Skip to main content
Fachgebiete
Automobil + Motoren Bauwesen + Immobilien Business IT + Informatik Elektrotechnik + Elektronik Energie + Nachhaltigkeit Finance + Banking Management + Führung Marketing + Vertrieb Maschinenbau + Werkstoffe Versicherung + Risiko
DE
EN
Bücher
Zeitschriften
Themenseiten
Organisationspsychologie Projektmanagement Marketing Smart Manufacturing
Weitere Formate
Podcasts Webinare Technik Webinare Wirtschaft Kongresse Veranstaltungskalender Awards
Jetzt Einzelzugang starten
Zugang für Unternehmen
Referenzkunden
SLX-Digitalkonferenz: Zukunftswerkstatt 2024

Mehr Umsatz mit Top-Kontakten

Am 7. Mai erfahren Sie, wie Vertriebsteams Leadgenerierung, Leadnurturing und Leadstrategien effizient steuern können.
Erweiterte Suche
Anmelden
nach oben
Erschienen in:
Introduction: Physico-Chemical Experiments as the Key to Diamond Genesis Problems Kapitel lesen Erstes Kapitel lesen

2017 | OriginalPaper | Buchkapitel

2. Mantle Rocks and Diamond-Associated Phases: Role in Diamond Origin

verfasst von : Yuriy A. Litvin

Erschienen in: Genesis of Diamonds and Associated Phases

Verlag: Springer International Publishing

Einloggen

Aktivieren Sie unsere intelligente Suche, um passende Fachinhalte oder Patente zu finden.

search-config
loading …

Abstract

The components of rock-forming and accessory minerals of the upper mantle, transition zone and lower mantle rocks have been involved into the processes of diamond genesis. Through their dissolving in primary carbonate melts, the mantle minerals have turned into components of the parental silicate-(±oxide)-carbonate-carbon melts-solutions for diamonds and co-crystallized paragenetic minerals. The minerals newly crystallized from the melts-solutions have been fragmentarily included into diamonds commonly growing with them.

Sie haben noch keine Lizenz? Dann Informieren Sie sich jetzt über unsere Produkte:

Springer Professional "Wirtschaft+Technik"

Online-Abonnement

Mit Springer Professional "Wirtschaft+Technik" erhalten Sie Zugriff auf:

  • über 102.000 Bücher
  • über 537 Zeitschriften

aus folgenden Fachgebieten:

  • Automobil + Motoren
  • Bauwesen + Immobilien
  • Business IT + Informatik
  • Elektrotechnik + Elektronik
  • Energie + Nachhaltigkeit
  • Finance + Banking
  • Management + Führung
  • Marketing + Vertrieb
  • Maschinenbau + Werkstoffe
  • Versicherung + Risiko

Jetzt Wissensvorsprung sichern!

Jetzt informieren

Springer Professional "Technik"

Online-Abonnement

Mit Springer Professional "Technik" erhalten Sie Zugriff auf:

  • über 67.000 Bücher
  • über 390 Zeitschriften

aus folgenden Fachgebieten:

  • Automobil + Motoren
  • Bauwesen + Immobilien
  • Business IT + Informatik
  • Elektrotechnik + Elektronik
  • Energie + Nachhaltigkeit
  • Maschinenbau + Werkstoffe




 

Jetzt Wissensvorsprung sichern!

Jetzt informieren
Vorheriges Kapitel Introduction: Physico-Chemical Experiments as the Key to Diamond Genesis Problems
Nächstes Kapitel Strongly Compressed Carbonate Systems in Diamond Genesis
Literatur
Akaogi M (2007) Phase transitions of minerals in the transition zone and upper part of the lower mantle In: Ohtani E (ed) Advances in high-pressure mineralogy, Geological Society of America Special Paper 421, pp 1–13. doi:10.​1130/​2007.​2421(01)
Akaogi M, Akimoto S (1979) High-pressure phase equilibria in a garnet lherzolite, with special reference to Mg2+–Fe2+ partitioning among constituent minerals. Phys Earth Planet Inter 19:31–51CrossRef
Angel RJ, Alvaro M, Nestola F, Mazzucchelli MI (2015) Diamond thermoelastic properties and implications for determining the pressure of formation of diamond-inclusion systems. Russ Geol Geophys 56(1–2):208–220
Aulbach S, Stachel T, Heaman LM, Carlson JA (2011) Microxenoliths from the Slave craton: archives of diamond formation along fluid conducts. Lithos 126:419–434CrossRef
Barashkov YP, Zudin NG (1997) Composition of garnets with diamond inclusions from kimberlite pipe Krasnopresnenskaya (Yakutia). Geol Geofiz 38(2):353–357
Bartoshinsky ZV (1960) On diamonds from eclogites of the kimberlitic pipe Mir. Geol Geofiz 6:129–131
Bobriyevich AP, Bondarenko MN, Gnevushev MA et al (1959) Diamond deposits of Yakutia. Gosgeoltechizdat, Moscow
Bobrov AV, Litvin YA (2009) Peridotite-eclogite-carbonatite systems at 7.0–8.5 GPa: concentration barrier of diamond nucleation and syngenesis of its silicate and carbonate inclusions. Russ Geol Geophys 50(12):1221–1233
Bobrov AV, Litvin YA (2011) Mineral equilibria of diamond-forming carbonate-silicate systems. Geochem Int 49(13):1–97CrossRef
Bobrov AV, Litvin YA, Dymshits AM (2011) Experimental studies of mantle carbonate–silicate systems and problem of the diamond formation. GEOS, Moscow, p 208
Bonney TG (1899) The parent rock of the diamond in South Africa. Geol Mag 6:309–321CrossRef
Bonney TG (1900) Additional notes on boulders and other rock specimen from the Newlands Diamond Mines, Griqualand-West. Proc R Soc Lond 67:475–484CrossRef
Corstophine GS (1908) The occurrence in kimberlite of garnet-pyroxene nodules carrying diamonds. Trans Geol Soc S Afr 10
Creighton S, Stachel T, McLean H et al (2008) Diamondiferous peridotitic microxenolith from the Diavik Diamond Mine, NT. Contrib Miner Petrol 155:541–554CrossRef
Davidson CF (1967) The so-called “cognate xenoliths” of kimberlite. In: Wyllie PJ (ed) The ultramafic and related rocks. New York, pp 269–278
Dawson JB (1968) Recent researches on kimberlite and diamond geology. Econ Geol 63(5):504–511CrossRef
Dawson JB, Smith JV (1975) Occurrence of diamond in a mica-garnet lherzolite xenoliths from kimberlite. Nature 254:580–581CrossRef
Dymshits AM, Bobrov AV, Litasov KD et al (2010) Experimental study of the pyroxene-garnet phase transition in the Na2MgSi5O12 system at pressures of 13–20 GPa: first synthesis of sodium majorite. Dokl Earth Sci 434(1):1263–1266CrossRef
Dymshits AM, Bobrov AV, Bindi L et al (2013) Na-bearing majoritic garnet in the Na2MgSi5O12–Mg3Al2Si3O12 join at 11–20 GPa: phase relations, structural peculiarities and solid solutions. Geochim Cosmochim Acta 105(1):13. doi:10.​1016/​j.​gsa.​2012.​11.​032
Fei Y, Wang Y, Finger LW (1996) Maximum solubility of FeO in (Mg, Fe)SiO2 perovskite as a function of temperature at 26 GPa: implication for FeO content in the lower mantle. J Geophys Res 101(B5):11525–11530CrossRef
Forbes RB (1965) The comparative chemical composition of eclogite and basalts. J Geophys Res 70:1515–1521CrossRef
Fursenko BA, Goryanov SB, Sobolev NV (2001) High pressures in coesite inclusions in diamond: combination scattering spectroscopy. Dokl Earth Sci 379:812–815
Gasparik T (2002) Stability of Na2Mg2Si2O7 and melting relations on the forsterite-jadeite join at pressures up to 22 GPa. Eur J Miner 9(2):311–326CrossRef
Gasparik T, Litvin YuA (1997) Stability of Na2Mg2Si2O7 and melting relations in the forsterite-jadeite join at pressures up to 22 GPa. Eur J Mineral 9:311–326
Glinnemann J, Kusaka K, Harris JW (2003) Oriented graphite single-crystal inclusions in diamond. Z Kristallogr 218:733–739
Griffin WL, Sobolev NV, Ryan CG et al (1993) Trace elements in garnets and chromites: diamond formation in the Siberian lithosphere. Lithos 29:235–256CrossRef
Gurney JJ, Siebert JC, Whitefield GG (1969) A diamondiferous eclogite from the Roberts Victor mine. In: Upper mantle project. Geological Society of South Africa Special Publication 2, pp 351–357
Haggerty SE (1986) Diamond genesis in a multiply-constrained model. Nature 520:34–38CrossRef
Harte B (2010) Diamond formation in the deep mantle: the record of mineral inclusions and their distribution in relation to mantle dehydration zones. Mineral Mag 74(2):189–215CrossRef
Harte B, Harris JW (1994) Lower mantle mineral association preserved in diamonds. Mineral Mag 58A:384–385CrossRef
Harte B, Cox KG, Gurney JJ (1975) Petrography and geological history of upper mantle xenoliths from the Matsoku kimberlite pipe. Phys Chem Earth 9:477–506CrossRef
Harte B, Harris JW, Hutchison MT et al (1999) Lower mantle mineral association in diamonds from Sao Luiz, Brazil. In: Fei Y, Bertka CM, Mysen BO (eds) Mantle petrology: field observations and high pressure experimentation: a tribute to Francis R. (Joe) Boyd. Geochemical Society Special Publication 6, pp 125–153
Hayman PC, Kopylova MG, Kaminsky FV (2005) Lower mantle diamonds from Rio Soriso (Juina area, Mato Grosso, Brazil). Contrib Mineral Petrol 149:430–445CrossRef
Hirose K (2002) Phase transitions in pyrolytic mantle around 670-km depth: Implications for upwelling of plumes from the lower mantle. J Geophys Res 107. doi:10.​1029/​2001JB000597
Holmes A, Paneth FA (1936) Helium ratios of rocks minerals from the diamond pipes of South Africa. Proc Royal Soc Lond A154:385–413CrossRef
Ilupin IP, Yefimova ES, Sobolev NV et al (1982) Inclusions in diamond from diamond-bearing dunite. Dokl Acad Nauk SSSR 264(2):454–456
Irifune T (1987) An experimental investigation of the pyroxene-garnet transformation in a pyrolite composition and its bearing on the constitution of the mantle. Phys Earth Planet Inter 45:324–336CrossRef
Izraeli ES, Schrauder M, Navon O (1998) On the connection between fluid and mineral inclusions in diamonds. In: VII International Kimberlite Conference Extended Abstracts, Cape Town, p. 352–354
Jacob D., Jagoutz E (1994) A diamond-graphite bearing xenolith from Roberrs Victor (South Africa): indications from petrogenesis from Pb-, Nb-, and Sr-isotopes. In: Meyer HOA, Leonardos OH (eds) Kimberlites, Related rocks and Mantle Xenoliths. Special Publication 1A-CPRM, p. 304–317
Kaminsky FV, Zakharchenko OD, Davies R et al (2001) Superdeep diamonds from the Juina area, Mato Grosso State, Brazil. Contrib Mineral Petrol 140:734–753CrossRef
Klein-BenDavid O, Logvinova AM, Izraeli ES et al (2003) Sulfide melt inclusions in Yubileinayan (Yakutia) diamonds. In: 8th International kimberlite conference extended abstracts, p 111
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(2–3):353–365CrossRef
Klein-BenDavid O, Izraeli FS, Hauri I, Navon O (2007a) Mantle fluid evolution—a tale of one diamond. Lithos 77:243–253CrossRef
Klein-BenDavid O, Izraeli FS, Hauri I, Navon O (2007b) Fluid inclusions in diamonds from the Diavik mine, Canada and the evolution of diamond-forming fluids. Geochim Cosmochim Acta 71(3):723–744CrossRef
Lee KKM, O’Neil B, Panero WR et al (2004) Equation of state of the high-pressure phases of a natural peridotite and implications for the Earth’s lower mantle. Earth Planet Sci Lett 223(3–4):381–393CrossRef
Leung IS, Guo W, Friedman I, Gleason J (1990) Natural occurrence of silicon carbide in diamondiferous kimberlite from Fuxian. Nature 346:352–354. doi:10.​1038/​346352a0 CrossRef
Leung IS, Taylor LA, Tsao CS, Han Z (1996) SiC in diamond and kimberlites: implications for nucleation and growth of diamond. Int Geol Rev 37:483–496
Litvin YA (1991) Physicochemical studies of melting in the earth’s interior. Nauka, Moscow, p 312
Litvin YA (1998) Hot spots of the mantle and experiment to 10 GPa: alkaline reactions, lithosphere carbonatization, and new diamond-generating systems. Russ Geol Geophys 39(12):1761–1767
Litvin YA (2007) High-pressure mineralogy of diamond genesis. In: Ohtani E (ed) Advances in high-pressure mineralogy. Geological Society of America Special Paper 421, pp 83–103. doi:10.​1130/​2007.​2421(06)
Litvin YuA (2009) The physicochemical conditions of diamond formation in the mantle matter: experimental studies. Russ Geol Geophys 50(12):1188–1200CrossRef
Litvin YA (2012) Physico-chemical formation conditions of natural diamond deduced from experimental study of the eclogite-carbonatite-sulfide-diamond system. Geol Ore Deposits 54(6):443–457CrossRef
Litvin YA (2013) Physico-chemical conditions of syngenesis of diamond and heterogeneous inclusions in the carbonate-silicate parental melts (experimental study). Mineral J 35(2):5–24
Litvin YA, Zharikov VA (1999) Primary fluid-carbonatite inclusions in diamond: experimental modeling in the system K2O–Na2O–CaO–MgO–FeO–CO2 as a diamond formation medium at 7–9 GPa. Dokl Earth Sci 367A:801–805
Litvin YA, Zharikov VA (2000) Experimental modeling of diamond genesis: diamond crystallization in multicomponent carbonate-silicate melts at 5–7 GPa and 1200–1570 °C. Dokl Earth Sci 373:867–870
Litvin YA, Litvin VY, Kadik AA (2008) Experimental characterization of diamond crystallization in melts of mantle silicate-carbonate-carbon systems at 7.0–8.5 GPa. Geochem Int 46(6):531–553
Litvin YA, Vasiliev PG, Bobrov AV et al (2012) Parental media of natural diamonds and primary mineral inclusions in them: evidence from physicochemical experiment. Geochem Int 50(9):726–759CrossRef
Litvin YA, Spivak AV, Kuzyura AV (2016) The bases of the mantle-carbonatite conception of diamond genesis. Geochem Int 10 (accepted)
Logvinova AM, Klein-BenDavid O, Izraeli ES et al (2003) Microinclusions in fibrous diamonds from Yubileinaya kimberlite pipe (Yakutia). In: VIII International kimberlite conference long abstract. Mineralogical Society of America, Victoria, Canada
Logvinova AM, Taylor LA, Floss C, Sobolev NV (2005) Geochemistry of multiple diamond inclusions of harzburgitic garnets as examined in-situ. Int Geol Rev 47:1223–1233CrossRef
Logvinova AM, Wirth R, Fedorova EN, Sobolev NV (2008) Nanometre-sized mineral and fluid inclusions in cloudy Siberian diamonds: new insights on diamond formation. Eur J Mineral 20:317–331CrossRef
Logvinova AM, Taylor LA, Fedorova EN et al (2015) A unique diamondiferous peridotite xenolith from the Udachnaya kimberlite pipe (Yakutia): role in subduction in diamond formation. Russ Geol Geophys 56(1–2):397–415
MacGregor ID, Carter JL (1970) The chemistry of clinopyroxenes and garnets of eclogite and peridotite xenoliths from the Roberts Victor Mine, South Africa. Phys Earth Planet Int 3:391–397CrossRef
Marakushev AA (1984) Peridotite nogules in kimberlites as the indicators for depp structure of lithosphere. In: Doklady of soviet geologists to the 27th session of international geological congress. Petrology. Publishing House “Nauka”, Moscow, pp 153–160
Marakushev AA, Bobrov AV (1998) Specificity of crystallization of eclogitic magmas within the diamond deep-situated facies. Dokl Acad Sci 358(4):526–530
Marx PC (1972) Pyrrotine and the origin of terrestrial diamonds. Mineral Mag 38:636–638CrossRef
Mathias M, Siebert JC, Rickwood PC (1970) Some aspects of the mineralogy and petrology of ultramafic xenoliths in kimberlite. Contrib Mineral Petrol 26:75–123CrossRef
McCallum ME, Eggler DH (1976) Diamonds in upper mantle peridotite nodule from kimberlite in Southern Wyoming. Science 192:253–256CrossRef
Meyer HOA, Boyd FR (1972) Composition and origin of crystalline inclusions in natural diamonds. Geochim Cosmochim Acta 36:1255–1273CrossRef
Navon O (1999). Diamond formation in the Earth’s mantle In: Gurney JJ, Gurney JL, Pascoe MD, Richardson SH (eds) Proceedings of the VII international kimberlite conference: red roof design, Cape Town, vol 2, pp 584–604
Navon O, Izraeli ES, KleinBen-David O (2003) Fluid inclusions in diamonds of the carbonatitic connection. In: VIII International kimberlite conference long abstract. Mineralogical Society of America, Victoria, Canada
Nestola F, Nimis P, Angel RJ et al (2014) Olivin with diamond-imposed morphology included in diamond. Syngenesis or protogenesis? Int Geol Rev 56:1658–1667CrossRef
O’Hara MJ (1968) The bearing of phase equilibria on synthetic and natural systems on the origin and evolution of basic and ultrabasic rocks. Earth Sci Rev 4:69–133CrossRef
O’Hara MJ, Yoder HS (1967) Formation and fractionation of basic magmas at high pressure. Scott J Geol 3:67–117CrossRef
Palot M, Pearson DG, Stern RA et al (2014) Isotopic constraints on the nature and circulation of deep mantle C–O–H–N fluids: carbon and nitrogen systematics within ultra-deep diamonds from Kankan (Guinea). Geochim Cosmochim Acta 139:24–46CrossRef
Pokhilenko NP, Sobolev NV, Sobolev VS, Lavrent’ev YG (1976) Xenolith of diamond-bearing ilmenite-pyropic lherzolite from Udachnaya pipe (Yakutia). Dokl Acad Nauk SSSR 231(2):438–441
Pokhilenko NP, Sobolev NV, Yefimova ES (1982) Xenolith of kataklazed diamond-bearing disten eclogites from the Udachnaya pipe, Yakutia. Dokl Acad Nauk SSSR 266(1):212–216
Ponomarenko AI, Sobolev NV, Pokhilenko NP et al (1976) Diamond-bearing grospydite and diamond-bearing disten eclogites from the kimberlite pipe Udachnaya, Yakutia). Dokl Acad Nauk SSSR 226(4):927–930
Ponomarenko AI, Spetsius ZV, Sobolev NV (1980) New type of diamond-bearing rocks—garnet-bearing pyroxenites. Dokl Acad Nauk SSSR 251(2):438–441
Rickwood PC, Mathias M (1970) Diamondiferous eclogite xenoliths in kimberlite. Lithos 3:223–235
Rickwood PC, Gurney J, White-Cooper DB (1969) The nature and occurrences of eclogite xenoliths in the kimberlites of Southern Africa. Geol Soc S Afr Spec Pub 2:371–393
Ringwood AE (1975) Composition and petrology of the earth’s mantle. McGraw-Hill, New York, p 618
Ringwood AE, Major A (1971) Synthesis of majorite and other high pressure garnets and perovskites. Earth Planet Sci Lett 12:411–418CrossRef
Satsukawa T, Griffin WT, Piazolo S, O’Reilly SY (2015) Messengers from the deep: fossil wadsleite-chromite microstructures from the mantle transition zone. Sci Rep 5:16484. doi:10.​1038/​srep16484 CrossRef
Shatsky VS, Ragozin A, Zedgenizov D Mityukhin S (2008) Evidence for multistage evolution of diamond-bearing eclogite from the Udachnaya kimperlite pipe. Lithos 105:289–300
Snyder GA, Taylor LA, Crozaz G et al (1997) The origin of Yakutian eclogite xenoliths. J Petrol 38:83–113CrossRef
Sobolev NV (1977) The deep-seated inclusions in kimberlites and the problem of the composition of the upper mantle. American Geophysical Union, Washington, D.C., 304 p
Sobolev NV, Kuznetsova IK (1965) New data on mineralogy of eclogites from kimberlitic pipes of Yakutia. Dokl Acad Nauk SSSR 163(2):471–474
Sobolev NV, Botkunov AI, Lavrent’ev YG (1974) Diamond-bearing corundum eclogite from kimberlite pipe Mir, Yakutia. Geol Geofiz 5
Sobolev NV, Efimova ES, Pospelova LN (1981) Native iron in diamond from Yakutia and its paragenesis. Geol Geofiz 22:25–29
Sobolev NV, Fursenko BA, Goryainov SV et al (2000) Fossilized high pressure from the Earth’s deep interior: coesite-in-diamond barometer. Proc Nat Acad Sci U S A 97(22):11875–11879CrossRef
Sobolev NV, Logvinova AM, Zedgenizov DA et al (2008) Petrogenetic significance of minor elements in olivines from diamonds and peridotite xenoliths from kimberlites of Yakutia. Lithos 112S:701–713
Sobolev NV, Logvinova AM, Yefimova ES (2009) Syngenetic inclusions of phlogopite of diamonds from kimberlites: evidence concerning the role of volatiles in diamond formation. Geol Geofiz 50(2):1588–1606
Sobolev VS (1960) Formation conditions of diamond deposits. Geol Geofiz 1:7–22
Sobolev VS, Naii BS, Sobolev NV et al (1969) Xenolith of diamond-bearing pyropic serpentinites from Aikhal pipe. Dokl Acad Nauk SSSR 188(5):1141–1143
Sobolev VS, Sobolev NV, Lavrent’ev YG (1972) Inclusions in diamonds from a diamond-bearing eclogite. Dokl Acad Nauk SSSR 207(1):164–167
Spetsius ZV, Taylor LA (2008) Diamonds of siberia: photographic evidence for their origin. Tranquility Base Press, Lenoir City, Tennessee, 278 p
Spetsius ZV, Bogush IN, Kovalchuk OE (2015) FTIR mapping of diamond plates of eclogitic and peridotitic xenoliths from the Nyurbimskaya pipe (Yakutia): genetic implications. Russ Geol Geophys 56(1–2):442–454
Stachel T (2001) Diamonds from the asthenosphere and the transition zone. Eur J Mineral 13(5):883–892CrossRef
Stachel T, Brey G, Harris JW (2000a) Kankan diamonds (Guines) I: from the lithosphere dawn to the transition zone. Contrib Mineral Petrol 140:1–15CrossRef
Stachel T, Brey GP, Harris W, Joswig W (2000b) Kankan diamonds (Guinea) II: lower mantle inclusion parageneses. Contrib Mineral Petrol 140:16–27
Stachel T, Brey G, Harris JW (2005) Inclusions in sublithospheric diamonds: glimpses of deep earth. Elements 1(2):73–78CrossRef
Stagno V, Tange Y, Miayjima N et al (2011) The stability of magnesite in the transition zone and the lower mantle as function of oxygen fugacity. Geophys Res Lett 38:L19309. doi:10.​1029/​2911GL049560 CrossRef
Stepanov AS, Shatsky VS, Zedgenizov DA, Sobolev NV (2007) Causes of variations in morphology and impurities of diamonds from the Udachnaya Pipe eclogite. Russ Geol Geofiz 48:758–769CrossRef
Stepanov AS, Shatsky VS, Zedgenizov DA, Sobolev NV (2008) Chemical heterogeneity in the diamondiferous eclogite xenolith from the Udachnaya kimberlite pipe. Dokl Earth Sci 419:308–311CrossRef
Streckeisen A (1976) To each plutonic rock its proper name. Earth Sci Rev 12:1–33CrossRef
Switzer G, Melson WG (1969) Partially melted kyanite eclogite from the Roberts Victor mine, South Africa. Contrib Earth Sci 1:1–9CrossRef
Takahashi T (1986) Melting of dry peridotite KLB-1 up to 14 GPa: implication to on the origin of peridotitic upper mantle. J Geophys Res 91:899367–899382
Taylor LA, Keller RA, Snyder GA et al (2000) Diamonds and their mineral inclusions, and what they tell us: a detailed «pull-apart» of a diamondiferous eclogites. Int Geol Rev 42:959–983
Titkov SV, Gorshkov AI, Solodova YP et al (2006) Mineral microinclusions in diamonds of cubic habitus from Yakutian deposits by data of analytic electronemicroscopy. Dokl Earth Sci 410(2):255–258
Tschauner O, Ma C, Becket JR et al (2014) Discovery of bridgmanite, the most abundant mineral in Earth, in a shocked meteorite. Science 346(6213):1100–1102CrossRef
Viljoen KS, Swash PM, Otter MI et al (1992) Diamondiferous garnet garzburgites from the Finsch kimberlite, Northern Cape, South Africa. Contrib Mineral Petrol 110:133–138CrossRef
Viljoen KS, Robinson DN, Swash PM et al (1994) Diamond and graphite-bearing peridotite xenoliths from the Roberts Victor kimberlite, South Africa. In: Meyer HOA, Leonardos OH (eds) Proceedings of fifth international kimberlite conference, vol 1. Araxa, Brazil, pp 285–303
Viljoen KS, Dobbe R, Smit B et al (2004) Petrology and geochemistry of a diamondiferous lherzolites from the premier diamond mine, South Africa. Lithos 77:539–552CrossRef
Von Eckermann HA (1967) Comparison of Swedish, African and Russian kimberlites. In: Wyllie PJ (ed) Ultramafic and related rocks. Wiley, New York, pp 302–312
Wagner PA (1909) Die diamantfuehrenden Gesteine Suedafrikas. Ihre Abbau und ihre Aufbereitung, Berlin
Wagner PA (1928) The evidence on the kimberlite pipes on the constitution of the outer part of the Earth. S Afr J Sci 25:125–148
Walter MJ, Bulanova GP, Armstrong LS et al (2008) Primary carbonate melt from deeply subducted oceanic crust. Nature 454:622–625CrossRef
Williams AF (1932) The genesis of the diamond, vols 1 and 2. Ernest Benn Ltd. London, 636 p
Yoder HS, Tilley CE (1962) Origin of basalt magmas: an experimental study of natural and synthetic rock systems. J Petrol 3:342–532CrossRef
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 68:61–73CrossRef
Zedgenizov DA, Ragozin AL, Shatsky VS et al (2009) Mg and Fe-rich carbonate-silicate high-density fluids in cuboid diamonds from the Internationalnaya kimberlite pipe (Yakutia). Lithos 112:638–647CrossRef
Zedgenizov DA, Ragozin AL, Shatsky VS et al (2011) Carbonate and silicate media of crystallization of fibrous diamonds from placers of north-eastern Siberian platform. Russ Geol Geophys 52(11):1649–1664CrossRef
Zedgenizov DA, Kagi H, Shatsky VS, Ragozin AL (2014) Local variations of carbon isotope composition in diamonds from São-Luis (Brazil): evidence for heterogenous carbon reservoir in sublithospheric mantle. Chem Geol 363:114–124CrossRef
Metadaten
Titel
Mantle Rocks and Diamond-Associated Phases: Role in Diamond Origin
verfasst von
Yuriy A. Litvin
Copyright-Jahr
2017
Buch
Genesis of Diamonds and Associated Phases

Print ISBN: 978-3-319-54542-4

Electronic ISBN: 978-3-319-54543-1

Copyright-Jahr: 2017

DOI
https://doi.org/10.1007/978-3-319-54543-1_2