The role of mantle ultrapotassic fluids in diamond formation
- Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences, Pr. Koptuyga 3, 630090 Novosibirsk, Russia
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Edited by Ho-kwang Mao, Carnegie Institution of Washington, Washington, DC, and approved January 1, 2007 (received for review September 15, 2006)
Abstract
Analysis of data on micro- and nano-inclusions in mantle-derived and metamorphic diamonds shows that, to a first approximation, diamond-forming medium can be considered as a specific ultrapotassic, carbonate/chloride/silicate/water fluid. In the present work, the processes and mechanisms of diamond crystallization were experimentally studied at 7.5 GPa, within the temperature range of 1,400–1,800°C, with different compositions of melts and fluids in the KCl/K2CO3/H2O/C system. It has been established that, at constant pressure, temperature, and run duration, the mechanisms of diamond nucleation, degree of graphite-to-diamond transformation, and formation of metastable graphite are governed chiefly by the composition of the fluids and melts. The experimental data suggest that the evolution of the composition of deep-seated ultrapotassic fluids/melts is a crucial factor of diamond formation in mantle and ultrahigh-pressure metamorphic processes.
Footnotes
- *To whom correspondence should be addressed. E-mail: palyanov{at}uiggm.nsc.ru
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Author contributions: Y.N.P., V.S.S., N.V.S., and A.G.S. designed research; Y.N.P. and A.G.S. performed research; A.G.S. contributed new reagents/analytic tools; Y.N.P., V.S.S., N.V.S., and A.G.S. analyzed data; and Y.N.P., V.S.S., N.V.S., and A.G.S. wrote the paper.
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The authors declare no conflict of interest.
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This article is a PNAS Direct Submission.
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↵ † Under conditions of complete miscibility between water-containing melts and aqueous fluids, we will conventionally refer to water-poor and water-rich compositions as melts and fluids, respectively.
- Abbreviations:
- FG,
- film growth;
- TGG,
- temperature-gradient growth;
- UHP,
- ultrahigh-pressure.
- © 2007 by The National Academy of Sciences of the USA





