Role of Weak Materials in Earthquake Rupture Dynamics Article Swipe
Tetsuro Hirono
,
Kenichi Tsuda
,
Shunya Kaneki
·
YOU?
·
· 2019
· Open Access
·
· DOI: https://doi.org/10.1038/s41598-019-43118-5
YOU?
·
· 2019
· Open Access
·
· DOI: https://doi.org/10.1038/s41598-019-43118-5
Weak materials in seismic slip zones are important in studies of earthquake mechanics. For instance, the exceptionally large slip during the 2011 Tohoku-Oki earthquake has been attributed to the presence of smectite in the fault zone. However, weak fault rocks cannot accumulate large amounts of elastic strain, which is thought to counter their ability to enhance seismic rupture. It is well known that if the permeability of a weak fault is low enough to allow friction-induced thermal pressurization of interstitial fluid, the fault strength decreases dramatically. However, whether intrinsic weakness of fault material or thermal pressurization more efficiently produces large slip on faults bearing weak materials has not been determined. To investigate the role of weak materials in earthquake rupture dynamics, we conducted friction experiments and dynamic rupture simulations using pure smectite and pure graphite to represent weak fault materials. Even when we assumed no thermal pressurization, simulated faults in both media were able to trigger large slip because their extremely low friction was insufficient to arrest the inertial motion of rupture propagating along the fault. We used similar rupture simulations to investigate the cause of the huge slip near the trench during the 2011 Tohoku-Oki earthquake and demonstrated that it can be attributed to thermal pressurization, although our findings suggest that the presence of smectite in the plate-boundary fault may also be required.
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Metadata
- Type
- article
- Language
- en
- Landing Page
- https://doi.org/10.1038/s41598-019-43118-5
- https://www.nature.com/articles/s41598-019-43118-5.pdf
- OA Status
- gold
- Cited By
- 27
- References
- 34
- Related Works
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- OpenAlex ID
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All OpenAlex metadata
Raw OpenAlex JSON
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https://openalex.org/W2941250343Canonical identifier for this work in OpenAlex
- DOI
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https://doi.org/10.1038/s41598-019-43118-5Digital Object Identifier
- Title
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Role of Weak Materials in Earthquake Rupture DynamicsWork title
- Type
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articleOpenAlex work type
- Language
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enPrimary language
- Publication year
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2019Year of publication
- Publication date
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2019-04-29Full publication date if available
- Authors
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Tetsuro Hirono, Kenichi Tsuda, Shunya KanekiList of authors in order
- Landing page
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https://doi.org/10.1038/s41598-019-43118-5Publisher landing page
- PDF URL
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https://www.nature.com/articles/s41598-019-43118-5.pdfDirect link to full text PDF
- Open access
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YesWhether a free full text is available
- OA status
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goldOpen access status per OpenAlex
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https://www.nature.com/articles/s41598-019-43118-5.pdfDirect OA link when available
- Concepts
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Cabin pressurization, Slip (aerodynamics), Geology, Earthquake rupture, Trench, Thermal, Elastic-rebound theory, Fault (geology), Seismology, Geotechnical engineering, Seismic gap, Materials science, Composite material, Thermodynamics, Physics, Meteorology, Layer (electronics)Top concepts (fields/topics) attached by OpenAlex
- Cited by
-
27Total citation count in OpenAlex
- Citations by year (recent)
-
2025: 3, 2024: 9, 2023: 2, 2022: 9, 2021: 2Per-year citation counts (last 5 years)
- References (count)
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34Number of works referenced by this work
- Related works (count)
-
10Other works algorithmically related by OpenAlex
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