Tectonic tremor as friction-induced inertial vibration

2021 ◽  
Vol 576 ◽  
pp. 117238
Author(s):  
Kyungjae Im ◽  
Jean-Philippe Avouac
Keyword(s):  
Author(s):  
Kevin Chao ◽  
Zhigang Peng ◽  
William B. Frank ◽  
Germán A. Prieto ◽  
Kazushige Obara

ABSTRACT We report new observations of triggered tectonic tremor in three regions in South America along the plate boundary between the Nazca and South America plates: southern Chile, Ecuador, and central Colombia. In these regions, tremor was observed during the passage of large‐amplitude surface waves of recent large earthquakes, which occurred in South America and around the world. In southern Chile, triggered tremor was observed around an ambient tremor active zone in the Chile triple junction region. In Ecuador and central Colombia, only one seismic station in each region recorded triggered tremor. With a single‐station approach, we are able to estimate potential tremor sources in these regions. Triggered tremor in Ecuador is likely associated with an inland fault near the volcanic region. In central Colombia, triggered tremor may be associated with the Romeral fault system rather than the subduction zone interface. In addition, we summarize global observations of tremor‐triggering stress and background ambient tremor activity in 24 tremor‐active regions. Based on the global summary of triggered and ambient tremor activity, the relative lack of triggered tremor in central and northern Chile and Peru is consistent with the lack of background tremor activity in these regions, suggesting tectonic tremor occurs only in isolated regions along major faults.


2019 ◽  
Vol 94 ◽  
pp. 102178
Author(s):  
Yohei Nishitsuji ◽  
Luis Franco Marín ◽  
Martín Gomez ◽  
C.A. Rowe ◽  
Deyan Draganov

2015 ◽  
Vol 105 (3) ◽  
pp. 1779-1786 ◽  
Author(s):  
Anna Pfohl ◽  
Linda M. Warren ◽  
Stefany Sit ◽  
Michael Brudzinski

2016 ◽  
Vol 454 ◽  
pp. 259-271 ◽  
Author(s):  
Michael R. Brudzinski ◽  
Kristen M. Schlanser ◽  
Nicholas J. Kelly ◽  
Charles DeMets ◽  
Stephen P. Grand ◽  
...  

2020 ◽  
Author(s):  
Natalia Poiata ◽  
Jean-Pierre Vilotte ◽  
Nikolai Shapiro ◽  
Mariano Supino ◽  
Kazushige Obara

<p>Short-duration transient seismic events known as low-frequency earthquakes (LFEs) are a component of the slow earthquakes family observed in the transition zone, at the root of seismogenic regions of the subduction zones or active faults. LFEs are the signature of impulse seismic energy radiation associated to and often mixed within complex tectonic tremor signal. Detailed analysis and characterization of LFE space-time activity in relation to other slow earthquake phenomena can provide important information about the state and the processes of fault interface.</p><p>We derive a catalog of LFEs in western Shikoku (Japan) by applying a full waveform coherency-based detection and location method to the 4-year continuous data covering the period of 2013-2016 and recorded at Hi-net seismic stations of NIED. The obtained catalog of over 150,000 detected events allows looking into the details of LFE space-time activity during the tectonic tremor sequences and inter-sequence periods.</p><p>We use this catalogue of LFEs to perform a systematic statistical analysis of the event occurrence patterns by applying correlation and clustering analysis to infer the large-scale (long temporal ~ 1-2 day duration) space-time characteristics and interaction patterns of activity and its potential relation to the structural complexity of the subducting plate. We also analyze the correlation between the migration of clustered LFE activity during energetic tremor sequences and short-term slow slip events occurring in the area during the analyzed period.</p>


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