Spatiotemporal Characteristics of Tectonic Tremors in the Collisional Orogen of Taiwan
Taiwan offers a distinctive tectonic setting as a collisional orogen, ideal for studying tectonic tremors and the slow deformation process in the mountain‐building process.
Kate Huihsuan Chen, Satoshi Ide
exaly +3 more sources
The big impact of small quakes on tectonic tremor synchronization. [PDF]
Tectonic tremor tracks the repeated slow rupture of certain major plate boundary faults. One of the most perplexing aspects about tremor is that some fault segments produce strongly periodic, spatially extensive tremor episodes, while others have more disorganized, asynchronous activity. Here, we measure the size of segments that activate synchronously
Farge G, Brodsky EE.
europepmc +5 more sources
Laboratory Hydrofractures as Analog to Tectonic Tremor
This package includes the laboratory datasets and scripts for reproducing most of figures in the manuscript namely "Laboratory Hydrofractures as Analog to Tectonic Tremor".
Yuan, Congcong +3 more
core +5 more sources
Seismological Structures on Bimodal Distribution of Deep Tectonic Tremor [PDF]
AbstractDeep tectonic tremors occur at the downdip extent of the seismogenic zone due to fluid processes. Beneath the northeastern Kii Peninsula, southwestern Japan, there is an along‐dip bimodal distribution of tremor. However, no constraint exists on the structures controlling that distribution. We extract detailed seismological structures from multi‐
Yasunori Sawaki +4 more
openaire +3 more sources
Single station seismic observations enable high resolution localization of tectonic tremor sources using a vision transformer [PDF]
Precisely locating tectonic tremor events is essential for understanding subduction zone dynamics. However, the lack of impulsive phase arrivals typically necessitates multi-station observations, posing a fundamental challenge for high-resolution ...
Amane Sugii, Yoshihiro Hiramatsu
doaj +2 more sources
Depth and Thickness of Tectonic Tremor in the Northeastern Olympic Peninsula
AbstractTectonic tremor has been explained as a swarm of low‐frequency earthquakes (LFEs), which are located on a narrow fault at the plate boundary. However, due to the lack of clear impulsive phases in the tremor signal, it is difficult to determine the depth of the tremor source with great precision.
A. Ducellier, K. C. Creager
openaire +3 more sources
Spatiotemporal Characteristics of Tectonic Tremors in California
California, as a transform plate boundary, provides a distinctive tectonic setting and an ideal natural laboratory for investigating tectonic tremors and the slow deformation associated with plate motion.
Weifan Lu, Satoshi Ide
doaj +2 more sources
Tectonic Tremor Reveals Slow Deformation Along the Antarctic–South American Subduction Zone
The Antarctic–South American subduction zone is among the least explored convergent margins and lacks documented large interplate earthquakes despite ongoing convergence.
K. Azúa, S. Ruiz, S. Ide
doaj +2 more sources
Forecasting tectonic tremor activity using a renewal process model
In many tectonically active regions of the world, a variety of slow deformation phenomena have been discovered and collectively termed slow earthquakes.
Satoshi Ide, Shunichi Nomura
doaj +2 more sources
Tectonic tremor: The chatter of mafic underplating
Tremor is a weak seismic signal accompanying slow fault slip at plate boundaries. The relationship between tremor and slow slip and the tremor source mechanism have been widely debated, owing largely to the challenge of accurately locating tremor in ...
Geena Littel +4 more
doaj +2 more sources

