Tectonic Tremor Explained by Successive Ruptures of Clustered Quartz‐Filled Shear Veins

Abstract A tectonic tremor is a successive seismic signal observed along plate boundaries in subduction zones. However, the source processes and mechanisms responsible for the tremor remain unclear. Quartz‐filled shear and extension veins are clustered in tens to hundreds of meters thick subduction...

Full description

Saved in:
Bibliographic Details
Main Authors: S. Yabe, K. Ujiie
Format: Article
Language:English
Published: Wiley 2025-07-01
Series:Geophysical Research Letters
Subjects:
Online Access:https://doi.org/10.1029/2025GL115447
Tags: Add Tag
No Tags, Be the first to tag this record!