Abstract
Twenty eclogitic diamonds from Orapa Mine (Botswana) with an unusual yellow colour are characterised for their growth structure, N systematics, and C isotope composition, and the major element composition of their silicate inclusions. The diamonds show complex luminescence with green, blue and non-luminescent zones and occasional sector zonation. All parts of the diamonds have low total N concentrations (<50 at.ppm, with one exception of <125 at.ppm) and a limited range in C isotope composition (−5.7 to −10.6‰). Fourier Transform Infrared spectra show bands at 1334, 1332, 1282, and 1240 cm−1 typical for Ib-IaA diamonds. Relict unaggregated N defects (Nso and Ns+) are present and the preservation is likely caused by the low N concentrations and possible low mantle residence temperatures rather than young diamond formation (inclusion ages of 140, 1096, 1699 Ma; Timmerman et al. Earth Planet Sc Lett 463:178–188, 2017). Garnet and clinopyroxene inclusions extracted from 14 diamonds have an eclogitic composition with relatively low Ca contents and based on all characteristics, these diamonds form a distinct population from Orapa.
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Allsopp HL, Bristow JW, Smith CB, Brown R, Gleadow AJW, Kramers JD, Garvie OG (1989) A summary of radiometric dating methods applicable to kimberlites and related rocks. In: Ross J, Jacques AL, Ferguson J, Green DH, O'Reilly SY, Danchin RV, Janse AJA (eds) Kimberlites and Related Rocks Volume 1. Proceedings of the Fourth International Kimberlite Conference. Geological Society of Australia Special Publication 14, Perth, Australia, pp. 343–357
Babich YV, Feigelson BN (2009) Distribution of N+ centers in synthetic diamond single crystals. Inorg Mater 45:616–619
Boyd SR, Kiflawi I, Woods GS (1994) The relationship between infrared absorption and the A defect concentration in diamond. Philos Mag 69B:1149–1153
Cartigny P, Harris JW, Javoy M (1999) Eclogitic, peridotitic and metamorphic diamonds and the problems of carbon recycling—the case of Orapa (Botswana). In: The JB Dawson volume—Proceedings of the Seventh International Kimberlite Conference, Cape Town. Red Roof Design, Cape Town, pp 117–124
Cartigny P, Stachel T, Harris JW, Javoy M (2004) Constraining diamond metasomatic growth using C- and N-stable isotopes: examples from Namibia. Lithos 77:359–373
Clark CD, Davey ST (1984) One-phonon infrared absorption in diamond. J Phys C Solid State 17:1127–1140
Coleman RG, Lee DE, Beatty LB, Brannock WW (1965) Eclogites and eclogites: their differences and similarities. Geol Soc Am Bull 76:483–508
Collins AT, Mohammed K (1982) Optical studies of vibronic bands in yellow luminescing natural diamonds. J Phys C Solid State 15:147–158
Deines P, Harris JW (2004) New insights into the occurrence of 13C-depleted carbon in the mantle from two closely associated kimberlites: Letlhakane and Orapa, Botswana. Lithos 77:125–142
Deines P, Harris JW, Robinson DN, Gurney JJ, Shee SR (1991) Carbon and oxygen isotope variations in diamond and graphite eclogites from Orapa, Botswana, and the nitrogen content of their diamonds. Geochim Cosmochim Ac 55:515–524
Deines P, Harris JW, Gurney JJ (1993) Depth related carbon isotope and nitrogen concentration variability in the mantle below the Orapa kimberlite, Botswana, Africa. Geochim Cosmochim Ac 57:2781–1796
Deines P, Stachel T, Harris JW (2009) Systematic regional variations in diamond carbon isotopic composition and inclusion chemistry beneath the Orapa kimberlite cluster, in Botswana. Lithos 112:776–784
Droop GTR (1987) A general equation for estimating Fe3+ concentrations in ferromagnesian silicates and oxides from microprobe analyses, using stoichiometric criteria. Mineral Mag 51:431–435
Evans T, Qi Z (1982) The kinetics of the aggregations of nitrogen atoms in diamond. P Roy Soc Lond A Mat 381:159–178
Fritsch E (1998) The nature of color in diamonds. The Nature of Diamonds. Cambridge University Press, Cambridge, pp 23–47
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 26:145801–145806
Gress MU, Timmerman S, van den Heuvel Q, Schulten E, Chinn IL, Davies GR (2017) Variation in diamond growth events recorded in Botswanan diamonds. 11IKC extended abstract#4509
Gurney JJ, Harris JW, Rickard RS (1984) Silicate and oxide inclusions in diamonds from the Orapa Mine, Botswana. In: J. Kornprobst (Ed.), Kimberlites II: the mantle and crust–mantle relationships, Elsevier, Amsterdam, Dev Petrol 11:3–9
Hainschwang T, Fritsch E, Notari F, Rondeau B (2012) A new defect center in type Ib diamond inducing one phonon infrared absorption: the Y center. Diam Relat Mater 21:120–126
Kennedy CS, Kennedy GC (1976) The equilibrium boundary between graphite and diamond. J Geophys Res 81:2467–2470
Kiflawi I, Mayer AE, Spear PM, Van Wyk JA, Woods GS (1994) Infrared absorption by single nitrogen and A defect centres in diamond. Philos Mag 69B:1141–1147
King JM, Shigley JE, Gelb TH, Guhin SS, Hall M, Wang W (2005) Characterization and grading of natural-colour yellow diamonds. Gems Gemol 41:88–115
Kirkley MB, Gurney JJ, Otter ML, Hill SJ, Daniels LR (1991) The application of C isotope measurements to the identification of the sources of C in diamonds: a review. Appl Geochem 6:477–494
Klein-BenDavid O, Izraeli ES, Hauri E, Navon O (2004) Mantle fluid evolution—a tale of one diamond. Lithos 77:243–253
Krogh EJ (1988) The garnet-clinopyroxene Fe-Mg geothermometer - a reinterpretation of existing experimental data. Contrib Mineral Petrol 99:44–48
Lawson SC, Fisher D, Hunt DC, Newton ME (1998) On the existence of positively charged single-substitutional nitrogen in diamond. J Phys-Condens Mat 10:6171–6180
Liggins S (2010) Identification of point defects in treated single crystal diamond. Doctoral dissertation, University of Warwick, pp 241
Mendelssohn MJ, Milledge HJ (1995) Geologically significant information from routine analysis of the mid-infrared spectra of diamonds. Int Geol Rev 37:95–110
Meulemans TM, Borst AM, Davidheiser B, Davies GR. (2012) The origin and modification of the sub-continental lithospheric mantle of Botswana: constraints from peridotite xenoliths of the Orapa mine Botswana. 10IKC extended abstract#351
Navon O, Hutcheon ID, Rossman GR, Wasserburg GJ (1988) Mantle-derived fluids in diamond micro-inclusions. Nature 335:784–789
Petts DC, Stachel T, Stern RA, Hunt L, Fomradas G (2016) Multiple carbon and nitrogen sources associated with the parental mantle fluids of fibrous diamonds from Diavik, Canada, revealed by SIMS microanalysis. Contrib Mineral Petrol 171:1–15
Preston RP, Perritt SH, Seller MH, Wyatt BA (2012) Lithospheric structure beneath the Cretaceous Orapa kimberlite field, Botswana: 4D lithosphere imaging using garnet indicator mineral chemistry. 10IKC extended abstract#312
Schrauder M, Navon O (1994) Hydrous and carbonatitic mantle fluids in fibrous diamonds from Jwaneng, Botswana. Geochim Cosmochim Ac 58:761–771
Shee SR (1978) The mineral chemistry of xenoliths from the Orapa kimberlite pipe, Botswana. Unpublished M.Sc. thesis, University of Cape Town, Cape Town, pp 148
Shirey SB, Cartigny P, Frost DJ, Keshav S, Nestola F, Nimis P, Pearson DG, Sobolev NV, Walter MJ (2013) Diamonds and the geology of mantle carbon. In: Hazen RM, Jones AP, Baross JA (eds) Carbon in Earth. Rev Mineral Geochem, vol 75. Miner Soc Am, Chantilly, pp 355–421
Smit KV, Shirey SB, Wang W (2016) Type Ib diamond formation and preservation in the West African lithospheric mantle: Re–Os age constraints from sulphide inclusions in Zimmi diamonds. Precambrian Res 286:152–166
Stachel T, Harris JW (2008) The origin of cratonic diamonds - Constraints from mineral inclusions. Ore Geol Rev 34:5–32
Stachel T, Viljoen KS, McDade P, Harris JW (2004) Diamondiferous lithospheric roots along the western margin of the Kalahari Craton - the peridotitic inclusion suite in diamonds from Orapa and Jwaneng. Contrib Mineral Petrol 147:32–47
Taylor LA, Neal CR (1989) Eclogites with oceanic crustal and mantle signatures from the Bellsbank kimberlite, South Africa, Part I: mineralogy, petrography, and whole rock chemistry. J Geol 97:551–567
Taylor WR, Jaques AL, Ridd M (1990) Nitrogen-defect aggregation characteristics of some Australasian diamonds: time-temperature constraints on the source regions of pipe and alluvial diamonds. Am Mineral 75:1290–1310
Taylor WR, Canil D, Milledge HJ (1996) Kinetics of Ib to IaA nitrogen aggregation in diamond. Geochim Cosmochim Ac 60:4725–4733
Timmerman S, Matveev S, Gress MU, Davies GR (2015) A methodology for wavelength dispersive electron probe microanalysis of unpolished silicate minerals. J Geochem Explor 159:243–251
Timmerman S, Koornneef JM, Chinn IL, Davies GR (2017) Dated eclogitic diamond growth zones reveal variable recycling of crustal carbon through time. Earth Planet Sc Lett 463:178–188
Welbourn CM, Cooper M, Spear PM (1996) De Beers natural versus synthetic diamond verification instruments. Gems Gemol 32:156–169
Wiggers-de Vries DF (2013) Origin and evolution of Yakutian diamonds: constraints on sources and timing from a combined petrological and geochemical study of diamonds and their inclusions. Doctoral dissertation, VU University Amsterdam, pp. 275
Wiggers-de Vries DF, Pearson DG, Bulanova GP, Smelov AP, Pavlushin AD, Davies GR (2013a) 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 Ac 120:363–394
Wiggers-de Vries DF, Bulanova GP, De Corte K, Pearson DG, Craven JA, Davies GR (2013b) Micron-scale coupled carbon isotope and nitrogen abundance variations in diamonds: evidence for episodic diamond formation beneath the Siberian Craton. Geochim Cosmochim Ac 100:176–199
Woods GS, Collins AT (1983) Infrared absorption spectra of hydrogen complexes in type I diamonds. J Phys Chem Solids 44:471–475
Zedgenizov DA, Kalinina VV, Reutsky VN, Yuryeva OP, Rakhmanova MI (2016) Regular cuboid diamonds from placers on the northeastern Siberian platform. Lithos 265:125–137
Acknowledgments
We thank Sergei Matveev and Susan Verdegaal-Warmerdam for their help with the EPMA and SIRMS analyses respectively. John Freeth of De Beers Technologies UK is thanked for laser cutting and polishing the diamond plates. Debswana is thanked for the generous provision of diamonds for this study. We thank two anonymous reviewers and editor Thomas Stachel for constructive comments that greatly improved the paper.
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Photographs of the diamonds prior to polishing (PDF 314 kb)
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DiamondView™ images of both sides of the polished plates (PDF 3.19 mb)
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FTIR spectrum of each diamond in the one phonon region (PDF 621 kb)
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Table of band height at 1282 cm−1 of the FTIR spectra (XLSX 13.1 kb)
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Timmerman, S., Chinn, I.L., Fisher, D. et al. Formation of unusual yellow Orapa diamonds. Miner Petrol 112 (Suppl 1), 209–218 (2018). https://doi.org/10.1007/s00710-018-0592-9
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DOI: https://doi.org/10.1007/s00710-018-0592-9