Oceanography The Official Magazine of
The Oceanography Society
Volume 32 Issue 01

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Volume 32, No. 1
Pages 102 - 104

Tōhoku-oki Fault Zone Frictional Heat Measured During IODP Expeditions 343 and 343T

Patrick M. Fulton Emily BrodskyJames J. MoriFrederick M. Chester
Article Abstract

During the March 11, 2011, Mw 9.1 Tōhoku-oki earthquake, the plate boundary fault slipped an astonishing 50 m or more, with the slip extending all the way to the seafloor within the Japan Trench. The result was a much larger earthquake and tsunami than expected as well as considerable devastation on land. The earthquake challenged our understanding of subduction zone mechanics but also presented an opportunity to resolve long-standing questions regarding the amount of frictional resistance faults exhibit during earthquakes, resistance that influences the amount of fault slip and associated tsunami hazards. Here we report on how scientific ocean drilling successfully allowed the measurement of frictional heating within the fault zone that ruptured during the Tōhoku-oki earthquake.

Citation

Fulton, P.M., E. Brodsky, J.J. Mori, and F.M. Chester. 2019. Tōhoku-oki fault zone frictional heat measured during IODP Expeditions 343 and 343T. Oceanography 32(1):102–104, https://doi.org/10.5670/oceanog.2019.129.

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