{"refrec":{"BRefID":282013,"RR":"<b>Nooner, S.L.; Chadwick Jr., W.W.</b> (2016). Inflation-predictable behavior and co-eruption deformation at Axial Seamount. <i>Science (Wash.) 354(6318)</i>: 1399-1403. <a href=\"http://dx.doi.org/10.1126/science.aah4666\" target=\"_blank\">http://dx.doi.org/10.1126/science.aah4666</a>","BEntID":274032,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Science (Wash.) 354(6318)</i>: 1399-1403. <a href=\"http://dx.doi.org/10.1126/science.aah4666\" target=\"_blank\">http://dx.doi.org/10.1126/science.aah4666</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Nooner, S.L.; Chadwick Jr., W.W.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Nooner, S.L.; Chadwick Jr., W.W.","Englishabstract":"Deformation of the ground surface at active volcanoes provides information about magma movements at depth. Improved seafloor deformation measurements between 2011 and 2015 documented a fourfold increase in magma supply and confirmed that Axial Seamount’s eruptive behavior is inflation-predictable, probably triggered by a critical level of magmatic pressure. A 2015 eruption was successfully forecast on the basis of this deformation pattern and marked the first time that deflation and tilt were captured in real time by a new seafloor cabled observatory, revealing the timing, location, and volume of eruption-related magma movements. Improved modeling of the deformation suggests a steeply dipping prolate-spheroid pressure source beneath the eastern caldera that is consistent with the location of the zone of highest melt within the subcaldera magma reservoir determined from multichannel seismic results.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Inflation-predictable behavior and co-eruption deformation at Axial Seamount","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-06-15 01:32:57.847834","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2016,"MonPub":null,"DateUpdate":"2018-02-13","DateCreate":"2016-12-16","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000390261300037","VABBcode":null,"OpenAcc":0,"DOI":"10.1126/science.aah4666"},"refs":null,"anarec":{"AnaID":282013,"PubliDate":2016,"Pagination":"1399-1403","XtraPublOfAnaID":null,"ISBN":null,"Volume":"354","Issue":"6318","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":43776,"SerRR":"Science (Washington). 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