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Recurrent slow slip event reveals the interaction with seismic slow earthquakes and disruption from large earthquake [PDF]
Zhen Liu, Angelyn W. Moore, Susan Owen
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Reconnaissance observations by CIGIDEN after the 2015 Illapel, Chile earthquake and tsunami
This paper describes the reconnaissance work conducted by researchers from the National Research Center for Integrated Natural Disaster Management (CIGIDEN) between September 23rd and October 2nd in the area affected by the Mw 8.3 Illapel megathrust ...
Rivera Jofré, Felipe Andrés +12 more
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Errata to “Characteristic activities of slow earthquakes in Japan”
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On the Observations of Slow Earthquake Motions
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Recent Report on "Slow Earthquake Database"
identifier:oai:t2r2.star.titech.ac.jp ...
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Probing Slow Earthquakes With Deep Learning [PDF]
AbstractSlow earthquakes may trigger failure on neighboring locked faults that are stressed sufficiently to break, and slow slip patterns may evolve before a nearby great earthquake. However, even in the clearest cases such as Cascadia, slow earthquakes and associated tremor have only been observed in intermittent and discrete bursts.
Ian W McBrearty +2 more
exaly +5 more sources
Earthquake and tsunami forecasts: Relation of slow slip events to subsequent earthquake rupture [PDF]
The 5 September 2012 Mw 7.6 earthquake on the Costa Rica subduction plate boundary followed a 62-y interseismic period. High-precision GPS recorded numerous slow slip events (SSEs) in the decade leading up to the earthquake, both up-dip and down-dip of ...
Marino Protti +2 more
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Connecting slow earthquakes to huge earthquakes
Science, 2016Slow earthquakes are characterized by a wide spectrum of fault slip behaviors and seismic radiation patterns that differ from those of traditional earthquakes. However, slow earthquakes and huge megathrust earthquakes can have common slip mechanisms and are located in neighboring regions of the seismogenic zone.
Aitaro Kato, Kazushige Obara
exaly +3 more sources
Physics of the Earth and Planetary Interiors, 1979
Anomalous earthquakes such as creep events, tsunami earthquakes and silent earthquakes have been reported in the recent literature. In this paper we discuss an anomalous “slow earthquake” that occurred on June 6, 1960 in southern Chile. Although the surface-wave magnitude of this event is only 6.9, it excited anomalously large long-period multiple ...
Kanamori, Hiroo, Stewart, Gordon S.
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Anomalous earthquakes such as creep events, tsunami earthquakes and silent earthquakes have been reported in the recent literature. In this paper we discuss an anomalous “slow earthquake” that occurred on June 6, 1960 in southern Chile. Although the surface-wave magnitude of this event is only 6.9, it excited anomalously large long-period multiple ...
Kanamori, Hiroo, Stewart, Gordon S.
openaire +2 more sources

