Fractional crystallization causes the iron isotope contrast between mid-ocean ridge basalts and abyssal peridotites
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Supplementary Information and Supplementary data 1-4 for the paper entitled "Fractional crystallization causes the iron isotope contrast between mid-ocean ridge basalts and abyssal peridotites". Topography data from Smith and Sandwell (1997) used to reproduce Figure 1b are also provided here. The files with Petrolog_Output prefix are the output of Petrolog3, which can be used to reproduce Figure 3.
创建时间：
2021-03-01
