Structural Controls on Megathrust Slip Behavior Inferred From a 3D, Crustal‐Scale, P‐Wave Velocity Model of the Alaska Peninsula Subduction Zone
- 14 November 2024
- journal article
- research article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research: Solid Earth
- Vol. 129 (11)
Abstract
In subduction zones, along‐strike and downdip variations in megathrust slip behavior are linked to changes in properties of the subducting and overriding plates. Although marine geophysical methods provide insights into subduction zone structures, most surveys consist of sparse 2D profiles, limiting our understanding of first‐order controls. Here, we use active‐source seismic data to derive a 3D crustal‐scale P‐wave velocity model of the Alaska Peninsula subduction zone that encompasses both plates and spans the Semidi segment and SW Kodiak asperity. Our results reveal modest variations within the incoming plate, attributed to a series of fracture zones, seamounts and their associated basement swell, collectively contributing to plate hydration. Basement swell appears to modulate the distribution and type of sediment entering the trench, likely impacting observed variations in slip behavior. The overriding plate exhibits significant heterogeneity. The updip limit and width of the dynamic backstop are similar between the SW Kodiak asperity and eastern Semidi segment, but differ significantly from the Western Semidi segment. These distinctions likely account for differences in earthquake rupture patterns and interseismic coupling among these segments. Additionally, high‐velocities in the mid‐lower forearc crust coincide with the location of megathrust slip during the Mw 8.2 2021 Chignik event. We interpret these velocities as intracrustal intrusions that contributed to the deep rupture of the 2021 event. Our findings suggest that the contrasting structural and material properties of both the incoming and overriding plates influence the spatially complex and semi‐persistent segmentation of the megathrust offshore the Alaska Peninsula.Keywords
Funding Information
- National Science Foundation (OCE‐1947758, OCE‐1948087)
This publication has 106 references indexed in Scilit:
- Spatial Variation of Slip Behavior Beneath the Alaska Peninsula Along Alaska‐Aleutian Subduction ZoneGeophysical Research Letters, 2018
- A possible transoceanic tsunami directed toward the U.S. west coast from the Semidi segment, Alaska convergent marginGeochemistry, Geophysics, Geosystems, 2015
- Identification of the static backstop and its influence on the evolution of the accretionary prism in the Nankai TroughEarth and Planetary Science Letters, 2015
- Origin of dipping structures in fast-spreading oceanic lower crust offshore Alaska imaged by multichannel seismic dataEarth and Planetary Science Letters, 2015
- Gravity anomalies, crustal structure, and seismicity at subduction zones: 2. Interrelationships between fore‐arc structure and seismogenic behaviorGeochemistry, Geophysics, Geosystems, 2015
- Gravity anomalies, crustal structure, and seismicity at subduction zones: 1. Seafloor roughness and subducting reliefGeochemistry, Geophysics, Geosystems, 2015
- Fluid accumulation along the Costa Rica subduction thrust and development of the seismogenic zoneJournal of Geophysical Research: Solid Earth, 2014
- Uplift and subsidence reveal a nonpersistent megathrust rupture boundary (Sitkinak Island, Alaska)Geophysical Research Letters, 2014
- The role of farfield tectonic stress in oceanic intraplate deformation, Gulf of AlaskaJournal of Geophysical Research: Solid Earth, 2013
- Do Trench Sediments Affect Great Earthquake Occurrence in Subduction Zones?1989