Фенокристаллы флогопита с включениями хромшпинелидов из неалмазоносных кимберлитов (на примере АН-195 Западно-Укукитского поля) = Phlogopite phenocrystals with inclusions of chrome spinelides from non-diamond-bearing kimberlites: the case of an-195 body of the west ukukit field
Статья в журнале
Русский
549.02(571.56-15)
10.25587/2587-8751-2023-4-12-19
флогопит; шпинелид; мантийные ксенолиты; эклогиты; MARID-серия; мантийный метасоматоз; кимберлит; фенокрист; ксенокрист; phlogopite; spinelide; mantle xenoliths; eclogites; MARID series; mantle metasomatosis; kimberlite; phenocryst; xenocryst
Геология
The article presents the results of a microprobe study of the composition of phlogopite macrocrystals with inclusions of chrome spinelides from An-195 kimberlite body of the West Ukukit eld, Yakut kimber liteprovince. The purposeofthis study was toestablis hthegenesi sofsuchphlogopites: whe ther they are representatives of deep mantle matter or their formation is directly related to the formation of kimberlites composing An-195. It was found that the inclusions of chrome spinelides are con ned only to chromic non-zonal phlogopites or to chromic sites of zonal macrocrystals (Cr O 0.75-1.55 wt. %, TiO 2.67-3.84 wt. %, Mg# 83-88). Based on a 2 3 2 comparative analysis of the studied phlogopites and chromespinelides with the composition of analogues from the parageneses of these minerals in various mantle xenoliths of ultrabasic rocks, eclogites and rocks of the MARID series, it was concluded that these phlogopites most likely represent a phenocrystal association of kimberlite minerals. They clearly di er from phlogopites of the MARID series rocks with equal Mg# and TiO in higher 2 Al O contents; from phlogopites of ultrabasic mantle rocks xenoliths - generally with lower magnesia content. Phlogopites from eclogites have a generally higher Cr O content. Inclusions of high-chromium spinelides in 233+phlogopite (Cr O 44-50 wt. %, TiO 3-5.5 wt. %, Fe < 0.35 f.e.) correspond in composition to spinelides from 232cataclysmic dunites and are products of their recrystallization under the in uence of high-temperature mantle uid. 3+Inclusions of less chromic spinelides (Cr O 30-44 wt. %, TiO 4-7.5 wt. %, Fe > 0.35 fe) probably crystallized 232simultaneously with phlogopite macrocrystals and were captured by them during long-term co-growth.
Бабушкина, С. А. Фенокристаллы флогопита с включениями хромшпинелидов из неалмазоносных кимберлитов (на примере АН-195 Западно-Укукитского поля) / С. А. Бабушкина ; Институт геологии алмаза и благородных металлов // Вестник Северо-Восточного федерального университета им. М. К. Аммосова. Серия: Науки о земле. - 2023. - N 4 (32). - C. 12-19. - DOI: 10.25587/2587-8751-2023-4-12-19
DOI: 10.25587/2587-8751-2023-4-12-19
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