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A seismic reflection image for the base of a tectonic plate. <i>Nature (Lond.) 518(7537)</i>: 85–88. <a href=\"http://dx.doi.org/10.1038/nature14146\" target=\"_blank\">http://dx.doi.org/10.1038/nature14146</a>","BEntID":236268,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Nature (Lond.) 518(7537)</i>: 85–88. <a href=\"http://dx.doi.org/10.1038/nature14146\" target=\"_blank\">http://dx.doi.org/10.1038/nature14146</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Stern, T.A.; Henrys, S.A.; Okaya, D.; Louie, J.N.; Savage, M.K.; Lamb, S.; Sato, H.; Sutherland, R.; Iwasaki, T.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Stern, T.A. <i>et al.</i>","Englishabstract":"A high-resolution image for the base of an oceanic plate that is subducting beneath North Island, New Zealand, reveals a channel, which is interpreted as a sheared zone of ponded partial melts or volatiles; this low-viscosity channel decouples the plate from mantle flow beneath, allowing plate tectonics to work.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"A seismic reflection image for the base of a tectonic plate","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-06-14 01:31:29.486212","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2015,"MonPub":null,"DateUpdate":"2018-02-13","DateCreate":"2015-02-06","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000349098000036","VABBcode":null,"OpenAcc":0,"DOI":"10.1038/nature14146"},"refs":null,"anarec":{"AnaID":244583,"PubliDate":2015,"Pagination":"85–88","XtraPublOfAnaID":null,"ISBN":null,"Volume":"518","Issue":"7537","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":43431,"SerRR":"Nature: International Weekly Journal of Science. 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