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Corrigendum to: ‘A Comparison of Oxygen Fugacities of Strongly Peraluminous Granites across the Archean–Proterozoic Boundary’

机译：勘犯：“跨越危险花岗岩的氧气度假率比较”跨越丛生古代边界“

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Claire E Bucholz; Edward M Stolper; John M Eiler; Frederick W Breaks;
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1. Multiple convergences along an Archean craton margin: Clues from Proterozoic ophiolite remnants, granites and granulite domains along the SE margin of India [J] . Saha Dilip, Sain Arnab Journal of geodynamics . 2019,第SEPa期

机译：沿太古代克拉通边缘的多重收敛：印度东南边缘沿元古代蛇绿岩遗迹，花岗岩和花岗石区域的线索
2. Multiple convergences along an Archean craton margin: Clues from Proterozoic ophiolite remnants, granites and granulite domains along the SE margin of India [J] . Saha Dilip, Sain Arnab Journal of geodynamics . 2019,第Sepa期

机译：沿着Archean Craton Rapgin的多次收敛：印度SE裕度的正常古代眼科遗留，花岗岩和粒状域的线索
3. Reactivation of the Archean-Proterozoic suture along the southern margin of Laurentia during the Mazatzal orogeny: Petrogenesis and tectonic implications of ca. 1.63 Ga granite in southeastern Wyoming [J] . Daniel S. Jones, Calvin G. Barnes, Wayne R. Premo Geological Society of America Bulletin . 2013,第1a2期

机译：在Mazatzal造山运动中沿Laurentia南部边缘的太古代-元古代缝合线的重新激活：岩石的成因和构造意义。怀俄明州东南部的1.63 Ga花岗岩
4. The Archean-Proterozoic Boundary in the Geologic History of the Earth [C] . Tamara F. Negrutsa, Vladimir Z. Negrutsa International GeologicalCongress . 1997

机译：地球地质历史中的阿奇 - 正古代边界
5. Geophysical investigation of Archean and Proterozoic crustal-scale boundaries in Wyoming and Colorado with emphasis on the Cheyenne Belt. [D] . Shoshitaishvili, Elena. 2002

机译：怀俄明州和科罗拉多州的太古代和元古代地壳尺度边界的地球物理研究，重点是夏安带。
6. Reply to Mulkidjanian and Galperin: Zn may have constrained evolution during the Proterozoic but not the Archean [O] . Christopher L. Dupont, Gustavo Caetano-Anollés 2010

机译：回复Mulkidjanian和Galperin：在元古代锌可能限制了进化但对太古代则没有限制
7. A Comparison of Oxygen Fugacities of Strongly Peraluminous Granites across the Archean–Proterozoic Boundary [O] . Claire E Bucholz, Edward M Stolper, John M Eiler, 2018

机译：跨越丛生古代边界强烈灭菌花岗岩的氧气度假村的比较

Corrigendum to: ‘A Comparison of Oxygen Fugacities of Strongly Peraluminous Granites across the Archean–Proterozoic Boundary’

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