Rare elements in the lower-middle miocene coals of the southwestern margin of the zeya–bureya sedimentary basin (amur region, far east)

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Abstract

The conditions of formation and metalliferous content of Lower-Middle Miocene coal deposits on the southwestern margin of the Zeya–Bureya basin are considered. Their formation took place within the Priamursky depression, bounded on the west by the Greater Khingan and on the east by the Kostyukovo–Blagoveschensk uplift system. For the first time, mineralogical composition, geochemistry of coal, and their combustion products were studied in detail. Uneven accumulation of REY (REE + Y), rare metals, non-ferrous metals, and noble metals was shown, which is largely related to the variety of the composition of feeding provinces that border the depression. The genetic types of enrichment of REE were identified, and the prospects of their use as raw materials for extraction during coal burning were determined.

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About the authors

A. P. Sorokin

Institute of Geology and Nature Management, Far East Branch, Russian Academy of Sciences

Author for correspondence.
Email: sorokinap@ignm.ru
Russian Federation, Blagoveshchensk

S. V. Dugin

Institute of Geology and Nature Management, Far East Branch, Russian Academy of Sciences

Email: duservad@gmail.com
Russian Federation, Blagoveshchensk

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2. Fig. 1. Structural and metallogenic scheme of the junction zone of the Zeya-Bureya sedimentary basin and the Greater Khingan: 1 - boundary of the Zeya-Bureya sedimentary basin; 2 - structures framing the basin: the Greater Khingan (I) with the Amur volcanic belt (II), the Amur-Mamyn ledge (III), the Blagoveshchensk uplift (IV); 3 - internal structures (positive): Kostyukovsky swell (V), Petropavlovsk uplift (VI); (negative): Tarakonsky (VII), Aktaisky (VIII), Kamensko-Selitkansky (IX), Korsakovsky (X), Belorechensky (XI), Spasovsky (XII), Sychevsky (XIII), Komissarovsky (XIV), Sergeevsky (XV), Dmitrievsky (XVI) troughs; 4 — faults: Priamursky (PA), East Amursky (VA), Nenjiangsky (NC), Verkhneselemdzhinsky (VS); 5 — coal-bearing areas: J — Dzhatvinskaya, Sm — Semenovskaya, Ks — Klimoutsevsko-Sergeevskaya, Gl — Golubinskaya; 6 — Sergeevskoye brown coal deposit; 7 — ore occurrences: Tarakonskoye (Tr), Korsakovskoye (Kr), Mostovskoye (Ms); 8 — placer halos; 9 — geochemical dispersion flows; 10 — single placers with increased mineral content; 11 — movement of terrigenous material, including ore material, from feeding provinces. The border between the Russian Federation and the PRC runs along the Amur River.

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3. Fig. 2. Ore minerals of the heavy fraction of Sergeevskiye coals: lead (a), grains of lead-zinc-iron composition (b), platinum (c, d), gold (d).

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4. Fig. 3. Distribution of standardized REY contents in PSU and in ashed coal: O-US(+10) – ashed coal; ШС – slag; ЗС-1, ЗС-2, ЗС-3 – fly ash; ШлС – sludge; ВТС – sediment.

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5. Fig. 4. Distribution of rare element and metal contents in the PSU on the southeastern outskirts of the Sergeevskoye deposit.

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