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- W2037571269 abstract "To better understand the physical mechanisms of slow slip events (SSEs) detected worldwide, we explore the scaling relationships of various source parameters and compare them with similar scaling laws for earthquakes. These scaling relationships highlight differences and similarities between slow slip events and earthquakes and hold implications for the degree of heterogeneity and fault‐healing characteristics. The static stress drop remains constant for different‐sized events as is observed for earthquakes. However, the static stress drop of slow slip events is within a range of 0.01–1.0 MPa, 1–2 orders of magnitude lower than that found for earthquakes, which could be related to the low stress state on the fault. The average rupture velocity, ranging from kilometers per second to kilometers per day, decreases linearly with increasing seismic moment in log–log space, unlike earthquakes that are nearly constant. This inverse relationship of rupture velocity with seismic moment could be related to the heterogeneity of fault properties. Slow slip events typically have ratios of event duration over dislocation rise time less than 3, while earthquakes have ratios greater than 3. This indicates that slow slip events are less pulselike than earthquakes in their mode of propagation and suggests that the healing behind the rupture front is delayed. The recurrence statistics of slow slip events on the northern Cascadia subduction zone are weakly time predictable and moderately antislip predictable (that is, the event size and preevent recurrence interval are anticorrelated), which may indicate that healing between events strengthens the fault with time.Online Material: Table of source parameters and data sources." @default.
- W2037571269 created "2016-06-24" @default.
- W2037571269 creator A5028132066 @default.
- W2037571269 creator A5061946242 @default.
- W2037571269 creator A5078483143 @default.
- W2037571269 date "2012-02-01" @default.
- W2037571269 modified "2023-10-16" @default.
- W2037571269 title "Scaling Relationships of Source Parameters for Slow Slip Events" @default.
- W2037571269 cites W1544657794 @default.
- W2037571269 cites W1561808238 @default.
- W2037571269 cites W1563678390 @default.
- W2037571269 cites W1596858049 @default.
- W2037571269 cites W1634007466 @default.
- W2037571269 cites W1649850841 @default.
- W2037571269 cites W1712686321 @default.
- W2037571269 cites W1775797309 @default.
- W2037571269 cites W1863242008 @default.
- W2037571269 cites W1892630873 @default.
- W2037571269 cites W1923296853 @default.
- W2037571269 cites W1933782576 @default.
- W2037571269 cites W1937091048 @default.
- W2037571269 cites W1964767638 @default.
- W2037571269 cites W1965656294 @default.
- W2037571269 cites W1970707286 @default.
- W2037571269 cites W1971962318 @default.
- W2037571269 cites W1974393412 @default.
- W2037571269 cites W1974719076 @default.
- W2037571269 cites W1975036168 @default.
- W2037571269 cites W1975486742 @default.
- W2037571269 cites W1979921178 @default.
- W2037571269 cites W1982125760 @default.
- W2037571269 cites W1984796697 @default.
- W2037571269 cites W1989509352 @default.
- W2037571269 cites W1995044678 @default.
- W2037571269 cites W1996830300 @default.
- W2037571269 cites W2003241928 @default.
- W2037571269 cites W2005556313 @default.
- W2037571269 cites W2010681628 @default.
- W2037571269 cites W2013782998 @default.
- W2037571269 cites W2014782452 @default.
- W2037571269 cites W2017418343 @default.
- W2037571269 cites W2017546865 @default.
- W2037571269 cites W2018077987 @default.
- W2037571269 cites W2032251485 @default.
- W2037571269 cites W2032459453 @default.
- W2037571269 cites W2033229237 @default.
- W2037571269 cites W2035661275 @default.
- W2037571269 cites W2037168657 @default.
- W2037571269 cites W2041191706 @default.
- W2037571269 cites W2046673561 @default.
- W2037571269 cites W2052528966 @default.
- W2037571269 cites W2052673198 @default.
- W2037571269 cites W2054747879 @default.
- W2037571269 cites W2059727200 @default.
- W2037571269 cites W2064433518 @default.
- W2037571269 cites W2065837783 @default.
- W2037571269 cites W2066073101 @default.
- W2037571269 cites W2076795790 @default.
- W2037571269 cites W2076952418 @default.
- W2037571269 cites W2084926856 @default.
- W2037571269 cites W2089011565 @default.
- W2037571269 cites W2089308771 @default.
- W2037571269 cites W2092301733 @default.
- W2037571269 cites W2092574457 @default.
- W2037571269 cites W2098779397 @default.
- W2037571269 cites W2107981066 @default.
- W2037571269 cites W2111986227 @default.
- W2037571269 cites W2120425185 @default.
- W2037571269 cites W2120887430 @default.
- W2037571269 cites W2127570720 @default.
- W2037571269 cites W2128251347 @default.
- W2037571269 cites W2131005822 @default.
- W2037571269 cites W2135859374 @default.
- W2037571269 cites W2137729302 @default.
- W2037571269 cites W2139192420 @default.
- W2037571269 cites W2141396940 @default.
- W2037571269 cites W2148580551 @default.
- W2037571269 cites W2151763383 @default.
- W2037571269 cites W2152322721 @default.
- W2037571269 cites W2161963059 @default.
- W2037571269 cites W2164522782 @default.
- W2037571269 cites W2170559182 @default.
- W2037571269 cites W2171690125 @default.
- W2037571269 cites W2172139298 @default.
- W2037571269 cites W2270732534 @default.
- W2037571269 doi "https://doi.org/10.1785/0120110096" @default.
- W2037571269 hasPublicationYear "2012" @default.
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