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The fate of water within Earth and super-Earths and implications for plate tectonics
The Earth is likely to have acquired most of its water during accretion. Internal heat of planetesimals by short-lived radioisotopes would have caused some water loss, but impacts into planetesimals were insufficiently energetic to produce further drying. Water is thought to be critical for the deve...
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| 出版年: | Philos Trans A Math Phys Eng Sci |
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| 主要な著者: | , |
| フォーマット: | Artigo |
| 言語: | Inglês |
| 出版事項: |
The Royal Society Publishing
2017
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| 主題: | |
| オンライン･アクセス: | https://ncbi.nlm.nih.gov/pmc/articles/PMC5394257/ https://ncbi.nlm.nih.gov/pubmed/28416729 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1098/rsta.2015.0394 |
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