WITHDRAWN Fast and Slow Earthquakes in Alaska: Insights From Three-Dimensional Thermal Structure and Slab Dehydration
Description:
WITHDRAWN Fast and slow earthquakes are predominantly generated along faults constituting active plate boundaries. Characterized by repeated devastating earthquakes and frequent slow slip events and tremors, the Alaska megathrust presents a chance to better know the complicated dynamics of a subduction system changing from steep to shallow dips associated with enigmatically abundant fast and slow seismic events. Based on three-dimensional thermal modeling, we find that the downgoing metamorphosed oceanic crust containing bound water releases a large amount of fluid and causes the recurrence of fast and slow earthquakes by elevated pore fluid pressure and hydrofracturing. The seismogenic interface and the slow slip events (SSEs) identified beneath the Upper Cook Inlet coincide well with the slab metamorphic dehydration regions. The observed slow earthquakes with quasi-stable fault slips preferentially occur, accompanied by high dehydration and temperature downdip along the transition zone.
Session: From Geodynamics to Earthquake Rupture, Models That Cross Time- and Length-Scales [Poster Session]
Type: Poster
Date: 5/3/2024
Presentation Time: 08:00 AM (local time)
Presenting Author: Yingfeng
Student Presenter: No
Invited Presentation:
Authors
Yingfeng Ji
Presenting Author
Corresponding Author
31911431@qq.com
Chinese Academy of Sciences
Rui Qu
qurui@itpcas.ac.cn
Chinese Academy of Sciences
Weiling Zhu
zhuweiling@itpcas.ac.cn
Chinese Academy of Sciences
WITHDRAWN Fast and Slow Earthquakes in Alaska: Insights From Three-Dimensional Thermal Structure and Slab Dehydration
Category
From Geodynamics to Earthquake Rupture, Models That Cross Time- and Length-Scales