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...

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Autores principales: J. Kotková, Y. Fedortchouk, R. Wirth, M. J. Whitehouse
Formato: article
Lenguaje:EN
Publicado: Nature Portfolio 2021
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Acceso en línea:https://doaj.org/article/f6d5b5892a714f4e89311eb149504134
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