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ИГЕМ

ИНОЗ. ИГ РАН. МНИЦ ГП Бишкек. ИПИ. GC RAS. ИГЕМ. ИППИ. ВИНИТИ. МСЦ РАН. ГГМ. ГЕОХИ. ГИН. ИГГД. МИДПАН. Interrelation portal the GC RAS with other participants of project of “Electronic Earth” of the Russian Academe of Sciences. Kimberlites. and. Carbonatites.

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  1. ИНОЗ ИГ РАН МНИЦ ГП Бишкек ИПИ GC RAS ИГЕМ ИППИ ВИНИТИ МСЦ РАН ГГМ ГЕОХИ ГИН ИГГД МИДПАН Interrelation portal the GC RAS with other participants of project of “Electronic Earth” of the Russian Academe of Sciences

  2. Kimberlites and Carbonatites are the most deep magmatic rocks in the crust. They have enormous mineragenic potential ore Nb, Ta, TR, P, Fe, Ti, Zr Diamonds

  3. Scheme of interaction the database with GIS-technology Carbonatites Kimberlites

  4. Example of reflection of the multifactorial information about kimberlite massif "Маdjgavan"

  5. Carbonatites & kimberlitesdisposition from axis of rift zones. Carbonatites Kimberlites axis of rift 400 km from rift

  6. Evolution of carbonatite magmatism.Leading epochs of their formationare shown

  7. Mineragenic Evolution(Nb → TR → P → Fe) age age

  8. Age evolution of content of diamonds age

  9. 21 Tempo of kimberlite magmatism & formation of diamonds 11 5

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