An experimental demonstration of diamond formation in the dolomite-carbon and dolomite-fluid-carbon systems

European Journal of Mineralogy

Volumn 13, Issue 5, 2001, Pages 893-900

  Sokol, A G ^a   Borzdov, Y M ^a   Pal'Yanov, Y N ^a   Khokhryakov, A F ^a   Sobolev, N V ^a  

^a SOBOLEV INSTITUTE OF GEOLOGY AND MINERALOGY   (Russian Federation)

Author keywords

Carbon; Diamond crystallisation; Dolomite; Fluid; HP HT experiments

Indexed keywords

CARBON; CARBON DIOXIDE; CRYSTALLIZATION; FLUIDS; NUCLEATION;

CARBON SYSTEMS; DIAMOND FORMATION; DIAMOND NUCLEATION; DOLOMITE; EXPERIMENTAL DEMONSTRATIONS; INDUCTION PERIODS; NATURAL DIAMONDS; SEED CRYSTAL;

DIAMONDS;

CARBON; CRYSTALLIZATION; DIAMOND; DOLOMITE; FLUID COMPOSITION; HIGH PRESSURE; HIGH TEMPERATURE;

EID: 0034804180     PISSN: 09351221     EISSN: None     Source Type: Journal    
DOI: 10.1127/0935-1221/2001/0013/0893     Document Type: Article

References (34)

1. Synthesis of diamond from graphite-carbonate systems under very high temperature and pressure
2. Crystallization of diamond from C-O-H fluids under high-pressure and high-temperature conditions
3. Redox states of lithospheric and asthenospheric upper mantle
4. Experimental evidence for carbonate stability in the Earth's lower mantle
5. Formation of diamond
6. 2 systems to 12 GPa: Implications for the origin of kimberlite and carbonate stability in the Earth's upper mantle
7. 2 from 3 to 7 GPa
8. 2 at 6 GPa
9. Origin of group IA kimberlites: Fluid-saturated melting experiments at 45-55 kbar
10. Thermal stability of dolomite at high temperatures and pressures
11. A diamond trilogy: Superplumes, supercontinents, and supernovae
12. The properties of natural and synthetic diamond
13. On manmade diamonds
14. Hot spots of mantle and experiment to 10 GPa: Alkaline reactions, lithosphere carbonatization, and new diamond-generating systems
15. In situ X-ray diffraction of aragonite and dolomite at high pressure and high temperature: Evidence for dolomite breakdown to aragonite and magnesite
16. Inclusions in diamond
17. Growth conditions and real structure of synthetic diamond crystals
18. 3 solvent-catalysts at P=7 GPa and T=1700-1750 °C
19. 2-C systems
20. Diamond formation from mantle carbonate fluids
21. Experimental study of diamond crystallization in carbonate-carbon systems in connection with the problem of diamond genesis in magmatic and metamorphic rocks
22. 3-C at 7.7 GPa
23. Hydrous and carbonatitic mantle fluids in fibrous diamond from Jwaneng, Botswana
24. Diamond-bearing metamorphic rocks of the Kokchetav Massif (Northern Kazakhstan)
25. The deep-seated inclusions in kimberlites and the problem of the composition of the upper mantle
26. Mineral inclusions in diamonds from the Sputnik kimberlite pipe, Yakutia
27. Diamond inclusions in garnets from metamorphic rocks: A new environment for diamond formation
28. Formation conditions of diamond deposits
29. Fluid regime of diamond crystallisation in carbonate-carbon systems
30. 2 systems at high pressure of 9-10 GPa region
31. Magnesite-bearing inclusion assemblage in natural diamond
32. Diamond formation at high pressures
33. Mantle oxidation state and its relationship to tectonic environment and fluid speciation
34. Model system controls on conditions for formation of magnesiocarbonatite and calciocarbonatite magmas from the mantle