{"refrec":{"BRefID":337159,"RR":"(2021). Megathrusts exhumed. <i>Nature Geoscience 14(5)</i>: 255. <a href=\"https://hdl.handle.net/10.1038/s41561-021-00757-6\" target=\"_blank\">https://hdl.handle.net/10.1038/s41561-021-00757-6</a>","BEntID":333781,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Nature Geoscience 14(5)</i>: 255. <a href=\"https://hdl.handle.net/10.1038/s41561-021-00757-6\" target=\"_blank\">https://hdl.handle.net/10.1038/s41561-021-00757-6</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":null,"OrigTitleTranslFlag":0,"Authorstringtrunc":null,"Englishabstract":"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. 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