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Genetic Mineralogy of Lower Mantle Diamonds and Their Inclusions

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Evolution of Magmatic and Diamond-Forming Systems of the Earth's Lower Mantle

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Abstract

The generalized composition diagram of lower mantle diamonds-and-inclusions-forming melts demonstrates physico-chemical correlation of variable compositions of the melts with major and minor components of the parental system. Along with this, compositional links between the components set the stage for genetic classification of primary inclusions in lower mantle diamonds. The peritectic breakdown of ferriferous bridgmanite during fractional crystallization of diamond-parental melts opens up possibility for their ultrabasic-basic evolution. The features of the lower mantle diamond-producing systems which have displayed in physico-chemical experiments are in close agreement with the mantle-carbonatite conception of diamond genesis.

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References

  • Akaogi M (2007) Phase transitions of minerals in the transition zone and upper part of the lower mantle. In: Othani E (ed) Advances in high-pressure mineralogy. Geological Society of America Special Paper, vol 421, pp 1–13

    Google Scholar 

  • 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 Geoph 50(12):1221–1233

    Article  Google Scholar 

  • Kaminsky FV (2012) Mineralogy of the lower mantle: a review of “super-deep” mineral inclusions in diamonds. Earth Sci Rev 110:127–147

    Article  Google Scholar 

  • Kaminsky FV (2017) The Earth’s lower mantle. Springer, 331 p

    Book  Google Scholar 

  • Kaminsky FV, Wirth R (2011) Iron carbide inclusions in lower-mantle diamond from Juina, Brazil. Can Mineral 49(2):555–572

    Article  Google Scholar 

  • Kaminsky FV, Wirth R, Schreiber A (2013) Carbonatitic inclusions in deep mantle diamond from Juina, Brazil: new minerals of the carbonate-halide association. Can Mineral 51:669–688

    Article  Google Scholar 

  • Litvin YA (2007) High-pressure mineralogy of diamond genesis. In: Ohtani E (ed) Advances in high-pressure mineralogy. Geological Society of America Special Paper, vol 421, pp 83–103

    Chapter  Google Scholar 

  • Litvin YA (2009) The physicochemical conditions of diamond formation in the mantle matter: experimental studies. Russ Geol Geoph 50:1188–1200

    Article  Google Scholar 

  • Litvin YA (2014) The stishovite paradox in genesis of ultradeep diamonds. Dokl Earth Sci 455(1):274–278

    Article  Google Scholar 

  • Litvin YA (2017) Genesis of diamonds and associated phases. Springer, 137 p

    Chapter  Google Scholar 

  • Litvin YA, Butvina VG (2004) Diamond-forming media in the system eclogite-carbonatite-sulfide-carbon: experiments at 6.0–8.5 GPa. Petrology 12(4):377–382

    Google Scholar 

  • 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 Internat 50(9):726–759

    Article  Google Scholar 

  • Litvin YA, Spivak AV, Kuzyura AV (2016a) Fundamentals of mantle carbonatite concept of diamond genesis. Geochem Internat 54(10):839–857

    Article  Google Scholar 

  • Litvin YA, Spivak AV, Dubrovinsky LS (2016b) Magmatic evolution of the material of the earth’s lower mantle: stishovite paradox and origin of superdeep diamonds (experiments at 24-26 GPa). Geochem Internat 54(11):936–942

    Article  Google Scholar 

  • Litvin YA, Bovkun AV, Androsova NA, Garanin VK (2017) The system ilmenite-carbonatite-carbon in the origin of diamond: correlation between the titanium content and diamond potential of kimberlites. Dokl Earth Sci 473(1):287–291

    Article  Google Scholar 

  • Rhines FN (1956) Phase diagrams in metallurgy: their development and application. McGraw-Hill Book Company Inc, New York, Toronto, London, p 348

    Google Scholar 

  • Shushkanova A, Litvin YA (2005) Phase relations in diamond-forming carbonate-silicate-sulfide systems on melting. Russ Geol Geophys 46(12):1317–1326

    Google Scholar 

  • Spivak A, Solopova N, Dubrovinsky L, Litvin Yu (2015) Melting relatios of multicomponent carbonate MgCO3–FeCO3–CaCO3–Na2CO-system at 11–26 GPa: application to deeper mantle diamonds formation. Phys Chem Miner 42:817–824

    Article  Google Scholar 

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Correspondence to Anna V. Spivak .

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Spivak, A.V., Litvin, Y.A. (2019). Genetic Mineralogy of Lower Mantle Diamonds and Their Inclusions. In: Evolution of Magmatic and Diamond-Forming Systems of the Earth's Lower Mantle. Springer Geology. Springer, Cham. https://doi.org/10.1007/978-3-319-78518-9_6

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