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Megathrusts exhumed
(2021). Megathrusts exhumed. Nature Geoscience 14(5): 255. https://hdl.handle.net/10.1038/s41561-021-00757-6
In: Nature Geoscience. Nature Publishing Group: London. ISSN 1752-0894; e-ISSN 1752-0908, meer
Is gerelateerd aan:
Arnulf, A.F.; Biemiller, J.; Lavier, L.; Wallace, L.M.; Bassett, D.; Henrys, S.; Pecher, I.; Crutchley, G.; Plaza-Faverola, A. (2021). Physical conditions and frictional properties in the source region of a slow-slip event. Nature Geoscience 14(5): 334-340. https://hdl.handle.net/10.1038/s41561-021-00741-0, meer
Guo, H.; McGuire, J.J.; Zhang, H. (2021). Correlation of porosity variations and rheological transitions on the southern Cascadia megathrust. Nature Geoscience 14(5): 341-348. https://hdl.handle.net/10.1038/s41561-021-00740-1, meer
Lindsey, E.O.; Mallick, R.; Hubbard, J.A.; Bradley, K.E.; Almeida, R.V.; Moore, J.D.P.; Bürgmann, R.; Hill, E.M. (2021). Slip rate deficit and earthquake potential on shallow megathrusts. Nature Geoscience 14(5): 321-326. https://hdl.handle.net/10.1038/s41561-021-00736-x, meer
Melnick, D. (2021). Unrushed megathrusts. Nature Geoscience 14(5): 260-261. https://hdl.handle.net/10.1038/s41561-021-00750-z, meer
Peer reviewed article  
Beschikbaar in
Abstract
    Plate boundary faults in subduction zones can generate large earthquakes and tsunamis. Recent studies have revealed that these faults slip in various ways and may be influenced by many factors. Better understanding them should improve hazard assessments.
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