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Slow Earthquakes and Nonvolcanic Tremor
Abstract
Nonvolcanic tremor is observed in close association with geodetically observed slow-slip events in subduction zones. Accumulating evidence points to these events as members of a family of slow earthquakes that occur as shear slip on the downdip extensions of fault zones in a regime that is transitional between a frictionally locked region above and a freely slipping region below. By virtue of their locations and their properties, slow earthquakes are certain to provide new insights into the behavior of earthquakes and faulting and into the hazard they embody.
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Cited by
Slab1.0: A three‐dimensional model of global subduction zone geometries
Hayes, G. P., Wald, D. J., & Johnson, R. L. (2012) · Journal of Geophysical Research: Solid Earth · doi:10.1029/2011jb008524 · Cited by 1,081
The Mechanics of Earthquakes and Faulting
Scholz, C. H. (2019) · Cambridge University Press eBooks · doi:10.1017/9781316681473 · Cited by 910
Depth‐varying rupture properties of subduction zone megathrust faults
Lay, T., Kanamori, H., Ammon, C. J., Koper, K. D., Hutko, A. R., Ye, L., Yue, H., & Rushing, T. M. (2012) · Journal of Geophysical Research: Solid Earth · doi:10.1029/2011jb009133 · Cited by 640
Seismic Arrival-time Picking on Distributed Acoustic Sensing Data using Semi-supervised Learning
Zhu, W., Biondi, E., Li, J., Yin, J., Ross, Z. E., & Zhan, Z. (2023) · Nature Communications · doi:10.1038/s41467-023-43355-3 · Cited by 130
Metadata
- Authors
- Beroza, G. C., & Ide, S.
- Venue
- Annual Review of Earth and Planetary Sciences
- Publisher
- Annual Reviews
- Published
- 2011-05-30
- Volume
- 39
- Issue
- 1
- Pages
- 271-296
- ISSN
- 0084-6597 (ISSN-L)
- 1545-4495
- OpenAlex
- W2136668526
- Cited by
- 487
- References
- 0
- FWCI
- 4.29
- Type
- journal article
- Language
- en
- Open access
- closed
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