A Long‐Term View of Episodic Tremor and Slip in Cascadia

Abstract Episodic Tremor and Slip, or ETS, is a well‐recognized phenomenon in the Cascadia subduction zone. Constraining the precise location of geodetically measured slip during ETS is important for clarifying the relationship between slip and tremor during ETS, the location of ETS slip relative to...

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Main Author: Noel M. Bartlow
Format: Article
Language:English
Published: Wiley 2020-02-01
Series:Geophysical Research Letters
Subjects:
Online Access:https://doi.org/10.1029/2019GL085303
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author Noel M. Bartlow
author_facet Noel M. Bartlow
author_sort Noel M. Bartlow
collection DOAJ
description Abstract Episodic Tremor and Slip, or ETS, is a well‐recognized phenomenon in the Cascadia subduction zone. Constraining the precise location of geodetically measured slip during ETS is important for clarifying the relationship between slip and tremor during ETS, the location of ETS slip relative to the strongly locked zone, and the role of ETS in the overall slip budget. Here I present a new method for separating Global Navigation Satellite System time series in Cascadia into ETS and inter‐ETS components, deriving long‐term average ETS velocities for each site. These velocities are then inverted for a time‐averaged ETS slip rate on the plate interface. I find that ETS and its role in the slip budget are highly variable and segmented along strike. This inversion represents the highest‐resolution image of the ETS zone derived from geodetic data to date. Slip correlates well with tremor locations, and a possible second updip ETS zone is detected.
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spelling doaj-art-70a43eb5c5a7482ab2e93e77db04f57f2025-08-20T03:49:32ZengWileyGeophysical Research Letters0094-82761944-80072020-02-01473n/an/a10.1029/2019GL085303A Long‐Term View of Episodic Tremor and Slip in CascadiaNoel M. Bartlow0Berkeley Seismological Laboratory University of California Berkeley CA USAAbstract Episodic Tremor and Slip, or ETS, is a well‐recognized phenomenon in the Cascadia subduction zone. Constraining the precise location of geodetically measured slip during ETS is important for clarifying the relationship between slip and tremor during ETS, the location of ETS slip relative to the strongly locked zone, and the role of ETS in the overall slip budget. Here I present a new method for separating Global Navigation Satellite System time series in Cascadia into ETS and inter‐ETS components, deriving long‐term average ETS velocities for each site. These velocities are then inverted for a time‐averaged ETS slip rate on the plate interface. I find that ETS and its role in the slip budget are highly variable and segmented along strike. This inversion represents the highest‐resolution image of the ETS zone derived from geodetic data to date. Slip correlates well with tremor locations, and a possible second updip ETS zone is detected.https://doi.org/10.1029/2019GL085303Episodic Tremor and SlipCascadiaslow sliptremorslip budget
spellingShingle Noel M. Bartlow
A Long‐Term View of Episodic Tremor and Slip in Cascadia
Geophysical Research Letters
Episodic Tremor and Slip
Cascadia
slow slip
tremor
slip budget
title A Long‐Term View of Episodic Tremor and Slip in Cascadia
title_full A Long‐Term View of Episodic Tremor and Slip in Cascadia
title_fullStr A Long‐Term View of Episodic Tremor and Slip in Cascadia
title_full_unstemmed A Long‐Term View of Episodic Tremor and Slip in Cascadia
title_short A Long‐Term View of Episodic Tremor and Slip in Cascadia
title_sort long term view of episodic tremor and slip in cascadia
topic Episodic Tremor and Slip
Cascadia
slow slip
tremor
slip budget
url https://doi.org/10.1029/2019GL085303
work_keys_str_mv AT noelmbartlow alongtermviewofepisodictremorandslipincascadia
AT noelmbartlow longtermviewofepisodictremorandslipincascadia