The ubiquitous creeping segments on oceanic transform faults

Oceanic transform faults are a significant component of the global plate boundary system and are well known for generating fewer and smaller earthquakes than expected. Detailed studies at a handful of sites support the hypothesis that an abundance of creeping segments is responsible for most of the observed deficiency of earthquakes on those faults. We test this hypothesis on a global scale. We relocate M-w >= 5 earthquakes on 138 oceanic transform faults around the world and identify creeping segments on these faults. We demonstrate that creeping segments occur on almost all oceanic transform faults, which could explain their deficiency of earthquakes. We also find that most of the creeping segments are not associated with any large-scale geological structure such as a fault step-over, indicating that along-strike variation of fault zone properties may be the main reason for their existence.

Automated summary

Oceanic transform faults are important components of the global plate boundary system, known for generating fewer and smaller earthquakes. Research suggests that the presence of creeping segments could explain the deficiency of earthquakes on these faults, and the variation of fault zone properties may be the main reason for their existence.