{"refrec":{"BRefID":242739,"RR":"<b>Marjanovic, M.; Carbotte, S.M.; Carton, H.; Nedimovic, M.R.; Mutter, J.C.; Canales, J.P.</b> (2014). A multi-sill magma plumbing system beneath the axis of the East Pacific Rise. <i>Nature Geoscience 7(11)</i>: 825–829. <a href=\"http://dx.doi.org/10.1038/ngeo2272\" target=\"_blank\">http://dx.doi.org/10.1038/ngeo2272</a>","BEntID":234438,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Nature Geoscience 7(11)</i>: 825–829. <a href=\"http://dx.doi.org/10.1038/ngeo2272\" target=\"_blank\">http://dx.doi.org/10.1038/ngeo2272</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Marjanovic, M.; Carbotte, S.M.; Carton, H.; Nedimovic, M.R.; Mutter, J.C.; Canales, J.P.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Marjanovic, M. <i>et al.</i>","Englishabstract":"At mid-ocean ridges, upper oceanic crust forms from a central magma reservoir, but it is unclear how the lower crust forms. 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