The Parkfield tremors reveal slow and fast ruptures on the same asperity.
about
Connecting slow earthquakes to huge earthquakes.Precursory changes in seismic velocity for the spectrum of earthquake failure modesAreas prone to slow slip events impede earthquake rupture propagation and promote afterslip.Slow-slip events in semi-brittle serpentinite fault zones.A 15 year catalog of more than 1 million low-frequency earthquakes: Tracking tremor and slip along the deep San Andreas FaultReconsidering earthquake scalingPiecemeal Rupture of the Mentawai Patch, Sumatra: The 2008 M w 7.2 North Pagai Earthquake Sequence
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The Parkfield tremors reveal slow and fast ruptures on the same asperity.
description
2016 nî lūn-bûn
@nan
2016年の論文
@ja
2016年学术文章
@wuu
2016年学术文章
@zh
2016年学术文章
@zh-cn
2016年学术文章
@zh-hans
2016年学术文章
@zh-my
2016年学术文章
@zh-sg
2016年學術文章
@yue
2016年學術文章
@zh-hant
name
The Parkfield tremors reveal slow and fast ruptures on the same asperity.
@en
The Parkfield tremors reveal slow and fast ruptures on the same asperity.
@nl
type
label
The Parkfield tremors reveal slow and fast ruptures on the same asperity.
@en
The Parkfield tremors reveal slow and fast ruptures on the same asperity.
@nl
prefLabel
The Parkfield tremors reveal slow and fast ruptures on the same asperity.
@en
The Parkfield tremors reveal slow and fast ruptures on the same asperity.
@nl
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P356
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P1476
The Parkfield tremors reveal slow and fast ruptures on the same asperity.
@en
P2860
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P304
P356
10.1038/NATURE17190
P407
P577
2016-04-04T00:00:00Z
P6179
1025312015