Frictional afterslip following the 2005 Nias-Simeulue earthquake, Sumatra
Continuously recording Global Positioning System stations near the 28 March 2005 rupture of the Sunda megathrust [moment magnitude (Mw) 8.7] show that the earthquake triggered aseismic frictional afterslip on the subduction megathrust, with a major fraction of this slip in the up-dip direction from...
| Váldodahkkit: | , , , , , , , , |
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| Materiálatiipa: | Journal Article |
| Giella: | English |
| Almmustuhtton: |
2012
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| Fáttát: | |
| Liŋkkat: | https://hdl.handle.net/10356/94599 http://hdl.handle.net/10220/8671 |