Aseismic transient slip on the Gofar transform fault, East Pacific Rise

Proceedings of the National Academy of Sciences
By: , and 

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Abstract

Oceanic transform faults display a unique combination of seismic and aseismic slip behavior, including a large globally averaged seismic deficit, and the local occurrence of repeating magnitude (M) 6∼6 earthquakes with abundant foreshocks and seismic swarms, as on the Gofar transform of the East Pacific Rise and the Blanco Ridge in the northeast Pacific Ocean. However, the underlying mechanisms that govern the partitioning between seismic and aseismic slip and their interaction remain unclear. Here we present a numerical modeling study of earthquake sequences and aseismic transient slip on oceanic transform faults. In the model, strong dilatancy strengthening, supported by seismic imaging that indicates enhanced fluid-filled porosity and possible hydrothermal circulation down to the brittle–ductile transition, effectively stabilizes along-strike seismic rupture propagation and results in rupture barriers where aseismic transients arise episodically. The modeled slow slip migrates along the barrier zones at speeds ∼10 to 600 m/h, spatiotemporally correlated with the observed migration of seismic swarms on the Gofar transform. Our model thus suggests the possible prevalence of episodic aseismic transients in M 6∼6 rupture barrier zones that host active swarms on oceanic transform faults and provides candidates for future seafloor geodesy experiments to verify the relation between aseismic fault slip, earthquake swarms, and fault zone hydromechanical properties.

Publication type Article
Publication Subtype Journal Article
Title Aseismic transient slip on the Gofar transform fault, East Pacific Rise
Series title Proceedings of the National Academy of Sciences
DOI 10.1073/pnas.1913625117
Volume 117
Issue 19
Year Published 2020
Language English
Publisher National Academy of Sciences
Contributing office(s) Earthquake Science Center
Description 7 p.
First page 10188
Last page 10194
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