Figure 4
From: Genesis of ultra-high-Ni olivine in high-Mg andesite lava triggered by seamount subduction
Sr–Nd–Pb isotopic compositions of the EC lavas. (a) 87Sr/86Sr vs. 143Nd/144Nd and (b) 206Pb/204Pb vs. 208Pb/204Pb compared with the Detroit Seamount49, 53 and Hawaiian Islands (GEOROC geochemical database: http://georoc.mpch-mainz.gwdg.de), MORB78, and previously reported compositions for EVF, KVG, and the Sredinny Range (SR) in Kamchatka7. Colors represent each rock type as identified in Fig. 2.
