{"refrec":{"BRefID":243948,"RR":"<b>Dick, H.J.B.; Zhou, H.</b> (2015). Ocean rises are products of variable mantle composition, temperature and focused melting. <i>Nature Geoscience 8(1)</i>: 68-74. <a href=\"http://dx.doi.org/10.1038/ngeo2318\" target=\"_blank\">http://dx.doi.org/10.1038/ngeo2318</a>","BEntID":235651,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Nature Geoscience 8(1)</i>: 68-74. <a href=\"http://dx.doi.org/10.1038/ngeo2318\" target=\"_blank\">http://dx.doi.org/10.1038/ngeo2318</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Dick, H.J.B.; Zhou, H.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Dick, H.J.B.; Zhou, H.","Englishabstract":"The composition of mid-ocean ridge basalts varies with the properties of the mantle that feeds the ridges. 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