Erratum
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. 24056 –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.
Relationship between plagioclase An content and liquid An# in equilibrium for the H2O-saturated (light gray field) and dry experiments (dark gray field) of Waters and Lange (2015). Superimposed are ranges in An content of plagioclase phenocrysts from this study, at their respective whole-rock (i.e., ~liquid) An# (black bars). The overlap of data ranges with the dry experiments suggests that most crystals are not in equilibrium with hydrous mafic arc melts. Rather, if formed from hydrous melts, as indicated by hydrous melt inclusions in Mexican arc samples, the liquid An# of their equilibrium melts must have ranged to much lower values (down to An~10), i.e., crystals would have formed from much more evolved melts than those in which they are carried.
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Articles in the same Issue
- An evolutionary system of mineralogy. Part III: Primary chondrule mineralogy (4566 to 4561 Ma)
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- Fluid source and metal precipitation mechanism of sediment-hosted Chang’an orogenic gold deposit, SW China: Constraints from sulfide texture, trace element, S, Pb, and He-Ar isotopes and calcite C-O isotopes
- Iron isotope fractionation in reduced hydrothermal gold deposits: A case study of the Wulong gold deposit, Liaodong Peninsula, East China
- Tungsten mineralization during the evolution of a magmatic-hydrothermal system: Mineralogical evidence from the Xihuashan rare-metal granite in South China
- Crystallization and melt extraction of a garnet-bearing charnockite from South China: Constraints from petrography, geochemistry, mineral thermometry, and rhyolite-MELTS modeling
- Reducing epistemic and model uncertainty in ionic inter-diffusion chronology: A 3D observation and dynamic modeling approach using olivine from Piton de la Fournaise, La Réunion
- Memorial of James Joseph Papike (1937–2020)
- Erratum
Articles in the same Issue
- An evolutionary system of mineralogy. Part III: Primary chondrule mineralogy (4566 to 4561 Ma)
- Raman spectroscopy study of manganese oxides: Layer structures
- Raman signatures of the distortion and stability of MgCO3 to 75 GPa
- Competitive adsorption geometries for the arsenate As(V) and phosphate P(V) oxyanions on magnetite surfaces: Experiments and theory
- Probing the transformation paths from aluminum (oxy)hydroxides (boehmite, bayerite, and gibbsite) to metastable alumina: A view from high-resolution 27Al MAS NMR
- Crystal structures of K-cymrite and kokchetavite from single-crystal X-ray diffraction
- Fluid source and metal precipitation mechanism of sediment-hosted Chang’an orogenic gold deposit, SW China: Constraints from sulfide texture, trace element, S, Pb, and He-Ar isotopes and calcite C-O isotopes
- Iron isotope fractionation in reduced hydrothermal gold deposits: A case study of the Wulong gold deposit, Liaodong Peninsula, East China
- Tungsten mineralization during the evolution of a magmatic-hydrothermal system: Mineralogical evidence from the Xihuashan rare-metal granite in South China
- Crystallization and melt extraction of a garnet-bearing charnockite from South China: Constraints from petrography, geochemistry, mineral thermometry, and rhyolite-MELTS modeling
- Reducing epistemic and model uncertainty in ionic inter-diffusion chronology: A 3D observation and dynamic modeling approach using olivine from Piton de la Fournaise, La Réunion
- Memorial of James Joseph Papike (1937–2020)
- Erratum
