Abstract
In the Northern California region, the transform fault and related transcurrent faults are running between oceanic ridges, and this tectonic situation is different with that of the subduction boundary in the Japanese region. The characteristic features of the seismicity in the Northern California region are possibly investigated by the correlated seismicity likely to the Japanese seismicity.
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References
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Toriumi, M. (2021). Correlated Seismicity of the Northern California Region. In: Global Seismicity Dynamics and Data-Driven Science. Advances in Geological Science. Springer, Singapore. https://doi.org/10.1007/978-981-15-5109-3_7
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DOI: https://doi.org/10.1007/978-981-15-5109-3_7
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