Victor M. Kvasnytsya, UNUSUAL INCLUSIONS AND GENESIS OF MICRODIAMONDS FROM THE ZELENYI YAR NEOGENE PLACER (THE UKRAINIAN SHIELD): A TEM STUDY

https://doi.org/10.15407/mineraljournal.47.02.003

UDC 549.211

UNUSUAL INCLUSIONS AND GENESIS OF MICRODIAMONDS

FROM THE ZELENYI YAR NEOGENE PLACER (THE UKRAINIAN SHIELD): A TEM STUDY

Victor M. Kvasnytsya 1, DrSc (Mineralogy and Crystallography), Prof., Head of Department

orcid: 0000-0002-3692-7153

Richard Wirth 2, PhD, Senior Research Scientist

E-mail: wirth@gfz-potsdam.de; Scopus ID: 7102907278

Oleksii A. Vyshnevskyi 1, PhD (Mineralogy and Petrology), Leading Researcher

E-mail: vyshnevskyy@i.ua; orcid: 0000-0002-7206-2185

Anja Schreiber 2, Technician, Specialist

E-mail: schreib@gfz-potsdam.de; Scopus ID: 34979283500

Viacheslav M. Pavliuk 1, Junior Research Fellow

E-mail: v-pavlyuk@ukr.net; orcid: 0000-0002-7035-8505

1 M.P. Semenenko Institute of Geochemistry, Mineralogy and Ore Formation of the NAS of Ukraine

34, Acad. Palladin Ave., Kyiv, Ukraine, 03142

2 GFZ Helmholtz Center for Geosciences

Telegrafenberg, Potsdam, Germany, 14473

Language: English

Mineralogical journal 2025, 47 (2): 03-19

Abstract: Sixteen diamond microcrystals 0.25-0.5 mm in size from the Neogene placer of Zelenyi Yar on the Ukrainian Shield have been studied using TEM. The investigated diamonds have different morphologies such as: octahedron (1), octahedron fragments (5), octahedroid (1), octahedron-rhombic dodecahedron (1), cube (1), cuboid (3), cubooctahedron (1), cubo-octahedron-rhombic dodecahedron (2) and fragment (1). 21 electron transparent TEM foils with the dimensions 15 × 10 × 0.15 μm were prepared from the crystals and analyzed. Two groups of mantle-derived diamonds were recognized based on solid inclusions and structural defects. Group 1: two crystals with nano-inclusions typical for diamonds from ophiolites; group 2: 12 crystals with multiphase inclusions and structural defects typical for diamonds from kimberlites, lamproites and lamprophyres. One diamond (cuboid) was found to be free of inclusions as well as structural defects. One crystal was identified as an impact diamond. The first group comprises a cubo-octahedron and a fragmented octahedron. These diamonds host unusual Mn-rich inclusions such as tephroite, MnNi alloys with minor Si content, MnNiO3, Mn5C2, rhodonite Mn5Si5O15 and amorphous silica. The MnNiO3 inclusions are associated with amorphous silica and chlorine-rich amorphous quench phases. Most crystals of the second group are characterized by curved dislocations; carbon platelets are found in several crystals and nitrogen platelets (oriented aggregates of nitrogen atoms) in a single crystal. Solid inclusions in these diamonds are: dolomite, ilmenite, magnetite, apatite, phlogopite, chlorite, forsterite and enstatite. These inclusions represents the eclogitic (2 diamonds), peridotitic (1) and websteritic (1) assemblages in mantle-derived diamonds from kimberlites.

Keywords: diamond, inclusions,·microstructure, genesis, placer deposits, Ukrainian Shield.

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