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MINERAL COMPOSITION AND PT PARAMETERS OF CRYSTALLIZATION OF MANTLE ROCKS UNDER KIMBERLITE FIELDS OF THE ANABAR REGION

https://doi.org/10.5800/GT-2022-13-4-0665

Abstract

The composition of barophilic minerals from mantle xenoliths and Cpx from concentrates of the Kuranakh, Luchakan, Dyuken, and Ary-Mastakh fields of the Anabar region has been studied. Under these fields, the lithospheric mantle compositions vary significantly. The PT parameters of crystallization were calculated using the composition of clinopyroxenes from xenoliths and heavy fraction of kimberlites. The lithospheric mantle rocks under the northern fields have higher values of Mg# of minerals and calculated mantle geotherm (35–48 mW/m2) compared to the parameters for the southern diamond fields. The pipes from the southwestern part of the Ary-Mastakh field are promising for the diamond potential, presenting Grt-bearing lherzolites and harzburgites with a high content of Cr2O3 (to 8.5 wt. %).

About the Authors

S. I. Kostrovitsky
Vinogradov Institute of Geochemistry, Siberian Branch of the Russian Academy of Sciences; Institute of the Earth’s Crust, Siberian Branch of the Russian Academy of Sciences
Russian Federation

1а Favorsky St, Irkutsk 664033

128 Lermontov St, Irkutsk 664033



T. V. Kalashnikova
Vinogradov Institute of Geochemistry, Siberian Branch of the Russian Academy of Sciences
Russian Federation

1а Favorsky St, Irkutsk 664033



I. V. Ashchepkov
Vinogradov Institute of Geochemistry, Siberian Branch of the Russian Academy of Sciences; Sobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences
Russian Federation

1а Favorsky St, Irkutsk 664033

3 Academician Koptyug Ave, Novosibirsk 630090



References

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Review

For citations:


Kostrovitsky S.I., Kalashnikova T.V., Ashchepkov I.V. MINERAL COMPOSITION AND PT PARAMETERS OF CRYSTALLIZATION OF MANTLE ROCKS UNDER KIMBERLITE FIELDS OF THE ANABAR REGION. Geodynamics & Tectonophysics. 2022;13(4):0665. (In Russ.) https://doi.org/10.5800/GT-2022-13-4-0665

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