{"refrec":{"BRefID":334934,"RR":"<b>Ito, G.</b> (2021). Oceanic fault zones reconstructed. <i>Nature (Lond.) 591(7850)</i>: 376-377. <a href=\"https://dx.doi.org/10.1038/d41586-021-00639-2\" target=\"_blank\">https://dx.doi.org/10.1038/d41586-021-00639-2</a>","BEntID":331491,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Nature (Lond.) 591(7850)</i>: 376-377. <a href=\"https://dx.doi.org/10.1038/d41586-021-00639-2\" target=\"_blank\">https://dx.doi.org/10.1038/d41586-021-00639-2</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Ito, G.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Ito, G.","Englishabstract":"Tectonic-plate material is generally thought to be neithercreated nor destroyed at plate boundaries called oceanictransform faults. 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