Abstract
In the products of modern volcanic identified carbonaceous mineral phase paragenes explosive-atmoelektrogenese origin comprising diamond cuboctahedral habitus with non-aggregated nitrogen defects (no signs mantle annealing), disordered graphite, shungito shaped asphalts (kerite-anthraxolite), carbon globules – cluster allotrope diuglerod composition, metallo-carbon nanomicrocomposites – a product of the shock-thermal decomposition of organometallic compounds and a biogenic organic compounds. The identified carbon paragenes is considered as a unique natural phenomenon indicating the existence of a global process of endogenous carbonization of the Earth's crust during the course of the crust-mantle interactions.
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