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Economic Geology ( IF 5.8 ) Pub Date : 2020-12-01 , DOI: 10.5382/econgeo.115.8.er01


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.

中文翻译:

勘误表

在论文中,Tristan Childress撰写了“三氧(δ18O,Δ17O),氢(δ2H)和铁(δ56Fe)的稳定同位素特征,表明智利El Laco的硅酸盐岩浆源和岩浆水热成因”。亚当·西蒙(Adam C.Simon),马丁·赖希(Martin Reich),费尔南多·巴拉(Fernando Barra),劳拉·德​​·比伦克(Laura D.Bilenker),尼基塔·拉·克鲁兹(Ilya N.Bindeman)和J. ,使用了错误的图形。更正后的图形和标题如下。
更新日期:2020-12-18
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