Relationship Between the High-Amplitude Magnetic Anomalies and Serpentinized Fore-Arc Mantle in the Cascadia Subduction Zone
Author:
Funder
Ministry of Science and Technology of Taiwan
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology,Geophysics
Link
https://link.springer.com/content/pdf/10.1007/s00024-023-03337-4.pdf
Reference56 articles.
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2. Amante, C., & Eakins, B.W. (2009). ETOPO1 1 arc-minute global relief model: procedures, data sources and analysis. NOAA technical memorandum NESDIS NGDC-24. National Geophysical Data Center, NOAA. https://doi.org/10.7289/V5C8276M.
3. Audet, P., Bostock, M. G., Christensen, N. I., & Peacock, S. M. (2009). Seismic evidence for overpressured subducted oceanic crust and megathrust fault sealing. Nature, 457, 76–78. https://doi.org/10.1138/nature07650
4. Bilek, S. L. (2009). Seismicity along the South American subduction zone: Review of large earthquakes, tsunamis, and subduction zone complexity. Tectonophysics, 495, 2–14. https://doi.org/10.1016/j.texto.2009.02.037
5. Blakely, R. J., Brocher, T. M., & Wells, R. E. (2005). Subduction-zone magnetic anomalies and implications for hydrated forearc mantle. Geology, 33, 445–448. https://doi.org/10.1130/G21447.1
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