{"refrec":{"BRefID":330464,"RR":"<b>Cobden, L.</b> (2020). Melt mapped inside Earth’s mantle. <i>Nature (Lond.) 586(7830)</i>: 506-507. <a href=\"https://dx.doi.org/10.1038/d41586-020-02925-x\" target=\"_blank\">https://dx.doi.org/10.1038/d41586-020-02925-x</a>","BEntID":324074,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Nature (Lond.) 586(7830)</i>: 506-507. <a href=\"https://dx.doi.org/10.1038/d41586-020-02925-x\" target=\"_blank\">https://dx.doi.org/10.1038/d41586-020-02925-x</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Cobden, L.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Cobden, L.","Englishabstract":"An analysis of seismic data reveals the location and quantity of melted rock, known as melt, in Earth’s upper mantle. The results show how these factors are correlated with the movement of the planet’s tectonic plates. 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