High internal pressures in diamond fluid inclusions determined by infrared absorption

Details High internal pressures in diamond fluid inclusions determined by infrared absorption High internal pressures in diamond fluid inclusions determined by infrared absorption

Oct 1991

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1991natur.353..746n&link_type=abstract

Nature (ISSN 0028-0836), vol. 353, Oct. 24, 1991, p. 746-748. Research supported by Israel Academy of Sciences and Humanities an

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16

Diamonds, Earth Mantle, Fluid Pressure, Geophysical Fluids, High Pressure, Inclusions, Infrared Absorption, Internal Pressure, Peridotite

Scientific paper

Infrared spectroscopic evidence is reported for residual internal pressures of 1.5-2.1 GPa within fluid microinclusions in cubic and coated diamonds. These pressures fall within the diamond stability field in the upper mantle, suggesting that the deep-seated fluids, rich in H2O, CO2, SiO2, and K2O, are probably the mother solutions from which cubic, and possibly eclogitic, diamonds grow.

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