Search engine for discovering works of Art, research articles, and books related to Art and Culture
ShareThis
Javascript must be enabled to continue!

Enhanced deep learning approach for detecting and locating tectonic tremors in the Nankai subduction zone

View through CrossRef
Abstract Tectonic tremors are key indicators of slow-slip phenomena, and detecting them accurately is a challenging task. Conventional techniques often fail to detect tremors during periods of intense tremor activity. We present here a deep learning approach for detecting and locating tremors in the Nankai subduction zone that is more effective than conventional techniques. We utilized two convolutional neural networks (CNNs): a CNN for classification of seismic waveforms into noise, tremors, or earthquakes, and a CNN for regression prediction of tremor epicenters from amplitude data. The accuracy, recall, and precision of the CNN for classification all exceeded 95%. The CNN for regression used ensemble predictions to produce estimates of tremor locations with a median error of 3.2 km. When this approach was applied to continuous data, it successfully mapped key features of tremor activity and improved the detection and location of tremors, especially during high-activity periods. Graphical Abstract
Title: Enhanced deep learning approach for detecting and locating tectonic tremors in the Nankai subduction zone
Description:
Abstract Tectonic tremors are key indicators of slow-slip phenomena, and detecting them accurately is a challenging task.
Conventional techniques often fail to detect tremors during periods of intense tremor activity.
We present here a deep learning approach for detecting and locating tremors in the Nankai subduction zone that is more effective than conventional techniques.
We utilized two convolutional neural networks (CNNs): a CNN for classification of seismic waveforms into noise, tremors, or earthquakes, and a CNN for regression prediction of tremor epicenters from amplitude data.
The accuracy, recall, and precision of the CNN for classification all exceeded 95%.
The CNN for regression used ensemble predictions to produce estimates of tremor locations with a median error of 3.
2 km.
When this approach was applied to continuous data, it successfully mapped key features of tremor activity and improved the detection and location of tremors, especially during high-activity periods.
Graphical Abstract.

Related Results

Geodynamic modelling of continental subduction beneath oceanic lithosphere
Geodynamic modelling of continental subduction beneath oceanic lithosphere
Subduction of an oceanic plate beneath either an oceanic, or a continental, overriding plate requires two main conditions to occur in a steady state: i) a high enough subduction ra...
Enhanced deep learning approach for detecting and locating tectonic tremors in the Nankai subduction zone
Enhanced deep learning approach for detecting and locating tectonic tremors in the Nankai subduction zone
Abstract Tectonic tremors are key indicators of slow-slip phenomena, and detecting them accurately is a challenging task. Conventional techniques often fail to detect tremo...
Sismotectonique du prisme de la Barbade : implications sur le potentiel sismogénique de la zone de subduction des Antilles
Sismotectonique du prisme de la Barbade : implications sur le potentiel sismogénique de la zone de subduction des Antilles
La zone de subduction des Petites Antilles résulte de la subduction des plaques nord- et sud-américaines sous la plaque Caraïbe dans une direction SW à ~ 2 cm/an. Cette zone pourra...
Diversity of transient slow slip along the Mexican subduction zone
Diversity of transient slow slip along the Mexican subduction zone
Diversité des glissements lents transitoires au niveau de la zone de subduction mexicaine Les glissements asismiques, sont des événements lents et transitoires qui ...
Dynamics of multiple microcontinent accretion during oceanic subduction
Dynamics of multiple microcontinent accretion during oceanic subduction
Microcontinent accretion during oceanic subduction is one of the main contributors to continental crustal growth. Many of the continental mountain belts we find today were built fr...
Interaction between aseismic slip phenomena in a collision orogen
Interaction between aseismic slip phenomena in a collision orogen
Using continuous seismological data of Central Weather Administration (CWA) Seismographic Network and Broadband Array in Taiwan for Seismology (BATS), we applied the envelope corre...
Towards a Reconstruction of the Magmatic and Tectonic Evolution of the Demise of the Antarctic Peninsula Subduction Zone
Towards a Reconstruction of the Magmatic and Tectonic Evolution of the Demise of the Antarctic Peninsula Subduction Zone
The Antarctic Peninsula preserves the life cycle of a subduction zone from initiation to demise. The Antarctic-Phoenix subduction zone was active from the Late Jurassic till the in...

Back to Top