Tectonic tremor is the seismic manifestation of slow slip on the deep extensions of some major geological faults. It is composed of many repeating low-frequency earthquakes (LFEs). LFE analysis should provide valuable insights into plate motion and slow slip processes. However, LFEs have seismic amplitudes little above background noise levels, making them difficult to detect. Therefore, in most locations, they are detected only by targeted analysis using prior waveform templates. Using a 15-year catalog of more than 1 million LFEs along the San Andreas Fault, we implement and train a convolutional neural network (CNN) for LFE detection. We demonstrate that we detect new LFEs with low signal amplitude, even below the noise level, without a p...
Experiment to detect and locate low-frequency earthquakes (LFEs) in the Mexican subduction zone. We ...
We use stations in the Willamette valley and Oregon coast ranges to identify low-frequency earthquak...
International audienceMachine learning is becoming increasingly important in scientific and technolo...
International audienceLow-frequency earthquakes (LFEs), which frequently originate from multiplet-ge...
International audienceStudies of low-frequency earthquakes (LFEs) have focused on detecting events w...
International audienceActive faults release tectonic stress imposed by plate motion through a spectr...
Automatic detection of low-magnitude earthquakes has become an increasingly important research topic...
Abstract Low-frequency tremors have been widely detected in many tectonic zones, and are often locat...
[1] Recent studies have shown that deep tremor in the Nankai Trough under western Shikoku consists o...
International audienceSlow slip events (SSEs) originate from a slow slippage on faults that lasts fr...
To optimally monitor earthquake‐generating processes, seismologists have sought to lower detection s...
Experiment to detect and locate low-frequency earthquakes (LFEs) in the Mexican subduction zone. We ...
We use stations in the Willamette valley and Oregon coast ranges to identify low-frequency earthquak...
International audienceMachine learning is becoming increasingly important in scientific and technolo...
International audienceLow-frequency earthquakes (LFEs), which frequently originate from multiplet-ge...
International audienceStudies of low-frequency earthquakes (LFEs) have focused on detecting events w...
International audienceActive faults release tectonic stress imposed by plate motion through a spectr...
Automatic detection of low-magnitude earthquakes has become an increasingly important research topic...
Abstract Low-frequency tremors have been widely detected in many tectonic zones, and are often locat...
[1] Recent studies have shown that deep tremor in the Nankai Trough under western Shikoku consists o...
International audienceSlow slip events (SSEs) originate from a slow slippage on faults that lasts fr...
To optimally monitor earthquake‐generating processes, seismologists have sought to lower detection s...
Experiment to detect and locate low-frequency earthquakes (LFEs) in the Mexican subduction zone. We ...
We use stations in the Willamette valley and Oregon coast ranges to identify low-frequency earthquak...
International audienceMachine learning is becoming increasingly important in scientific and technolo...