Predictable seismic cycles result from structural rupture barriers on oceanic transform faults

Science
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Abstract

Earthquakes of magnitude (M) >5.5 on oceanic transform faults (OTFs) repeatedly rupture the same locked patches, sometimes quasiperiodically. These patches are separated by “barriers” that halt earthquake propagation and slip mostly aseismically. However, the physical processes governing this systematic behavior remain unclear. We analyzed two barriers along the Gofar transform fault that have arrested ~15 M6 earthquakes over the past three decades. Ocean bottom seismometer data indicate that the barriers hosted intense microseismicity before the mainshocks and comprise multistrand faults and transtensional stepovers with 100- to 400-m lateral offset. These characteristics contradict earthquake rupture termination models invoking velocity-strengthening friction or large geometric steps and instead point to damage-enhanced porosity and dilatancy-strengthening mechanisms. By isolating rupture segments, the barriers regulate the quasiperiodic recurrence of OTF earthquakes.

Suggested Citation

Gong, J., Fan, W., McGuire, J.J., Behn, M.D., Warren, J.M., Roland, E., Boettcher, M.S., Collins, J.A., Liu, Y., and German, C.R., 2026, Predictable seismic cycles result from structural rupture barriers on oceanic transform faults: Science, v. 392, p. 718-723, https://doi.org/10.1126/science.ady6190.

Publication type Article
Publication Subtype Journal Article
Title Predictable seismic cycles result from structural rupture barriers on oceanic transform faults
Series title Science
DOI 10.1126/science.ady6190
Volume 392
Publication Date May 14, 2026
Year Published 2026
Language English
Publisher AAAS
Contributing office(s) Earthquake Science Center
Description 6 p.
First page 718
Last page 723
Other Geospatial Gofar transform fault, Pacific Ocean
Additional publication details