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Mechanism of underthrusting in southwest Japan: A model of convergent plate interactions

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Fitch, Thomas J., Scholz, Christopher H.·1971·Journal of Geophysical Research

Abstract

An elastic rebound mechanism consistent with underthrusting at the time of the magnitude 8.2 Nankaido earthquake of 21 December, 1946 accounts for a reversal in sense between seismic and preseismic changes in elevation throughout a large portion of southwest Japan. It is shown that the seismic movements during the earthquake were generated by slip on a complex thrust fault that is inferred to intersect the surface near the base of the continental slope. The preseismic deformation is explained by strain accumulation equivalent to a virtual dislocation with the same orientation as the fault surface but a sense opposite to that of the real dislocation that occurred at the time of the earthquake. Adjustments by slip along the fault surface and extensions of that surface can account for postseismic movements.

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Metadata

Authors
Fitch, T. J., & Scholz, C. H.
Venue
Journal of Geophysical Research
Published
1971-10-10
Volume
76
Issue
29
Pages
7260-7292
ISSN
0148-0227 (ISSN-L)
OpenAlex
W2013823208
Cited by
310
References
0
FWCI
13.16
Type
journal article
Language
en
Open access
green

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CoChat. (2026). Citation check: Mechanism of underthrusting in southwest Japan: A model of convergent plate interactions. https://app.cochat.ai/papers/10.1029/jb076i029p07260
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Fitch, T. J., & Scholz, C. H. (1971). Mechanism of underthrusting in southwest Japan: A model of convergent plate interactions. Journal of Geophysical Research. https://doi.org/10.1029/jb076i029p07260

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Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).

Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.