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Structures of dolomite at ultrahigh pressure and their influence on the deep carbon cycle
Carbon-bearing solids, fluids, and melts in the Earth's deep interior may play an important role in the long-term carbon cycle. Here we apply synchrotron X-ray single crystal micro-diffraction techniques to identify and characterize the high-pressure polymorphs of dolomite. Dolomite-II, observe...
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| 主要な著者: | , , , , , , |
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| フォーマット: | Artigo |
| 言語: | Inglês |
| 出版事項: |
National Academy of Sciences
2012
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| 主題: | |
| オンライン･アクセス: | https://ncbi.nlm.nih.gov/pmc/articles/PMC3427128/ https://ncbi.nlm.nih.gov/pubmed/22869705 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1201336109 |
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