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On the partitioning of mantle heat loss below oceans and continents over time and its relationship to the Archaean paradox

机译：随着时间的推移与海洋和大陆低于海洋和大陆的分区及其与古代悖论的关系

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A. Lenardic;
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1. Global warming of the mantle beneath continents back to the Archaean [J] . Coltice N, Bertrand H, Rey P, Gondwana research: international geoscience journal . 2009,第3a4期

机译：大陆下方的地幔的全球变暖回到古生界
2. Evidence for a dominantly reducing Archaean ambient mantle from two redox proxies, and low oxygen fugacity of deeply subducted oceanic crust [J] . Sonja Aulbach, Alan B. Woodland, Richard A. Stern, Scientific reports. . 2019,第1期

机译：从两种氧化还原代理中占主导地位考古环境披风的证据，以及深层底层外壳的低氧气不足
3. Continental hyperextension, mantle exhumation, and thin oceanic crust at the continent-ocean transition, West Iberia: New insights from wide-angle seismic [J] . Davy R. G., Minshull T. A., Bayrakci G., Journal of geophysical research. Solid earth: JGR . 2016,第5期

机译：西伊比利亚大陆-海洋过渡带的大陆过度扩张，地幔掘出和薄薄的海洋壳：广角地震的新见解
4. Characteristics of the oceanic MCC, continental MCC, and coastal MCC over the Indonesian maritime continent [C] . Trismidianto International Symposium on LAPAN-IPB Satellite for Food Security and Environmental Monitoring . 2017

机译：印度尼西亚海洋大陆海洋MCC，大陆MCC和沿海MCC的特点
5. The structure and development of the continent-ocean transition zone of the Exmouth Plateau and Cuvier margin, Northwest Australia: Implications for extensional strain partitioning. [D] . Tischer, Michael Johann. 2006

机译：澳大利亚西北部埃克斯茅斯高原和库维埃边缘的大陆-海洋过渡带的结构和发育：对伸展应变分区的影响。
6. Publisher Correction: Maritime Continent water cycle regulates low-latitude chokepoint of global ocean circulation [O] . Tong Lee, Séverine Fournier, Arnold L. Gordon, -1

机译：出版商更正：海上大陆水循环调节全球海洋环流的低纬瓶颈
7. Archaean plate tectonics revisited 1. Heat flow, spreading rate, and the age of subducting oceanic lithosphere and their effects on the origin and evolution of continents [O] . Abbott Dallas Helen, Hoffman S. E. 1984

机译：古代古板块构造学的再研究1.热流，扩散速率，俯冲海洋岩石圈的年龄及其对大陆起源和演化的影响

On the partitioning of mantle heat loss below oceans and continents over time and its relationship to the Archaean paradox

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