Khokhoy deposit is a new Carlin-type gold-bearing object (Aldan shield)

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To the west of the unique gold-mining Central Aldan ore district at the Khokhoy deposit of Verkhneamginskaya area, gold mineralization has been identified for the first time in terms of regional position, structural, morphological, and mineralogical-geochemical parameters comparable to its global analogue, the Carlin type. The deposit is located on the northern margin of the Precambrian Aldan shield in the deep Amga fault zone at the junction of two large structural units: the Olekminsky granite-greenstone region (Olekminsky craton) and the Aldan granulite-gneiss region (mobile belt). The mineralization is represented by sandy loam-clay-clastic karst formations developed on the tectonized contact of Lower Cambrian carbonate and Lower Jurassic terrigenous sedimentary rocks. Ore-bearing sublongitudinal steeply falling discontinuous faults are accompanied by Cretaceous dikes of sub-alkaline rocks. The friable supergenic formations consist of quartz, muscovite, clay minerals (illite, clinochlore, Fe-clinochlore, kaolinite), lepidocrocite, carbonates, barite, fluorite, goethite, jarosite, and hematite. The primary ores were preserved in the form of fragments/relics of jasperoids – pyrite-adularia-quartz metasomatites formed as a result of silicic-potassic metasomatism of carbonate rocks. Jasperoids carry low-temperature mineralization, represented by fine-grained quartz, chalcedony, adularia, sericite, calcite, barite, fluorite, illite, hollandite, pyrite, minerals of thallium, antimony, arsenic, tellurium and mercury. Geochemical association of elements – Au-As-Sb-Tl-Te-Hg. Finely dispersed native gold of primary ores with a size of no more than 0.005 mm is found in oxidized pyrite enriched with Sb, As and Hg, as well as in association with minerals of thallium and mercury. In friable karst formations, the residual gold was released and enlarged to 0.1–0.5 mm. High-grade supergenic gold is characterized by a spongy structure and an admixture of Hg. A new mineral, thallium tellurate Tl2TeO6 – amgaite, has been discovered in the ores. The substantiation of the highly productive Carlin type of gold mineralization of the Khokhoy deposit will serve as the basis for the revision and revaluation of the Kuranakh type in the area of the Aldan shield.

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Sobre autores

L. Kondratieva

Diamond and Precious Metals Geology Institute, Siberian Branch, Russian Academy of Sciences

Autor responsável pela correspondência
Email: lkon12@yandex.ru
Rússia, Lenin Avenue, 39, Yakutsk, 677981

G. Anisimova

Diamond and Precious Metals Geology Institute, Siberian Branch, Russian Academy of Sciences

Email: gsanisimova1952@mail.ru
Rússia, Lenin Avenue, 39, Yakutsk, 677981

E. Sokolov

Yakutskgeologiya Joint Stock Company

Email: geol63@mail.ru
Rússia, Kalvitsa St., 24, Yakutsk, 677000

V. Kardashevskaia

Diamond and Precious Metals Geology Institute, Siberian Branch, Russian Academy of Science

Email: kardashevskaya92@mail.ru
Rússia, Lenin Avenue, 39, Yakutsk, 677981

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1. JATS XML
2. Fig. 1. Scheme of tectonic zoning (after Goroshko et al., 2010, with modifications). Aldan granulite-gneiss region: 1 - Early Archean blocks, 2 - Late Archean graben-synclinor structures; 3 - Vendian-Cambrian platform cover; 4 - South Aldan system of Mesozoic continental coal-bearing basins and grabens: K - Kuranakh, Ch - Chulman; 5 - Olekminskaya granite-greenstone region; 6 - deep faults (letters in circles): A - Amginsky, O - Olongrinsky, R - Russky, E - Elkonsky, T - Tyrkandinsky, Tm - Timpton; 7 - other faults; 8 - ore regions: CA - Central Aldan, VA - Verkhneamginsky; 9 – Khokhoy ore field. The inset shows the location of the Khokhoy ore field.

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3. Fig. 2. Geological map of the Khokhoy ore field: 1 - Quaternary deposits; 2 - subalkaline dikes; 3 - Lebedinsky monzonite-syenite plutonic complex; 4 - Yukhtinskaya suite, inequigranular, oligomictic sandstones, lenses and interlayers of gravelites, conglomerates, siltstones; 5 - Lower Cambrian deposits of the Ungelinskaya, Tumuldurskaya and Pestrotsvetnaya suites, dolomites with interlayers of marls and marly dolomites, 6 - Vendian-Lower Cambrian deposits of the Ust-Yudomskaya suite, bituminous dolomites with thin interlayers of marly dolomites; 7 - faults: a - main, b - secondary; 8 - karst development zones; 9 - Khokhoy deposit.

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4. Fig. 3. Structure of karst cavities: 1 – clays; 2 – gravel, crushed rock; 3 – blocks; 4 – dolomites; 5 – marly dolomites; 6 – sandstones; 7 – zones of intense fracturing; 8 – mineralized zones of crushing and brecciation; 9 – karst.

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5. Fig. 4. General view of ore-bearing karst

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6. Fig. 5. Jasperoids of the Khokhoy ore field: a – limonitized K-feldspar-quartz metasomatites with morion brushes in caverns and fine dissemination of goethite over pyrite; b – the same, polished; c–d – ore breccias; d – K-feldspar-quartz metasomatites with phenocrysts of coarse-crystalline hematite and disseminated fine-grained goethite.

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7. Fig. 6. Thallium mineralization: a – weissbergite grains in quartz; b – avicenite; c – association of amgaite, avicenite and unidentified thallium antimonate; g – association of avicenite and native gold; d – yankovicite; e – intergrowth of yankovicite and weissbergite. Wsb – weissbergite, Av – avicenite, Amgt – amgaite, Au – native gold, Un – unidentified thallium antimonate, Jnk – yankovicite, Q – quartz.

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8. Fig. 7. Forms of amgaite allocation and its association with other minerals: a–b – zonal aggregates of amgaite; c – rhythmically zonal individuals of amgaite; g – veinlets of amgaite in unidentified thallium antimonate; d – rims of amgaite around quartz, e – close association of native gold and amgaite. Amgt – amgaite, Au – native gold, Un – unidentified thallium antimonate, Q – quartz.

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9. Fig. 8. Mercury mineralization: a – coloradoite; b – cinnabar veinlets in quartz; c – cinnabar veinlets and associated micron-sized native gold in goethite. Col – coloradoite, Cnb – cinnabar, Au – native gold, Gth – goethite, Adl – adularia, Q – quartz.

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10. Fig. 9. Micron native gold of primary ores

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11. Fig. 10. Hypergene gold in karst deposits: a – mustard microporous; b – spongy; c – stem dendrites; g – branch-shaped; d – massive; e – crystalline.

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