masahiro Yoshimoto
Nagoya, Japan - When tectonic plates that have been sliding past each other get stuck, a huge amount of energy builds up, and is eventually released in the form of an earthquake. Although much is known about the mechanisms behind this process, more needs to be understood about what happens at particular plate boundaries to determine the risk of earthquakes and tsunamis at specific sites and potentially to predict when these events might occur.
In a breakthrough in this field, researchers at Nagoya University and their colleagues in South America have studied several earthquakes that occurred at the Ecuador-Colombia subduction zone over the last hundred years, revealing the relationships between different earthquakes and the size and location of the ruptures at plate boundaries that caused them. The findings were published in Geophysical Research Letters.
The team used a combination of data sources and models to study large earthquakes that struck the west coast of South America in 1906, 1942, 1958, 1979, and 2016. These included information on tsunami waveforms recorded at sites across the Pacific, data on seismic waves obtained by monitoring stations in Ecuador and Colombia, and previous work on the intensity of coupling, or locking together, of adjacent plates and the distance that they slipped past each other to cause each earthquake.
"The Ecuador-Colombia subduction zone, where the Nazca plate passes underneath the South American plate, is particularly interesting because of the frequency of large earthquakes there," says study author Hiroyuki Kumagai of the Graduate School of Environmental Studies, Nagoya University. "It's also a good site to investigate whether the ruptures at plate boundaries causing huge earthquakes are linked to subsequent large earthquakes years or decades later."
By carefully modeling the fault area where these earthquakes arose in combination with the other data, the team showed that the strongest of the earthquakes, that of 1906, involved a rupture at a different site than the other earthquakes. They also used data on the known speed at which the plates are moving past each other and the simulated "slip" of a plate associated with the 2016 earthquake to show that the 1942 and 2016 earthquakes were triggered by ruptures at the same site.
"Now that we can precisely link previous earthquakes to ruptures at specific sites along plate boundaries, we can gauge the risks associated with the build-up of pressure at these sites and the likely frequency of earthquakes there," lead author Masahiro Yoshimoto says. "Our data also reveal for the first time differences in rupture mechanisms between oceanic trenches and deeper coastal regions in this subduction zone."
The findings provide a foundation for risk prediction tools to assess the likelihood of earthquakes and tsunamis striking this region and their potential periodicity and intensity.
The article "Depth-dependent rupture mode along the Ecuador-Colombia subduction zone" was published in Geophysical Research Letters at doi: 10.1002/2016GL071929.
Masahiro Yoshimoto 1, Hiroyuki Kumagai 1, Wilson Acero 2, Gabriela Ponce 2 , Freddy Vásconez 2, Santiago Arrais 2, Mario Ruiz 2 , Alexandra Alvarado 2 , Patricia Pedraza García 3, Viviana Dionicio 3, Orlando Chamorro 3, Yuta Maeda 1, and Masaru Nakano 4
1 Graduate School of Environmental Studies, Nagoya University, Nagoya, Japan
2 Instituto Geofísico, Escuela Politécnica Nacional, Quito, Ecuador
3 Servicio Geológico Colombiano, Bogota, Colombia
4 Japan Agency for Marine-Earth Science and Technology, Yokohama, Japan
Graduate School of Environmental Studies, Nagoya University
Instituto Geofísico, Escuela Politécnica Nacional, Quito, Ecuador
Servicio Geológico Colombiano, Bogota, Colombia
Funding: This work was supported by the Science and Technology Research Partnership for Sustainable Development (SATREPS) project in Colombia under the sponsorship of the Japan Science and Technology Agency (JST) and the Japan International Cooperation Agency (JICA) and the JICA technical cooperation project in Ecuador.