Metamorphic microdiamond formation is controlled by water activity, phase transitions and temperature
Abstract 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 under...
Main Authors: | J. Kotková, Y. Fedortchouk, R. Wirth, M. J. Whitehouse |
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Format: | Article |
Language: | English |
Published: |
Nature Publishing Group
2021-04-01
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Series: | Scientific Reports |
Online Access: | https://doi.org/10.1038/s41598-021-87272-1 |
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