From University of Tsukuba (筑波大学 Tsukuba daigaku)(JP): “New Model Reveals Previously Unrecognized Complexity of Oceanic Earthquake Zones”

From University of Tsukuba (筑波大学, Tsukuba daigaku)(JP)

Dec 09, 2020 [Just now in social media]

Assistant Professor OKUWAKI Ryo
Mountain Science Center, Faculty of Life and Environmental Sciences,
University of Tsukuba (JP)
rokuwaki@geol.tsukuba.ac.jp

University of Tsukuba researchers have developed a state-of-the-art model, which has revealed major complexity in rupture processes even in simple oceanic faults.

Researchers from the University of Tsukuba applied seismic data from around the world to build a model of the 2020 Caribbean earthquake. Oceanic transform faults are generally considered to be linear and simple and have been widely used in studies of earthquake dynamics. However, the research team found that high complexity in rupture speed and direction can occur even in a supposedly simple linear fault system.

On 28 January 2020, a large oceanic earthquake with magnitude 7.7 occurred at the Oriente transform fault in the Caribbean Sea, between Jamaica and Cuba. It caused a minor tsunami of 0.11 m height and was felt as far afield as Florida.

A research team at the University of Tsukuba have developed a new finite-fault inversion method for building models based on teleseismic waveform data from earthquake monitoring stations. This new approach to using the data takes a more flexible approach to resolving the fault geometry. Rather than relying on prior assumptions, the faulting components are separately evaluated in a wider model in both time and space, allowing all possible rupture evolutions to be considered. The team were keen to use the Caribbean earthquake to help to understand the faulting processes that occur during these shallow oceanic quakes.

“Some cases of complex rupture dynamics have recently been reported in previous earthquake studies, raising the question of whether or not we are correctly modeling these even in supposedly simple fault systems,” says study author Professor Yuji Yagi. “The initial monitoring of this January 2020 event suggested variations in the waveform shape between two stations at similar distances from the epicenter, suggesting that there remains complexity to be explored at this fault.”

This was an excellent opportunity to test the new method developed by the team, which used data from 52 seismic stations to construct a detailed model of the geophysical processes within the fault that gave rise to the earthquake.

“The results revealed complex rupture during the earthquake, caused by a bend in the fault that led to the changes in rupture speed and direction detected in the monitoring data,” explains author Professor Ryo Okuwaki. “These variations triggered several successive rupture episodes that occurred along the 300-km-long fault.” The modeling approach also allows some suggestions to be made about the possible occurrence of subsidence and the shape of the surrounding seabed following the earthquake event.

These findings reveal that oceanic transform faults, considered to be simple and linear, may be much more complicated than previously accepted, and therefore require a more comprehensive approach to earthquake modeling. This work will shed light on a possible interaction between the earthquake-fault motion and the evolution of the ocean floor around the transform boundary.

1
Overview of the study area and the schematic illustration of interaction of fault motion and the seafloor subsidence.

Science paper:
“Rupture Process of the 2020 Caribbean Earthquake along the Oriente Transform Fault, Involving Supershear Rupture and Geometric Complexity of Fault”
Geophysical Research Letters

See the full article here.

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The University of Tsukuba (筑波大学, Tsukuba daigaku) (JP), located in Tsukuba, Ibaraki, is one of the prestigious national universities (established by Japanese Government). The university has 28 college clusters and schools with around 16,500 students (as of 2014). The main Tsukuba campus covers an area of 258 hectares (636 acres), making it the second largest single campus in Japan. The branch campus is in Bunkyo-ku, Tokyo, which offers graduate programs for working adults in the capital and manages K-12 schools in Tokyo that are attached to the university.

The university’s academic strength is in STEMM fields (Science, Technology, Engineering, Mathematics, Medicine), physical education, and related interdisciplinary fields. It is by taking located in Tsukuba Science City which has more than 300 research institutions. The university has had three Nobel laureates (two in Physics and one in Chemistry, see also “History”), and about 70 athletes, their students and alumni, have participated in the Olympic Games.

It has established interdisciplinary Ph.D. programs in Human Biology and Empowerment Informatics, and the International Institute for Integrative Sleep Medicine, which were created through the Ministry of Education, Culture, Sports, Science and Technology’s competitive funding projects.

Its Graduate School of Life and Environmental Sciences is represented on the national Coordinating Committee for Earthquake Prediction.

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