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首页> 外文期刊>Contributions to Mineralogy and Petrology >Erratum to: Chemical interdiffusion of dacite and rhyolite: anhydrous measurements at 1 atm and 10 kbar, application of transition state theory, and diffusion in zoned magma chambers
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Erratum to: Chemical interdiffusion of dacite and rhyolite: anhydrous measurements at 1 atm and 10 kbar, application of transition state theory, and diffusion in zoned magma chambers

机译:勘误到:辉石和流纹岩的化学相互扩散:1 atm和10 kbar的无水测量,过渡态理论的应用,以及在分区岩浆室内的扩散

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摘要

On page 409 of Baker (1990), where the Boltzmann-Matano equation is presented, the term C_M in the equation was incorrectly described as the Matano interface. Instead, is the concentration at either the minimum or maximum along the diffusion profile whose origin is at the Matano interface, where x is set to 0. This mistake is only in the explanation of the term C_M in the equation and does not modify any results of Baker (1990).
机译:在Baker(1990)的第409页上,其中提出了Boltzmann-Matano方程,该方程中的C_M项被错误地描述为Matano接口。取而代之的是沿扩散轮廓的最小值或最大值处的浓度,其浓度起源于Matano界面,其中x设置为0。该错误仅在于解释方程式中的C_M且不修改任何结果贝克(1990)。

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