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Fe-oxide concretions formed by interacting carbonate and acidic waters on Earth and Mars
Spherical Fe-oxide concretions on Earth, especially in Utah, USA, have been investigated as an analog of hematite spherules found in Meridiani Planum on Mars to support interpretations of water-rock interactions in early Mars. Although several formation mechanisms have been proposed for the Fe-oxide...
में बचाया:
| में प्रकाशित: | Sci Adv |
|---|---|
| मुख्य लेखकों: | , , , , , , , , , , |
| स्वरूप: | Artigo |
| भाषा: | Inglês |
| प्रकाशित: |
American Association for the Advancement of Science
2018
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| विषय: | |
| ऑनलाइन पहुंच: | https://ncbi.nlm.nih.gov/pmc/articles/PMC6281427/ https://ncbi.nlm.nih.gov/pubmed/30525103 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1126/sciadv.aau0872 |
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