Earth’s free surface complicates inference of absolute stress from earthquake-Induced stress rotations
Geophysical Research Letters
Links
- More information: Publisher Index Page (via DOI)
- Open Access Version: Publisher Index Page
- Download citation as: RIS | Dublin Core
Abstract
The stress redistribution from an earthquake can produce localized measurable rotations of the principal stress axes if the absolute level of differential stress in the crust in on the order of the earthquake stress drop. Two simple analytic solutions have been developed to estimate the differential stress from an observed stress rotation. However, each has assumptions that may not be accurate near Earth’s free surface. I model synthetic earthquakes in an elastic half-space, and show that the assumptions of the methods are accurate for strike-slip earthquakes, and for deep dip-slip earthquakes. However, they are incorrect for shallow dip-slip earthquakes. I introduce a free surface correction for one of the methods for dip-slip earthquakes. I revise an analysis of stress rotations due to great subduction zone earthquakes, including this correction. The results support the original conclusion of near complete stress drop for many shallow subduction zone earthquakes.
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | Earth’s free surface complicates inference of absolute stress from earthquake-Induced stress rotations |
| Series title | Geophysical Research Letters |
| DOI | 10.1029/2023GL106574 |
| Volume | 51 |
| Issue | 4 |
| Year Published | 2024 |
| Language | English |
| Publisher | AGU |
| Contributing office(s) | Earthquake Science Center |
| Description | e2023GL106574, 8 p. |
| Google Analytic Metrics | Metrics page |