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Paragenetic relations of diamond with silicate and carbonate minerals

in the system carbonatite-diamond (experiment at 8.5 GPa)

Spivak A.V., Litvin J.A.

Institute of Experimental Mineralogy of RAS, 142432 Chernogolovka, the Moscow region

e-mail: spivak@iem.ac.ru

 

Experimental researches of melting phase relations of diamond and syngenetic minerals in multicomponent system natural carbonatite - diamond were carried out at pressure 8.5 GPa and temperatures 1300 - 1800оС (PT-conditions of thermodynamic stability of diamond). Natural carbonatite of the Chagatai complex (Uzbekistan) gets a mineralization of high-Ca eclogite – grospydites under these conditions.  Melting phase diagram of the system was studied and “syngenesis diagram” constructed. The curve of solubility of diamond in completely miscible carbonate-silicate melts (values of solubility - within 15 - 18 wt. % carbon) is of great importance in the syngenesis diagram. The curve of diamond solubility divides the phase diagram into two fields: (1) phase relations with participation nonsaturated to diamond melts-solutions of carbon, liquidus phase is  garnet (area of diamond dissolution) and (2) phase relations with participation of saturated to diamond melts-solutions, liquidus phase is diamond (area of diamond crystallization). Diamond bearing phase associations diamond + garnet + melt, diamond + garnet + clinopyroxene + melts, diamond + garnet + clinopyroxene + carbonate + melts and as a result subsolidus association diamond + garnet + clinopyroxene + carbonate are formed from carbonate-silicate melts at temperature lowering in the field of diamond crystallization.

 

 

The experimental data testifies  the paragenetic nature of silicate and carbonate minerals, crystallized with diamond. Physico-chemical mechanism of diamond formation in carbonate-silicate melts is demonstrated. Analysis of physical and chemical behavior of natural diamond-forming magma chamber is given on the basis of the syngenesis phase diagram.

This study was financially supported by RFBR grant 08-05-00110, 10-05-00110 and grants of the president RF МК-4754.2009.5, МК-4735.2009.5.