地幔热量可能在 30 亿年前推动了地球地壳的形成

Eos Pub Date : 2024-04-23 DOI:10.1029/2024eo240183
Rebecca Owen
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引用次数: 0

摘要

来自火成岩锆石分子的信息让研究人员对地球内部的运作有了新的认识。
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Mantle Heat May Have Boosted Earth’s Crust 3 Billion Years Ago
Information from igneous zircon molecules gives researchers new insight into the workings of inner Earth.
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Eos
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