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Mineralogy and Petrology

, Volume 113, Issue 3, pp 285–306 | Cite as

Protracted fluid-metasomatism of the Siberian diamondiferous subcontinental lithospheric mantle as recorded in coated, cloudy and monocrystalline diamonds

  • Sergei Yu. SkuzovatovEmail author
  • Dmitry A. Zedgenizov
Original Paper
  • 146 Downloads

Abstract

Five typical coated diamonds (from Udachnaya, Yubileynaya, and Aikhal kimberlite pipes) with untypically low microinclusion abundances and four monocrystalline diamonds (Udachnaya, Mir, Nyurbinskaya pipes) that exhibit thin intermediate microinclusion-bearing zones were examined in details for growth structures, characteristic infrared absorption and photoluminescence, and composition of microinclusions. The internal structures of diamonds of both types imply that fluid inclusions entrapment in diamonds does not necessarily relate to the terminal stage of rapid fibrous growth. Instead, nitrogen aggregation state in some diamonds showed that both fibrous coats and inclusion-bearing layers might experience an annealing during mantle residence long enough to pre-date the ultimate kimberlite eruption, whereas the diamonds with internal inclusion-bearing zones also experienced later protracted history of monocrystalline growth. The presence of chloride-carbonate-silicate fluids/melts in monocrystalline diamonds indicate their generation from media generally similar to that observed in some fibrous diamonds. However, the composition of these metasomatizing fluids is different for the mantle beneath Udachnaya (mostly carbonatitic) and other pipes (Aikhal, Yubileynaya, Mir; variable abundance of silicic high-density fluids). The abundance of silica-rich fluids record either a heterogeneous distribution of eclogites in the subcontinental lithospheric mantle, or the operation of silica-rich slab-derived fluids. The inclusion abundance as well as the type of growth (fibrous or monocrystalline) is considered to be controlled by the volume of fluid fluxes; in this case, fluid consumption leads to decreasing growth rates, diminishing inclusion entrainment and stability of layered octahedrons. The detected minor compositional variations of high-density fluids in these diamonds may be due to local scale thermal perturbation in the host source and/or limited chemical heterogeneity of the parental fluid. The high amount of chlorides in high-density fluids from monocrystalline diamonds provide a new evidence for compositions of fluids/melts acting as primary metasomatic agent in the deep mantle of Siberian craton.

Keywords

Siberian craton Diamond Coated diamonds Monocrystalline diamonds Nitrogen Fluid inclusions 

Notes

Acknowledgements

The authors are grateful to Alexander Rakevich (Institute of Laser Physics, Irkutsk, Russia) for performing PL studies that were partially funded by the Russian Foundation for Basic Research (grant 16-35-50020). The SpectrExamination software was compiled and kindly provided by Oleg Kovalchuk, Alrosa Co. We appreciate the effort of Yaakov Weiss and two anonymous experts whose constructive reviews helped to significantly improve the manuscript. This study is a contribution to the Russian Science Foundation grant 16-17-10067.

Supplementary material

710_2019_656_MOESM1_ESM.pdf (1.7 mb)
Fig. S1 (PDF 1783 kb)
710_2019_656_MOESM2_ESM.pdf (1.8 mb)
Fig. S2 (PDF 1850 kb)
710_2019_656_MOESM3_ESM.xlsx (16 kb)
Table S1 (XLSX 15 kb)
710_2019_656_MOESM4_ESM.xls (76 kb)
Table S2 (XLS 75 kb)

References

  1. Agashev AM, Pokhilenko NP, Tolstov AV, Polyanichko VV, Malkovets VG, Sobolev NV (2004) New age data on kimberlites from the Yakutian diamondiferous province. Dokl Earth Sci 399(8):1142–1145Google Scholar
  2. Akagi T, Masuda A (1988) Isotopic and elemental evidence for a relationship between kimberlite and Zaire cubic diamonds. Nature 336(6200):665–667Google Scholar
  3. Araujo DP, Griffin WL, O’Reilly S, Grant KJ, Ireland T, Holden P, Achterbergh P (2009) Microinclusions in monocrystalline octahedral diamonds and coated diamonds from Diavik, Slave craton: clues to diamond genesis. Lithos 112S:724–735Google Scholar
  4. Aulbach S, Shirey SB, Stachel T, Creighton S, Muehlenbachs K, Harris JW (2009) Diamond formation episodes at the southern margin of the Kaapvaal Craton: Re-Os systematics of sulfide inclusions from the Jagersfontein Mine. Contrib Mineral Petrol 157(4):525–540Google Scholar
  5. Bogush IN, Spetsius ZV, Koval’chuk OE, Pomazanskiy BS (2016) Distribution of structural impurities and fluid microinclusions in cubic and coated diamond crystals from the Udachnaya pipe, Yakutia, Russia. Geochem Int 54(8):681–690Google Scholar
  6. Bokii GB, Bezrukov GN, Klyuev YA, Naletov AM, Nepsha VI (1986) Natural and synthetic diamonds. Nauka, Moscow (in Russian)Google Scholar
  7. Bovenkerk HP, Bundy FP, Hall HT, Strong HM, Wentorf RH (1959) Preparation of diamond. Nature 184:14−18Google Scholar
  8. Boyd SR, Mattey DP, Pillinger CT, Milledge HJ, Mendelssohn M, Seal M (1987) Multiple growth events during diamond genesis: an integrated study of carbon and nitrogen isotopes and nitrogen aggregation state in coated stones. Earth Planet Sc Lett 86:341–353Google Scholar
  9. Boyd SR, Kiflawi I, Woods GS (1995) Infrared absorption by the B nitrogen aggregate in diamond. Philos Mag B 72:351–361Google Scholar
  10. Bulanova GP, Wiggers de Vries DF, Pearson DG, Beard A, Mikhail S, Smelov AP, Davies GR (2014) An eclogitic diamond from Mir pipe (Yakutia), recording two growth events from different isotopic sources. Chem Geol 381:40–54Google Scholar
  11. Burgess R, Turner G, Harris JW (1992) 40Ar–39Ar laser probe studies of clinopyroxene inclusions in eclogitic diamonds. Geochim Cosmochim Acta 56:389–402Google Scholar
  12. Burgess R, Layzelle E, Turner G, Harris JW (2002) Constraints on the age and halogen composition of mantle fluids in Siberian coated diamonds. Earth Planet Sc Lett 197:193–203Google Scholar
  13. Cartigny P, Stachel T, Harris JW, Javoy M (2004) Constraining diamond metasomatic growth using C- and N-stable isotopes: examples from Namibia. Lithos 77:359–373Google Scholar
  14. Chen F, Guo JG, Chen JC, Liu CR (1992) First discovery of high potassium and high chlorine in diamond. Chin Sci Bull 37:1557–1560Google Scholar
  15. Chrenko RM, McDonald RS, Darrow KA (1967) Infra-red spectrum of diamond coat. Nature 213:474–476Google Scholar
  16. Chrenko RM, Tuft RE, Strong HM (1977) Transformation of the state of nitrogen in diamond. Nature 270:141–144Google Scholar
  17. Collins AT, Stanley M (1985) Absorption and luminescence studies of synthetic diamond in which the nitrogen has been aggregated. J Phys D Appl Phys 18:2537–2545Google Scholar
  18. Dalton JA, Presnall DC (1998) The continuum of primary carbonatitic-kimberlitic melt compositions in equilibrium with lherzolite: data from the system CaO-MgO-Al2O3-SiO2-CO2 at 6 GPa. J Petrol 39:1953–1964Google Scholar
  19. Dawson JB (2002) Metasomatism and partial melting in upper-mantle xenoliths from the Lashaine volcano, Northern Tanzania. J Petrol 43(9):1749–1777Google Scholar
  20. Dawson JB, Smith JV (1977) The MARID (mica-amphibole-rutile-ilmenite-diopside) suite of xenoliths in kimberlite. Geochim Cosmochim Acta 41:309–323Google Scholar
  21. De Weerdt F, Collins AT (2006) Optical study of the annealing behaviour of the 3107 cm−1 defect in natural diamonds. Diam Relat Mater 15:593–596Google Scholar
  22. Doucet LS, Ionov DA, Golovin AV (2014) Paleoproterozoic formation age for the Siberian cratonic mantle: Hf and Nd isotope data on refractory peridotite xenoliths from the Udachnaya kimberlite. Chem Geol 391:42–55Google Scholar
  23. Dyer HB, Raal FA, Du Preez L, Loubser JHN (1965) Optical absorption features associated with paramagnetic nitrogen in diamond. Philos Mag 11(112):763–774Google Scholar
  24. Ellis D, Wyllie P (1980) Phase relations and their petrological implications in the system MgO-SiO2-CO2-H2O at pressures up to 100 kbar. Am Mmeral 65:540–556Google Scholar
  25. Erlank AJ, Waters FG, Hawkesworth CJ, Haggerty SE, Allsopp HL, Rickard RS, Menzies MA (1987) Evidence for mantle metasomatism in peridotite nodules from the Kimberly pipes, South Africa. In: Menzies MA, Hawkesworth C (eds) Mantle metasomatism. Academic, London, pp 221–309Google Scholar
  26. Evans T, Harris JW (1989) Nitrogen aggregation, inclusion equilibration temperatures and the age of diamonds. In: Ross N (ed) Kimberlites and related rocks, vol 2, Geological Society Special Publication, vol 14, pp 1001–1006Google Scholar
  27. Evans T, Qi Z (1982) The kinetics of the aggregation of nitrogen atoms in diamond. P Roy Soc A–Math Phy 381:169–178Google Scholar
  28. Field JE (1992) The properties of natural and synthetic diamond. Academic Press, London, 710 pGoogle Scholar
  29. Giardini AA, Tydings JE (1962) Diamond synthesis: observations on the mechanism of formation. Am Mineral 47:1393–1421Google Scholar
  30. Gladkochub D, Pisarevsky SA, Donskaya T, Natapov LM, Mazukabzov A, Stanevich AM, Sklyarov E (2006) Siberian craton and its evolution in terms of Rodinia hypothesis. Episodes 29:169–174Google Scholar
  31. Golovin AV, Sharygin IS, Kamenetsky VS, Korsakov AV, Yaxley GM (2018) Alkali-carbonate melts from the base of cratonic lithospheric mantle: links to kimberlites. Chem Geol 483:261–274Google Scholar
  32. Goss JP, Briddon PR, Hill V, Jones R, Rayson MJ (2014) Identification of the structure of the 3107 cm−1 H-related defect in diamond. J Phys-Condens Mat 26:145801Google Scholar
  33. Graham RJ, Buseck PR (1994) Cathodoluminescence of brown diamonds as observed by transmission electron microscopy. Philos Mag B 70:1177–1185Google Scholar
  34. Griffin WL, Spetsius ZV, Pearson NJ, O'Reilly SY (2002) In situ Re-Os analysis of sulfide inclusions in kimberlitic olivine: new constraints on depletion events in the Siberian lithospheric mantle. Geochem Geophys 3(11):1–25Google Scholar
  35. Griffin WL, O’Reilly SY, Afonso JC, Begg GC (2009) The composition and evolution of lithospheric mantle: a re-evaluation and its tectonic implications. J Petrol 50:1185–1204Google Scholar
  36. Gurney JJ, Helmstaedt HH, Richardson SH, Shirey SB (2010) Diamonds through time. Econ Geol 105:689–712Google Scholar
  37. Guthrie GD, Veblen DR, Navon O, Rossman GR (1991) Submicrometer fluid inclusions in turbid-diamond coats. Earth Planet Sc Lett 105(1–3):1–12Google Scholar
  38. Haggerty SE (1986) Diamond genesis in a multiply-constrained model. Nature 320:34–38Google Scholar
  39. Hammouda T (2003) High-pressure melting of carbonated eclogite and experimental constraints on carbon recycling and storage in the mantle. Earth Planet Sc Lett 214:283–297Google Scholar
  40. Ionov DA, Doucet LS, Ashchepkov IV (2010) Composition of the lithospheric mantle in the Siberian craton: new constraints from fresh peridotites in the Udachnaya-East kimberlite. J Petrol 51(11):2177–2210Google Scholar
  41. Ionov DA, Doucet LS, Carlson RW, Golovin AV, Korsakov AV (2015) Post-Archean formation of the lithospheric mantle in the central Siberian craton: Re–Os and PGE study of peridotite xenoliths from the Udachnaya kimberlite. Geochim Cosmochim Acta 165:466–483Google Scholar
  42. Izraeli ES, Harris JW, Navon O (2001) Brine inclusions in diamonds: a new upper mantle fluid. Earth Planet Sc Lett 187:323–332Google Scholar
  43. Izraeli ES, Harris JW, Navon O (2004) Fluid and mineral inclusions in cloudy diamonds from Koffiefontein, South African. Geochim Cosmochim Acta 68:2561–2575Google Scholar
  44. Jablon BM, Navon O (2016) Most diamonds were created equal. Earth Planet Sc Lett 443:41–47Google Scholar
  45. Jones R, Briddon PR, Öberg S (1992) First-principles theory of nitrogen aggregates in diamond. Philos Mag Lett 66(2):67–74Google Scholar
  46. Kalfoun F, Ionov D, Merlet C (2002) HFSE residence and Nb/Ta ratios in metasomatised, rutile-bearing mantle peridotites. Earth Planet Sc Lett 199:49–65Google Scholar
  47. Kamiya Y, Lang AR (1965) On the structure of coated diamonds. Philos Mag 11:347–356Google Scholar
  48. Kanda H, Watanabe K (1997) Distribution of the cobalt-related luminescence center in HPHT diamond. Diam Relat Mater 6:708–711Google Scholar
  49. Khain EV, Bibikova EV, Salnikova EB, Kröner A, Gibsher AS, Didenko AN, Degtyarev KE, Fedotova AA (2003) The Palaeo-Asian ocean in the Neoproterozoic and early Palaeozoic: new geochronologic data and palaeotectonic reconstructions. Precambrian Res 122:329–358Google Scholar
  50. Kiflawi I, Bruley J (2000) The nitrogen aggregation sequence and the formation of voidites in diamond. Diam Relat Mater 9:87–93Google Scholar
  51. Kiflawi I, Fisher D, Kanda H, Sittas G (1996) The creation of the 3107 cm−1 hydrogen absorption peak in synthetic diamond single crystals. Diam Relat Mater 5:1516–1518Google Scholar
  52. Kinny PD, Griffin BJ, Heaman LM, Brakhfogel FF, Spetsius ZV (1997) SHRIMP U/Pb ages of perovskite and zircon from Yakutian kimberlites. Russ Geol Geophys 38:97–105Google Scholar
  53. Kitayama Y, Thomassot E, Galy A, Golovin A, Korsakov A, d'Eyrames E, Assayag N, Bouden N, Ionov D (2017) Co-magmatic sulfides and sulfates in the Udachnaya-East pipe (Siberia): a record of the redox state and isotopic composition of sulfur in kimberlites and their mantle sources. Chem Geol 455:315–330Google Scholar
  54. Klein-BenDavid O, Izraeli ES, Hauri E, Navon O (2004) Mantle fluid evolution - a tale of one diamond. Lithos 77:243–253Google Scholar
  55. Klein-BenDavid O, Wirth R, Navon O (2006) TEM imaging and analysis of microinclusions in diamonds: a close look at diamond-growing fluids. Am Mineral 91:353–365Google Scholar
  56. Klein-BenDavid O, Izraeli ES, Hauri E, Navon O (2007) Fluid inclusions in diamonds from the Diavik mine, Canada and the evolution of diamond-forming fluids. Geochim Cosmochim Acta 71(3):723–744Google Scholar
  57. Kohn SC, Speich L, Smith CB, Bulanova GP (2016) FTIR thermochronometry of natural diamonds: a closer look. Lithos 265:148–158Google Scholar
  58. Konzett J, Krenn K, Rubatto D, Hauzenberger C, Stalder R (2014) The formation of saline mantle fluids by open-system crystallization of hydrous silicate-rich vein assemblages – evidence from fluid inclusions and their host phases in MARID xenoliths from the central Kaapvaal Craton, South Africa. Geochim Cosmochim Acta 147:1–25Google Scholar
  59. Kopylova M, Navon O, Dubrovinsky L, Khachatryan G (2010) Carbonatitic mineralogy of natural diamond-forming fluids. Earth Planet Sc Lett 291:126–137Google Scholar
  60. Kupriyanov IN, Gusev VA, Borzdov YM, Kalinin AA, Pal’yanov YN (1999) Photoluminescence study of annealed nickel- and nitrogen-containing synthetic diamond. Diam Relat Mater 8(7):1301–1309Google Scholar
  61. Lang AR, Walmsley JC (1983) Apatite inclusions in natural diamond coat. Phys Chem Miner 9:6–8Google Scholar
  62. Litasov KD, Safonov OG, Ohtani E (2010) Origin of Cl-bearing silica-rich melt inclusions in diamonds: experimental evidence for an eclogite connection. Geology 38(12):1131–1134Google Scholar
  63. Logvinova AM, Wirth R, Fedorova EN, Sobolev NV (2008) Nanometresized mineral and fluid inclusions in cloudy Siberian diamonds: new insights on diamond formation. Eur J Mineral 20(3):317–331Google Scholar
  64. Logvinova AM, Wirth R, Tomilenko AA, Afanas’ev VP, Sobolev NV (2011) The phase composition of crystal-fluid nanoinclusions in alluvial diamonds in the notheastern Siberian Platform. Russ Geol Geophys 52:1286–1297Google Scholar
  65. Mendelssohn MJ, Milledge HJ (1995) Geologically significant information from routine analysis of the mid-infrared spectra of diamonds. Int Geol Rev 37:95–110Google Scholar
  66. Menzies M, Hawkesworth C (1987) Mantle metasomatism. Academic Press, London, 472 pGoogle Scholar
  67. Mernagh TP, Kamenetsky VS, Kamenetsky MB (2011) A Raman microprobe study of melt inclusions in kimberlites from Siberia, Canada, SW Greenland and South Africa. Spectrochim Acta A 80:82–87Google Scholar
  68. Meyer HOA (1987) Inclusions in diamond. In: Nixon PH (ed) Mantle xenoliths. Wiley, New York, pp 501–522Google Scholar
  69. Michaut C, Jaupart C, Mareschal J-C (2009) Thermal evolution of cratonic roots. Lithos 109:47–60Google Scholar
  70. Miller CE, Kopylova M, Smith E (2014) Mineral inclusions in fibrous diamonds: constraints on cratonic mantle refertilization and diamond formation. Miner Petrol 108:317–331Google Scholar
  71. Nadolinny VA, Yelisseyev AP, Baker JM, Newton ME, Twitchen DJ, Lawson SC, Yuryeva OP, Feigelson BN (1999) A study of 13C hyperfine structure in the EPR of nickel-nitrogen-containing centres in diamond and correlation with their optical properties. J Phys Condens Mat 11:7357–7376Google Scholar
  72. Nadolinny VA, Yur’eva OP, Yelisseyev AP, Pokhilenko NP, Chepurov AA (2004) Destruction of nitrogen B1 centers by plastic deformation of natural type IaB diamonds and behavior of the defects formed during P, T treatment. Dokl Earth Sci 399A:1268 (in Russsian)Google Scholar
  73. Navon O (1991) High internal pressures in diamond fluid inclusions determined by infrared absorption. Nature 353:746–748Google Scholar
  74. Navon O, Hutcheon ID, Rossman GR, Wasserburg GJ (1988) Mantle-derived fluids in diamond microinclusions. Nature 335:784–789Google Scholar
  75. O’Reilly SY, Griffin WL (2010) The continental lithosphere–asthenosphere boundary: can we sample it? Lithos 120(1–2):1–13Google Scholar
  76. Pal’yanov YN, Sokol AG, Borzdov YM, Khokhryakov AF, Sobolev NV (1999) Diamond formation from mantle carbonate fluids. Nature 400:417–418Google Scholar
  77. Palot M, Pearson DG, Stachel T, Harris JW, Bulanova GP, Chinn I (2013) Multiple growth episodes or prolonged formation of diamonds? Inferences from infrared absorption data. In: Pearson DG et al (ed) Proceedings of 10th International Kimberlite Conference, Vol. 1. J Geol Soc India, pp 281–296Google Scholar
  78. Palyanov YN, Sokol AG (2009) The effect of composition of mantle fluid/melts on diamond formation processes. Lithos 112:690–700Google Scholar
  79. Palyanov YN, Khokhryakov AF, Borzdov YM, Kupriyanov IN (2013) Diamond growth and morphology under the influence of impurity adsorption. Cryst Growth Des 13(12):5411–5419Google Scholar
  80. Pearson DG, Shirey SB, Carlson RW, Boyd FR, Pokhilenko NP, Shimizu N (1995a) Re–Os, Sm–Nd, and Rb–Sr isotope evidence for thick Archaean lithospheric mantle beneath the Siberian craton modified by multistage metasomatism. Geochim Cosmochim Acta 59:959–977Google Scholar
  81. Pearson DG, Snyder GA, Shirey SB, Taylor LA, Carlson RW, Sobolev NV (1995b) Archean Re-Os age for Siberian eclogites and constraints on Archean tectonics. Nature 374:711–713Google Scholar
  82. Pearson DG, Shirey SB, Harris JW, Carlson RW (1998) Sulphide inclusions in diamonds from the Koffiefontein kimberlite, S Africa: constraints on diamond ages and mantle Re-Os systematics. Earth Planet Sc Lett 160(3):311–326Google Scholar
  83. Pearson DG, Shirey SB, Bulanova GP, Carlson RW, Milledge HJ (1999) Re–Os isotope measurements of single sulfide inclusions in a Siberian diamond and its nitrogen aggregation systematics. Geochim Cosmochim Acta 63:703–711Google Scholar
  84. Pearson DG, Parman SW, Nowell GM (2007) A link between large mantle melting events and continent growth seen in osmium isotopes. Nature 449:202–205Google Scholar
  85. Plotnikova SP, Klyuev YA, Parfianovich KA (1980) Long-wave photoluminescence of natural diamonds. Mineralog Zhurnal 2(4):75–80 (in Russian)Google Scholar
  86. Rege S, Griffin WL, Pearson NJ, Araujo D, Zedgenizov D, O'Reilly SY (2010) Trace-element patterns of fibrous and monocrystalline diamonds: insights into mantle fluids. Lithos 118:313–337Google Scholar
  87. Richardson SH, Harris JW (1997) Antiquity of peridotitic diamonds from the Siberian craton. Earth Planet Sc Lett 151:271–277Google Scholar
  88. Richardson SH, Pöml PF, Shirey SB, Harris JW (2009) Age and origin of peridotitic diamonds from Venetia, Limpopo Belt, Kaapvaal–Zimbabwe craton. Lithos 112S:785–792Google Scholar
  89. Rosen OM, Condie KC, Natapov LM, Nozhkin AD (1994) Paleoproterozoic evolution of the Siberian craton: a preliminary assessment. In: Condie KC (ed) Archean crustal evolution. Elsevier, Amsterdam, pp 411–459Google Scholar
  90. Rudnick RL, Eldridge CS, Bulanova GP (1993) Diamond growth history from in situ measurement of Pb and S isotopic compostions of sulfide inclusions. Geology 21:13–16Google Scholar
  91. Rudnick RL, Barth M, Horn I, McDonough WF (2000) Rutile-bearing refractory eclogites: missing link between continents and depleted mantle. Science 287(5451):278–281Google Scholar
  92. Safonov OG, Perchuk LL, Litvin YA (2007) Melting relations in the chloride-carbonate-silicate systems at high-pressure and the model for formation of alkalic diamond-forming liquids in the upper mantle. Earth Planet Sc Lett 253:112–128Google Scholar
  93. Schrauder M, Navon O (1994) Hydrous and carbonatitic mantle fluids in fibrous diamonds from Jwaneng, Botswana. Geochim Cosmochim Acta 58(2):761–771Google Scholar
  94. Schrauder M, Koeberl C, Navon O (1996) Trace element analyses of fluid-bearing diamonds from Jwaneng, Botswana. Geochim Cosmochim Acta 60(23):4711–4724Google Scholar
  95. Shimizu N, Sobolev NV (1995) Young peridotitic diamonds from the Mir kimberlite pipe. Nature 375:394–397Google Scholar
  96. Shirey SB, Richardson SH (2011) Start of the Wilson cycle at 3 Ga shown by diamonds from subcontinental mantle. Science 333:434–436Google Scholar
  97. Shirey SB, Richardson SH, Harris JW (2004) Integrated models of diamond formation and craton evolution. Lithos 77:923–944Google Scholar
  98. Simon NSC, Carlson RW, Pearson D, Davies G (2007) The origin and evolution of the Kaapvaal cratonic lithospheric mantle. J Petrol 48:549–565Google Scholar
  99. Skuzovatov SY, Zedgenizov DA, Shatsky VS, Ragozin AL, Kuper KE (2011) Composition of cloudy microinclusions in octahedral diamonds from the Internatsional’naya kimberlite pipe (Yakutia). Russ Geol Geophys 52(1):85–96Google Scholar
  100. Skuzovatov SY, Zedgenizov DA, Ragozin AL, Shatsky VS (2012) Growth medium composition of coated diamonds from the Sytykanskaya kimberlite pipe (Yakutia). Russ Geol Geophys 53(11):1197–1208Google Scholar
  101. Skuzovatov SY, Zedgenizov DA, Rakevich AL, Shatsky VS, Martynovich EF (2015) Multiple growth events in diamonds with cloudy microinclusions from the Mir kimberlite pipe: evidence from the systematics of optically active defects. Russ Geol Geophys 56(1–2):330–343Google Scholar
  102. Skuzovatov SY, Zedgenizov DA, Howell D, Griffin WL (2016) Various growth environments of cloudy diamonds from the Malobotuobia kimberlite field (Siberian craton). Lithos 265:96–107Google Scholar
  103. Skuzovatov SY, Zedgenizov DA, Rakevich AL (2017) Spectroscopic constraints on growth of Siberian mixed-habit diamonds. Contrib Mineral Petrol 172(6):46Google Scholar
  104. Smith EM, Kopylova MG, Nowell GM, Pearson DG, Ryder J (2012) Archean mantle fluids preserved in fibrous diamonds from Wawa, Superior craton. Geology 40(12):1071–1074Google Scholar
  105. Sobolev NV (1977) Deep-seated inclusions in kimberlites and the problem of the composition of the upper mantle. American Geophysical Union, Washington, 279 pGoogle Scholar
  106. Sobolev EV, Lisoivan VI (1978) Nitrogen centers and the growth of natural diamond crystals. In: Kuznetsov VA (ed) Problems of crustal and upper-mantle petrology, Transactions of the Institute of Geology and Geophysics, Issue 403. Nauka, Novosibirsk, pp 245–255 (in Russian)Google Scholar
  107. Stachel T, Harris JW (2008) The origin of cratonic diamonds — constraints from mineral inclusions. Ore Geol Rev 34:5–32Google Scholar
  108. Stachel T, Luth RW (2015) Diamond formation — where, when and how? Lithos 220–223:200–220Google Scholar
  109. Sumida N, Lang AR (1988) On the measurement of population density and size of platelets in type Ia diamond and its implication for platelet structure models. Proc R. Soc Lond A 419(1857):235–257Google Scholar
  110. Sun J, Kostrovitsky SI, Tappe S, Liu CZ, Skuzovatov SY, Wu FY (2018) Mantle sources of kimberlites through time: a U-Pb and Lu-Hf isotope study of zircon megacrysts from the Siberian diamond fields. Chem Geol 479:228–240Google Scholar
  111. Sunagawa I (1990) Growth and morphology of diamond crystals under stable and metastable conditions. J Cryst Growth 99(1–4):1156–1161Google Scholar
  112. Taylor WR, Canil D, Milledge HJ (1996) Kinetics of Ib to IAa nitrogen aggregation in diamond. Geochim Cosmochim Acta 60:4725–4733Google Scholar
  113. Thibault Y, Edgar AD, Lloyd FE (1992) Experimental investigation of melts from a carbonated phlogopite lherzolite: implications for metasomatism in the continental lithospheric mantle. Am Mineral 77:784–794Google Scholar
  114. Thomaz MF, Davies G (1978) The decay time of N3 luminescence in natural diamond. P Roy Soc A–Math Phy 362:405–419Google Scholar
  115. Tomlinson E, De Schrijver I, De Corte K, Jones AP, Moens L, Vanhaecke F (2005) Trace element compositions of submicroscopic inclusions in coated diamond: a tool for understanding diamond petrogenesis. Geochim Cosmochim Acta 69(19):4719–4732Google Scholar
  116. Tomlinson E, Jones AP, Harris JW (2006) Co-existing fluid and silicate inclusions in mantle diamond. Earth Planet Sc Lett 250:581–595Google Scholar
  117. Tomlinson EL, Müller W, EIMF (2009) A snapshot of mantle metasomatism: trace element analysis of coexisting fluid (LA-ICP-MS) and silicate (SIMS) inclusions in fibrous diamonds. Earth Planet Sc Lett 279:362–372Google Scholar
  118. van Wyk JA (1982) Carbon-12 hyperfine interaction of the unique carbon of the P2 (ESR) or N3 (optical) Centre in diamond. J Phys C Solid State Phys 15:981–983Google Scholar
  119. Vins VG, Yelisseyev AP, Chigrin SV, Grizenko AG (2006) Natural diamond enhancement: the transformation of intrinsic and impurity defects in the diamond lattice. Gems Gemol 42:120–121Google Scholar
  120. Walmsley JC, Lang AR (1992a) Oriented biotite inclusions in diamond coat. Mineral Mag 56:108–111Google Scholar
  121. Walmsley JC, Lang AR (1992b) On sub-micrometre inclusions in diamond coat: crystallography and composition of ankerites and related rhombohedral carbonates. Mineral Mag 56:533–543Google Scholar
  122. Wang W, Gasparik T (2001) Metasomatic clinopyroxene inclusions in diamonds from the Liaoning province, China. Geochim Cosmochim Acta 65(4):611–620Google Scholar
  123. Weiss Y, Kessel R, Griffin WL, Kiflawi I, Klein-BenDavid O, Bell DR, Harris JW, Navon O (2009) A new model for the evolution of diamond-forming fluids: evidence from microinclusion-bearing diamonds from Kankan, Guinea. Lithos 112:660–674Google Scholar
  124. Weiss Y, Kiflawi I, Davies N, Navon O (2014) High-density fluids and the growth of monocrystalline diamonds. Geochim Cosmochim Acta 141:145–159Google Scholar
  125. Weiss Y, McNeill J, Pearson DG, Nowell GM, Ottley CJ (2015) Highly saline fluids from a subducted slab as the source for fluid-rich diamonds. Nature 524:339–342Google Scholar
  126. Weiss Y, Navon O, Goldstein SL, Harris JW (2018) Inclusions in diamonds constrain thermo-chemical conditions during Mesozoic metasomatism of the Kaapvaal cratonic mantle. Earth Planet Sc Lett 491:134–147Google Scholar
  127. Wiggers de Vries DF, Pearson DG, Bulanova GP, Smelov AP, Pavlushin AD, Davies GR (2013) Re-Os dating of sulphide inclusions zonally distributed in single Yakutian diamonds: evidence for multiple episodes of Proterozoic formation and protracted timescales of diamond growth. Geochim Cosmochim Acta 120:363–394Google Scholar
  128. Woods GS (1986) Platelets and the infrared absorption of type Ia diamonds. Proc R Soc Lond A 407:219–238Google Scholar
  129. Woods GS, Collins AT (1983) Infrared absorption spectra of hydrogen complex in type I diamonds. J Phys Chem Solids 44:471–475Google Scholar
  130. Yelisseyev A, Kanda H (2007) Optical centers related to 3d transition metals in diamond. New Diam Front C Tech 17(3):127–178Google Scholar
  131. Yelisseyev AP, Pokhilenko NP, Steeds JW, Zedgenizov DA (2004) Afanasiev VP (2004) features of coated diamonds from the snap Lake/King Lake kimberlite dyke, Slave craton, Canada, as revealed by optical topography. Lithos 77:83–97Google Scholar
  132. Zaitsev AM (2001) Optical properties of diamond: a data handbook. Heidelberg, Springer, Berlin, 502 pGoogle Scholar
  133. Zedgenizov DA, Kagi H, Shatsky VS, Sobolev NV (2004) Carbonatitic melts in cuboid diamonds from Udachnaya kimberlite pipe (Yakutia): evidence from vibrational spectroscopy. Mineral Mag 68(1):61–73Google Scholar
  134. Zedgenizov DA, Harte B, EIMF SVS, Politov AA, Rylov GM, Sobolev NV (2006) Directional chemical variations in diamonds showing octahedral following cuboid growth. Contrib Mineral Petrol 151(1):45–57Google Scholar
  135. Zedgenizov DA, Ragozin AL, Shatsky VS, Araujo D, Griffin WL, Kagi H (2009) Mg and Fe-rich carbonate-silicate high-density fluids in cuboid diamonds from the Internationalnaya kimberlite pipe (Yakutia). Lithos 112:638–647Google Scholar

Copyright information

© Springer-Verlag GmbH Austria, part of Springer Nature 2019

Authors and Affiliations

  1. 1.Vinogradov Institute of GeochemistryRussian Academy of SciencesIrkutskRussia
  2. 2.Novosibirsk State UniversityNovosibirskRussia
  3. 3.Sobolev Institute of Geology and MineralogyRussian Academy of SciencesNovosibirskRussia

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