Geological position and features of the composition, structure and genesis of gold ore (with bismuth mineralization) deposits of Sikhote-Alin

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Abstract

A group of gold deposits with bismuth mineralization, potentially promising for industrial gold mineralization within the southern and western Sikhote-Alin, is considered. Ore bodies are represented by veins, stockworks, and ore zones. The ores are characterized by a close association of early-generation native gold with Ni, Co sulfoarsenides and bismuth sulfotellurides and tellurides, and late-generation native gold with sulfosalts of Pb-Bi, Pb-Bi-S, Pb-Cu-Sb composition. In the studied deposits, a significant variation in the size of native gold grains was revealed – from coarse and medium to dusty. Native gold of the early generation is characterized by a fineness of 775–900‰, rarely 990‰, and in the late generation – 600–850‰. Geological and mineralogical-geochemical data indicate a genetic connection in one case (Bolotistoe deposit) with bodies of Eocene dacites and granodiorites, as well as with an intrusion of Eocene gabbroids and monzonitoids. In other cases, deposits (Krinichnoye, Malinovskoye, Namovskoye and Pasechnoye) are characterized by a genetic connection with Early-Late Cretaceous granitoid magmatism.

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Anna A. Grebennikova

Far East Geological Institute, FEB RAS

Author for correspondence.
Email: anylotina@mail.ru
ORCID iD: 0000-0002-3651-8050

Candidate of Sciences in Geology and Mineralogy, Senior Researcher

Russian Federation, Vladivostok

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Supplementary files

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2. Fig. 1. Sikhote-Alin terranes [20] and the location of gold ore objects with gold-bismuth mineralization

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3. Fig. 2. Geological scheme of the Malinovskoye deposit (Belyansky G.S. et al., 2013, see also [12])

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4. Fig. 3. Schematic geological map of the Namovskoye deposit, based on materials by G.S. Belyansky (2012), V.A. Mikhailov (1998), K.N. Dobroshevsky (2012)

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5. Fig. 4. Schematic geological map of the Pasechnoye deposit (based on materials by V.V. Uglov, 1981)

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6. Fig. 5. Schematic geological map of the Krinichny gold-bearing cluster [32]

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7. Ris. 6. Skhematicheskaya geologicheskaya karta mestorozhdeniya Bolotistoye (Dymovich, 1981): 1 – bazal'ty kizinskoy svity, miotsen; 2 – andezity i andezito-bazal'ty kuznetsovskoy svity, eotsen; 3 – shchebnisto-glinistyye otlozheniya erozionno-tektonicheskogo vreza, paleogen; 4 – peschaniki, rezhe alevrolity, argillity, mel; 5–8 – eotsenovyy magmaticheskiy kompleks: 5 – datsity, 6 – intruziya slozhnogo sostava (gabbro, gabbro-diabazy, diabazy, gabbro-diority, diority, kvartsevyye diority), 7 – silly gabbro-dioritovykh porfiritov, granodioritov, 8 – dayki osnovnogo i srednego sostava; 9 – razryvnyye narusheniya; 10 – kontur rudnoy zony Ещё 609 / 5 000 Fig. 6. Schematic geological map of the Bolotistoye deposit (Dymovich, 1981): 1 - basalts of the Kizinskaya suite, Miocene; 2 - andesites and andesite-basalts of the Kuznetsovskaya suite, Eocene; 3 - rubble-clayey deposits of erosion-tectonic incision, Paleogene; 4 - sandstones, less often siltstones, argillites, chalk; 5-8 - Eocene igneous complex: 5 - dacites, 6 - intrusion of complex composition (gabbro, gabbro-diabase, diabase, gabbro-diorite, diorite, quartz diorite), 7 - sills of gabbro-diorite porphyrites, granodiorites, 8 - dikes of basic and intermediate composition; 9 - faults; 10 - contour of the ore zone

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