Petrogenesis of antecryst-bearing arc basalts from the Trans-Mexican Volcanic Belt: Insights into along-arc variations in magma-mush ponding depths, H2O contents, and surface heat flux by G.F. Zellmer, M. Pistone, Y. Iizuka, B.J. Andrews, A. Gómez-Tuena, S.M. Straub, and E. Cottrell (November, vol. 101, p. 2405-2422, 2016). Article DOI: http://dx.doi.org/10.2138/am-2016-5701. Erratum DOI: http://dx.doi.org/10.2138/am-2021-E10632.

The position and shape of the fields of H2O saturated and dry compositions reported in Figure 6 are incorrect. The new Figure 6 below corrects this. Please note that this correction does not change our interpretation of the data we provided in the original paper.

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