Overpressured Underthrust Sediment in the Nankai Trough Forearc Inferred From Transdimensional Inversion of High‐Frequency Teleseismic Waveforms
Author:
Affiliation:
1. Earthquake Research Institute The University of Tokyo Tokyo Japan
2. Department of Earth Resources Engineering Kyushu University Fukuoka Japan
3. Research Institute for Marine Geodynamics JAMSTEC Yokohama Japan
Publisher
American Geophysical Union (AGU)
Subject
General Earth and Planetary Sciences,Geophysics
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1029/2020GL088280
Reference48 articles.
1. Receiver function inversion by trans-dimensional Monte Carlo sampling
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3. Non-linear waveform analysis for water-layer response and its application to high-frequency receiver function analysis using OBS array
4. A fluid-rich layer along the Nankai trough megathrust fault off the Kii Peninsula inferred from receiver function inversion
5. Source mechanisms and tectonic significance of historical earthquakes along the nankai trough, Japan
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