“…Interest in shungite carbon increased after the first discovery of fullerenes of geological origin in it [ 19 ]. In addition to the shungite rocks of Karelia, significant occurrences with well-characterized structure and properties of D sp 2 C (referred to in the geological and mineralogical literature as anthraxolites and pyrobitumen) are located in Bakyrchik (Kyzyl fault zone, Kazakhstan) [ 20 , 21 , 22 ], Mitov (Bohemian massif, Czech Republic) [ 23 , 24 ], Novaya Zemlya island (Russia) [ 25 ], Sichuan province (China) [ 26 ], the Sudbury Astroblem (Canada) [ 27 , 28 , 29 ], the Franceville Sedimentary Basin (Gabon) [ 30 , 31 ], the Michigan Formation (USA) [ 32 , 33 ], and many others.…”