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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...

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Detalles Bibliográficos
Autores principales: Kotková, J., Fedortchouk, Y., Wirth, R., Whitehouse, M. J.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2021
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