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Lamproites of Kayla pipe and their mantle xenocrysts, SE Aldan shield, Russia: Geochemistry and petrology

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Abstract

Origin of abundant alkaline and related lamproite massifs and dykes in Aldan shield have no explanation and the geochemistry of rocks and their xenocrysts is used for the explanation. Bulk-rock geochemistry, mineral chemistry data of the Kayla lamproites of Russia and mineral chemical data (trace and rare elements) of the mantle xenocrysts found in these lamproites was studied using ICP MS and electron microprobe analyses (EPMA). The trace element spectrum of Kayla tuffs and breccias show the similarity with the olivine lamproites and belong to the orogenic type according to Th–U–Nb systematics. Primitive mantle normalized trace element (TRE) spider diagrams show right-leaning patterns with the peaks in large ion lithophile elements Sr, Pb, U, and troughs in Ta, Nb suggesting melting of original peridotites mixed with the ancient EMI (according to Nd, Sr isotopes) source probably belonging to eclogites or lower crust. The age of the emplacement is 132–134 Ma, similar to the Chompolo lamprophyres and many other alkaline Aldan complexes. Thermo-barometric estimation from Cr-diopsides and chromites xenocrysts suggest the origin from the spinel-garnet transition in the lithospheric mantle region. The P–T estimates derived from low-Cr-clinopyroxene xenocrysts, and related to lamproites show a high heat flow of 90 mW/m2 due to interaction with the plume-related magma. The Cr-diopsides and chromites give 45 mW/m2 geotherm similar to regional heat flow. The chondrite normalized rare earth element (REE) pattern for chrome-diopsides is steeper, compared to the low-chrome varieties. Primitive mantle normalized spidergram of Cr-diopsides displays peaks for Sr, U, and Th, and deep troughs of Nd, Nb, Ta. REE. The trace element spider diagrams of both types of xenocrysts show that they were equilibrated with the lamproitic melts and reconstructed parental melts of low-Cr-clinopyroxene coincides with the lamproite spectrums.

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Acknowledgements

The work was supported by the Ministry of Science and Higher Education of the Russian Federation N121031700315-2. RBRF grants 19-05-00788a, 18-05-00073a. Government tasks for Institute of Geochemistry SB RAS and Institute of Geology and Mineralogy SB RAS and the governmental assignment in terms of Project IX. 129.1.4.

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Authors and Affiliations

  1. Vinogradov Institute of Geochemistry SB RAS, Irkutsk, 664 033, Russia

    N V Vladykin & I A Sotnikova

  2. V.S. Sobolev Institute of Geology and Mineralogy SB RAS, Novosibirsk, 630 090, Russia

    I V Ashchepkov

  3. Nikolaev Institute of Inorganic Chemistry SB RAS, Novosibirsk, 630 090, Russia

    N S Medvedev

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  1. N V Vladykin
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Contributions

Vladykin Nikolai V sampled Kyala lamproite, prepared KIM concentrates and fractions for analyses, studied and described geology and samples and made their petrography and bulk rock major element and trace element analyses and described isotopic data. Ashchepkov Igor V performed the microprobe analyses, interpreted the data, wrote the manuscript; Sotnikova Irina V made petrographic and geological descriptions and did the field work. Medvedev Nkolai S made LA-ICP-MS analyses.

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Correspondence to I V Ashchepkov.

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Communicated by N V Chalapathi Rao

Supplementary material pertaining to this article is available on the Journal of Earth System Science website (http://www.ias.ac.in/Journals/Journal_of_Earth_System_Science).

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Vladykin, N.V., Ashchepkov, I.V., Sotnikova, I.A. et al. Lamproites of Kayla pipe and their mantle xenocrysts, SE Aldan shield, Russia: Geochemistry and petrology. J Earth Syst Sci 131, 81 (2022). https://doi.org/10.1007/s12040-022-01814-3

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