OLIVINE FROM NAMUAIV PIPE AILLIKITE, KOLA ALKALINE PROVINCE: THE PRIMARY MELT EVOLUTION AND RELATION TO KIMBERLITE MAGMATISM
- 作者: Lebedeva N.M.1, Sazonova L.1, Kargin A.V.2,3, Nosova А.А.1, Arzamastsev A.A.4, Shaikhutdinova D.R.4, Yapaskurt V.О.4
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隶属关系:
- Institute of Geology of Ore Deposits, Petrography, Mineralogy and Geochemistry Russian Academy of Sciences
- V.S. Sobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences
- Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry, Russian Academy of Sciences
- Institute of Precambrian Geology and Geochronology RAS
- 期: 卷 523, 编号 2 (2025)
- 栏目: PETROLOGY
- ##submission.dateSubmitted##: 26.04.2025
- ##submission.dateAccepted##: 05.05.2025
- ##submission.datePublished##: 11.06.2025
- URL: https://bakhtiniada.ru/2686-7397/article/view/289365
- ID: 289365
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This study presents petrographic and mineral chemical data for olivine in aillikites from the Namuive pipe intruded into the Khibiny Massif, the Kola Alkaline Carbonatite Province. Two distinct olivine populations are identified: phenocrysts and xenocrysts. The phenocrysts crystallized from the aillikite melt, whereas the xenocrysts were entrained from the mantle substrate. Xenocrysts are characterized by high Mg# (0.89-0.91) and elevated concentrations of Ni and Ti, and are compositionally similar to kimberlitic olivines, but differ from them by significantly higher Ca contents. "Elevated CaO concentrations in olivines from the aillikites of the Namuaiw pipe may reflect differences in the metasomatic processing of the mantle source (carbonate or aqueous fluid) or the intensity of its lherzolitization. The differences in the evolutionary trends of olivines from aillikites and kimberlites are caused by the assimilation of lithospheric material (mainly orthopyroxene) during the ascent of kimberlitic melts.
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作者简介
N. Lebedeva
Institute of Geology of Ore Deposits, Petrography, Mineralogy and Geochemistry Russian Academy of Sciences
编辑信件的主要联系方式.
Email: namil@mail.ru
ORCID iD: 0000-0002-8578-8858
кандидат геолого-минералогических наук, научный сотрудник лаборатории петрографии
俄罗斯联邦Ludmila Sazonova
Email: sazonovalv52@mail.ru
A. Kargin
V.S. Sobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences; Institute of Geology of Ore Deposits, Petrography, Mineralogy, and Geochemistry, Russian Academy of Sciences
Email: kargin-igem@mail.ru
Russian, Novosibirsk; Russian,
Moscow
А. Nosova
Institute of Geology of Ore Deposits, Petrography, Mineralogy and Geochemistry Russian Academy of Sciences
Email: nosova@igem.ru
俄罗斯联邦, Moscow
A. Arzamastsev
Institute of Precambrian Geology and Geochronology RAS
Email: arzamas@ipgg.ru
俄罗斯联邦, St. Petersburg
D. Shaikhutdinova
Email: darina@igem.ru
V. Yapaskurt
Email: vyapaskurt@mail.ru
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