Japan Geoscience Union Meeting 2018

Presentation information

[EE] Oral

S (Solid Earth Sciences) » S-IT Science of the Earth's Interior & Tectonophysics

[S-IT25] Deep Carbon: Diamond formation and carbon speciation in Earth and planetary processes

Tue. May 22, 2018 10:45 AM - 12:15 PM A11 (Tokyo Bay Makuhari Hall)

convener:Eiji Ohtani(Department of Earth and Planetary Materials Science, Graduate School of Science, Tohoku University), Konstantin Litasov(V.S. Sobolev Institute of Geology and Mineralogy SB RAS), Hiroyuki Kagi(東京大学大学院理学系研究科附属地殻化学実験施設, 共同), Craig E Manning (University of California Los Angeles), Chairperson:Kagi Hiroyuki(University of Tokyo), Ohtani Eiji(Tohoku University)

11:15 AM - 11:30 AM

[SIT25-03] Cuboctahedral diamonds from volcanic rocks of Kamchatka: Contamination or growth in unusual environments?

*Konstantin Litasov1, Sergey Voropaev2, Vyacheslav Sevastyanov2, Hiroyuki Kagi3, Hiroaki Ohfuji4, Hidemi Ishibashi5, Erik Galimov2 (1.V.S. Sobolev Institute of Geology and Mineralogy SB RAS, Novosibirsk, Russia, 2.Vernadsky Institute of Geochemistry and Analytical Chemistry RAS, Moscow, Russia, 3.Geochemical Research Center, University of Tokyo, Tokyo, Japan, 4.Geodynamic Research Center, Ehime University, Matsuyama, Japan, 5.Department of Geosciences, Faculty of Science, Shizuoka University, Shizuoka, Japan)

Keywords:cuboctahedral diamond, alkaline basalt, cavitation, high-pressure

Enigmatic appearance of cuboctahedral diamonds with morphology and infrared characteristics similar with synthetic diamonds grown from typical metal solvent, in natural ophiolitic and volcanic rocks (e.g., Howarth et al., 2015) requires more attention.
We studied several diamond crystals from Tolbachik volcano lava flow (Karpov et al., 2014) and from Ozernovskoe gold deposits, which is located not far away of Tolbachik, using transmission electron microscopy and synchrotron X-ray fluorescence. In the TEM films prepared using FIB technique we find only one metallic inclusions in Tolbachik diamonds. It contains Mn and Ni with minor Si. Ozernovskoe diamonds contain many inclusions. Their compositions correspond to Mn-Ni metals and Si-Ca-Mn oxides. X-ray fluorescence spectra, measured in the range of transitional metals with incident X-ray of 10 keV, confirm these compositions and also indicate presence of Fe-Ni and Fe-Ni-Mn inclusions with Cr, Ti, Cu, and Zn impurities. Bulk diamonds contain significant amounts of Mn,Ni and Fe in the range of 5-40 ppm. These values are much lower than those determined by LA-ICP-MS (Howell et al., 2015) for similar diamonds from Tibet ophiolites.FTIR spectra of Tolbachik diamonds indicate presence of minor carbonate and silicate inclusions.
Ozernovskoe diamonds are embedded to hydrothermally altered WC beads. This may clearly indicate contamination of rocks by drilling instruments. However, they are also extremely interesting for study as we can get an example of rapid alteration of WC during hydrothermal or weathering activity for short period of 30-40 years. Since we had only two crystals at present we cannot exclude natural origin for Ozernovskoe diamonds, because undoubtedly natural WC even with Co impurities (the composition, which is exactly as in industrial tools) was observed in hydrothermal deposits from Tolbachik eruption in 1975 and earlier (e.g., Glavatskih, 1990).
Mn-Ni (+Fe) solvent was used to produce industrial synthetic diamonds in USSR, thus the immediate conclusions is that Kamchatka cuboctahedral diamonds are contamination from drilling tools or other hard instruments. However, in case of Tolbachik this hypothesis is hardly possible, because diamonds were recovered from fresh lava flow of 2012-2013 eruption. Wide occurrence of similar diamonds in other rocks, including ophiolite and garnet peridotite may require their natural origin. One of the possible hypotheses is rapid growth in cavitation bubbles, where huge overpressure compared to detonation process is generated along with ultrahigh temperatures. However, detailed characterization of cavitation diamonds is yet to be reported. The study should be continued on larger amount of samples from different localities.
The work is supported by RFBR grant No 17-05-00935.

Glavatskih, S.F. (1990) Transact. (Doklady) USSR Acad. Sci., 313: 433-437.
Howell, D., Griffin, W.L., Yang, J., et al. (2015) Earth Planet. Sci. Lett., 430: 284-295.
Karpov, G.A., Silaev, V.I., Anikin, L.P. et al.(2014) J. Volcanol. Seismol., 8: 323-339.