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Mineral Phase Paragenesis in Explosive Ejecta Discharged by Recent Eruptions in Kamchatka and the Kuril Islands. Part 1. Diamonds, Carbonaceous Phases, and Condensed Organoids

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Abstract

Ejecta of recent volcanic eruptions were found to contain a carbonaceous mineral phase paragenesis of explosive atmospheric electrogenic origin. The paragenesis involves diamonds of octahedral habitus with non-aggregated nitrogen defects (without signs of mantle burning), disordered graphite, shungite-like bitumen (kerite–anthraxolite), carbonaceous globules (clustered allotropes of dicarbon composition), metal carbon nano-microcomposites resulting from thermal impact decomposition of metal organic compounds, and abiogenic organic compounds. The carbonaceous paragenesis identified here is considered as a unique natural phenomenon that indicates the existence of a global process that favor endogenous carbonization of the Earth’s crust during crust–mantle interactions.

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ACKNOWLEDGMENTS

We express our deep gratitude for the cooperation and great help rendered in this study to candidates of geologic–mineralogical sciences D.V. Kiseleva, S.N. Shanina, B.A. Makeev, and V.A. Rashidov, as well as to researchers V.N. Filippov, A.S. Shuisky, V.M. Chubarov, and K.V. Tarasov.

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Correspondence to V. I. Silaev or G. A. Karpov.

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Translated by A. Petrosyan

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Silaev, V.I., Karpov, G.A., Anikin, L.P. et al. Mineral Phase Paragenesis in Explosive Ejecta Discharged by Recent Eruptions in Kamchatka and the Kuril Islands. Part 1. Diamonds, Carbonaceous Phases, and Condensed Organoids. J. Volcanolog. Seismol. 13, 323–334 (2019). https://doi.org/10.1134/S0742046319050051

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