In the paper, “Triple Oxygen (δ18O, Δ17O), Hydrogen (δ2H), and Iron (δ56Fe) Stable Isotope Signatures Indicate a Silicate Magma Source and Magmatic-Hydrothermal Genesis for Magnetite Orebodies at El Laco, Chile,” by Tristan Childress, Adam C. Simon, Martin Reich, Fernando Barra, Laura D. Bilenker, Nikita L. La Cruz, Ilya N. Bindeman, and J. Tomás Ovalle (Vol. 115, issue 7, 2020, p. 1529, Fig. 8), an incorrect graphic was used. The corrected figure and caption are below.

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