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Metamorphic microdiamond formation is controlled by water activity, phase transitions and temperature
Metamorphic diamonds hosted by major and accessory phases in ultrahigh-pressure (UHP) metamorphic terranes represent important indicators of deep subduction and exhumation of continental crust at convergent plate boundaries. However, their nucleation and growth mechanisms are not well understood due...
Autores principales: | Kotková, J., Fedortchouk, Y., Wirth, R., Whitehouse, M. J. |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Nature Publishing Group UK
2021
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8032753/ https://www.ncbi.nlm.nih.gov/pubmed/33833325 http://dx.doi.org/10.1038/s41598-021-87272-1 |
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