Mantle Heat May Have Boosted Earth’s Crust 3 Billion Years Ago

Eos Pub Date : 2024-04-23 DOI:10.1029/2024eo240183
Rebecca Owen
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Abstract

Information from igneous zircon molecules gives researchers new insight into the workings of inner Earth.
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地幔热量可能在 30 亿年前推动了地球地壳的形成
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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Eos
Eos
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A Better Way to Predict Arctic Riverbank Erosion Climate Change Threatens 70% of Winemaking Regions Mars Mission’s Monetary Roller Coaster Hits New Lows What’s Next for the Anthropocene? Mantle Heat May Have Boosted Earth’s Crust 3 Billion Years Ago
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