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Jwaneng, Botswana. Geochim. Cosmochim. Acta 58, 761–771 (1994)
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environment for diamond formation. Nature 343, 742–746 (1990)
95. M. Akaishi, H. Kanda, S. Yamaoka, Synthesis of diamond from graphite-carbonate system
under very high temperature and pressure. J. Crystal Growth 104, 578–581 (1990)
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in the graphite-magnesium carbonate and graphite-K 2 Mg(CO 3 ) 2 systems at high pressure of
9–10 GPa region. J. Mater. Res. 11, 2622–2632 (1996)
97. Y.A. Litvin, L.T. Chudinovskikh, V.A. Zharikov, Crystallization of diamond and graphite in
the mantle alkaline carbonate melts in the experiments at pressure 7–11 GPa. Dokl. Akad.
Nauk SSSR 355, 669–672 (1997)
98. Y.A. Litvin, K.A. Aldushin, V.A. Zharikov, Synthesis of diamond at 8.5–9.5 GPa in the
system K 2 Ca(CO 3 ) 2 –Na 2 Ca(CO 3 ) 2 –C corresponding to the composition of fluidcarbonatitic
in inclusions diamond from kimberlites. Dokl. Akad. Nauk SSSR 367, 529–532 (1999)
99. A.G. Sokol, A.A. Tomilenko, Y.N. Palyanov, Y.M. Borzdov, G.A. Palyanova, A.F.
Khokhryakov, Fluid regime of diamond crystallisation in carbonate-carbon systems. Eur.
J. Mineral. 12, 367–375 (2000)
100. S. Ferro, Synthesis of diamond. J. Mater. Chem. 12, 2843–2855 (2002)
101. P.N. Gavryushkin, A. Behtenova, Z.I. Popov, V.V. Bakakin, A.Y. Likhacheva, K.D. Litasov,
A. Gavryushkin, Toward analysis of structural changes common for alkaline carbonates and
binary compounds: Prediction of high-pressure structures of Li 2 CO 3 , Na 2 CO 3 , and K 2 CO 3 .
Cryst. Growth Des. 16, 5612–5617 (2016)
102. J.W. Kim, H.G. Lee, Thermal and carbothermic decomposition of Na 2 CO 3 and Li 2 CO 3 .
Metall. Mater. Trans. B 32, 17–24 (2001)
103. A. Rohrbach, M.W. Schmidt, Redox freezing and melting in the Earth’s deep mantle resulting
from carbon–iron redox coupling. Nature 472, 209–212 (2011)
104. V. Stagno, D.O. Ojwang, C.A. McCammon, D.J. Frost, The oxidation state of the mantle and
the extraction of carbon from Earth’s interior. Nature 493, 84–88 (2013)
105. R. Burgess, E. Layzelle, G. Turner, J.W. Harris, Constraints on the age and halogen composition of mantle fluids in Siberian coated diamonds. Earth Planet. Sci. Lett. 197, 193–203
(2002)
106. L.H. Johnson, R. Burgess, G. Turner, J.W. Harris, Noble gas and halogen geochemistry of
mantle fluids: Comparison of African and Canadian diamonds. Geochim. Cosmochim. Acta
64, 717–732 (2000)
107. G. Turner, R. Burgess, M. Bannon, Isotope evidence for the involvement of recycled sediments
in diamond formation. Nature 344, 649–653 (1990)
108. Q. Zou, Y.G. Li, L.H. Zou, M.Z. Wang, Characterization of structures and surface states of
the nanodiamond synthesized by detonation. Mater. Charact. 60, 1257–1262 (2009)
109. J.H. Gong, M.S. Li, B. Xu, L.W. Yin, Y.X. Liu, H.G. Liu, TEM and DSC studies on the
synthesis diamond grown from Fe–Ni–C–B system under HPHT. J. Mater. Sci. 41, 3197–3200
(2006)
110. P.E. Pehrsson, T.W. Mercer, J.A. Chaney, Thermal oxidation of the hydrogenated diamond
(100) surface. Surf. Sci. 497, 13–28 (2002)
111. D. Berman, S.A. Deshmukh, S.K.R.S. Sankaranarayanan, A. Erdemir, A.V. Sumant,
Macroscale superlubricity enabled by graphene nanoscroll formation. Science 348, 1118–
1122 (2015)