The Devonian Kalarskoe Epithermal Occurrence of the Kaburchak Au-Ag Cluster in the Altai-Sayan Folded Area, Russia: Geological Setting; Mineralogical, Geochemical, and Geochronological Features
<p>Schematic map showing the distribution of epithermal Au-Ag mineralization in the western segment of the ASFA (Figure 2).</p> "> Figure 2
<p>Schematic map showing geological features and Au-bearing potential of the Kaburchak cluster (Figure 3).</p> "> Figure 3
<p>Schematic geological prospecting map showing the Au-Ag Kalarskoe occurrence.</p> "> Figure 4
<p>(<b>a</b>) The mineral composition and zoning of altered wall rocks of the Kalarskoe occurrence, according to Ref. [<a href="#B9-minerals-14-00708" class="html-bibr">9</a>] and new data. Samples from drill holes C1, C2, 7k, and S-17; (A, B, G—massive pyrite-arsenopyrite body; C—superimposed argillic alteration on propylite with disseminated pyrite and its veinlets; D, E, H, I—argillic metasomatites, with sulfide and later, carbonate (Ca, Mn) veinlets; F—relict porphyry texture of argillic-altered rock; J—argillic metasomatite with disseminated pyrite; K—argillic-altered rock with schistose structure. (<b>b</b>) Simplified geological cross-section of the Kalarskoe occurrence (all volcanic rocks were propylitically altered) (modified after Ref. [<a href="#B10-minerals-14-00708" class="html-bibr">10</a>]) (1) propylitic alteration; (2) hypergene zone; (3) argillic alteration with disseminated pyrite and its veinlets; (4) pyrite-arsenopyrite veins; (5) quaternary sediment; (6) number of drill holes. Letters corresponds to the sample numbers from (<b>a</b>).</p> "> Figure 5
<p>Photomicrograph of a massive pyrite-arsonopyrite assemblage at a 33.3 m depth from drill hole 7k. Some of the pyrite grains in this sample were used for (U-Th)-He dating. Py—pyrite; Apy—arsenopyrite.</p> "> Figure 6
<p>Changes in the content of elements with depth in the mineralized rocks and metasomatites from drill hole C2, based on the results of ICP-MS analysis. The vertical axis is the content of elements (ppm) on the logarithmic scale. The horizontal axis is the sampling depth.</p> "> Figure 7
<p>Images of polished sections (updated based on the work of Leibham, 2022 [<a href="#B9-minerals-14-00708" class="html-bibr">9</a>]). (<b>A</b>)—disseminated pyrite and arsenopyrite in the argillic-altered rock; (<b>B</b>,<b>C</b>)—massive pyrite-arsenopyrite vein; (<b>D</b>)—pyrrhotite and chalcopyrite in the propylite; (<b>E</b>)—pyrite vein crossed by galena-carbonate veinlet; (<b>F</b>)—pyrite and arsenopyrite fragments in sphalerite with inclusions of chalcopyrite; (<b>G</b>)—sphalerite, galena, and chalcopyrite in the carbonate veinlet; (<b>H</b>)—later chalcopyrite with fahlore; (<b>I</b>,<b>J</b>)—fahlore in the carbonate veinlet; (<b>K</b>)—sulfosalt with relicts of fahlore; (<b>L</b>)—the intergrowth of fahlore, chalcopyrite, and sulfosalt. Apy—arsenopyrite; Cb—carbonates; Ccp—chalcopyrite; Gn—galena; Py—pyrite; Pyh—pyrrhotite; Qz—quartz; Rds—rhodochrosite; Rt—rutile; Slf—sulfosalts; Sp—sphalerite; Ttr—tetrahedrite.</p> "> Figure 8
<p>BSE images of jamesonite (Ja), bournonite (Bnn), tetrahedrite-(Fe) (Ttr-Fe), and tetrahedrite-(Zn) (Ttr-Zn). The numbers of the analyses are shown in parentheses.</p> "> Figure 9
<p>BSE images. The compositions of electrum and native Au at the analysis points are indicated (wt.%).</p> "> Figure 10
<p>BSE image. A fractured pyrite-arsenopyrite aggregate with a marginal destruction zone, within which Au occurrences are noted (orange pins).</p> "> Figure 11
<p>Morphology of Au from eluvial sediments above the central Au-bearing zone of the Kalarskoe occurrence, with geochemical composition data.</p> "> Figure 12
<p>Paragenetic sequence of alteration and mineralization at the Kalarskoe occurrence. The numbers on the scheme indicate the different morphological forms of the minerals (see text). * calcite, kutnohorite, and rhodochrosite were identified and grouped.</p> "> Figure 13
<p>Distribution of (U,Th)-He ages of pyrite from the massive pyrite-arsenopyrite body, probability density plot (grey), and previous age estimations of the various rocks within the Kalarskoe field. Blue dots corresponds to the age of pyrite from the sample 7k-33.3; green dots—sample 7k-40.1. The plot is constructed using DensityPlotter software ver. 8.5 [<a href="#B21-minerals-14-00708" class="html-bibr">21</a>]. Error bars represents 2σ.</p> "> Figure 14
<p>Images of the pyrite from the sample 7k-33.3 m, which shows at least two coexisting generations of pyrite: grains with zonation (<b>A</b>,<b>B</b>) and grains without signs of the zonation. Dotted lines are used to emphasizes the internal zoning.</p> ">
Abstract
:1. Introduction
2. Geological Settings and Regional Metallogeny
3. Geochronology
4. Au-Bearing Potential of the Kaburchak Au-Ag Cluster
5. Mineralogical and Geochemical Features of Mineralization and Altered Rocks
6. Methods
6.1. Material
6.2. Mineralogical and Geochemical Studies
6.3. (U,Th)-He Dating
7. Results
7.1. Mineralogical and Geochemical Observations
(Sb3.95–4.29, As0.01–0.09, Bi0.01–0.14)Σ = 4–4.30 S12.45–13.48
7.2. Stages of the Mineralization
7.3. (U,Th)-He Dating Results
8. Discussion
8.1. Classification of the Kalarskoe Occurrence
8.2. The Age of Au-Ag Mineralization
9. Conclusions
Supplementary Materials
Author Contributions
Funding
Data Availability Statement
Acknowledgments
Conflicts of Interest
References
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Object | Rock/Complex | Age | Method | Source |
---|---|---|---|---|
Surich-2 | rhyolite porphyry/Kuyagan | 382 ± 3.5 | Zr U-Pb | [5] |
Tolstuha mountain | quartz-diorite porphyry | 378.9 ± 3.4 | Zr U-Pb | [5] |
Verbluzhya mountain | rhyolite porphyry/Kuyagan | 372.7 ± 3.7 | Zr U-Pb | [5] |
Kurya occurence | Rhyolite/Sagan | 389 ± 3 | Zr U-Pb | [3] |
390 ± 3 | Zr U-Pb | |||
393 ± 3 | Zr U-Pb | |||
Andesite | 390.5 ± 5.5 | Zr U-Pb | ||
Au-bearing breccias | ~400 | Zr U-Pb | ||
349 ± 3 | Zr U-Pb | |||
359 ± 7 | Zr U-Pb | |||
126 ± 3 | Zr U-Pb | |||
Kalarskoe occurence | Rhyolite porphyry | 379.5 ± 1.6 | Zr U-Pb | [10] |
Au-bearing beresites | 396.2 ± 3.8 | Ser Ar-Ar | [1] | |
Mineralized zones (pyrite-arsenopyrite massive body) | 371–399 | Pyr (U,Th)-He | (this study) |
Mineralized Veins and Veinlets | Argillic Alteration (Rarely, Relict Porphyry Texture) | Propylitic Alteration (Local Relict Porphyry Texture) | Dacite and Andesite Porphyries | ||
---|---|---|---|---|---|
Pyrite Arsenopyrite Calcite Kutnohorite Quartz ±Rhodochrosite ±Sphalerite ±Chalcopyrite ±Galena ±Sulfosalts ±Electrum, Au | Inner | Outer | Outer | Inner | phenocrysts: plagioclase, ±pyroxene, amphibole Matrix has a felsic or intermediate content |
Quartz Illite ±Kaolinite ±Pyrite ±Rutile | Quartz Illite Chlorite ±Sericite ±Pyrite ±Rutile | Albite Chlorite Quartz ±Pyrite ±Pyrrhotite ±Rutile | Albite Chlorite Epidote Quartz ±Pyrite ±Pyrrhotite ±Rutile |
n | Ag | Cu | Hg | Zn | Fe | Cd | In | Mn | S | Total |
---|---|---|---|---|---|---|---|---|---|---|
1 | 0.01 | 0.59 | 0.03 | 62.99 | 3.22 | 0.62 | 0.04 | 0.03 | 33.41 | 100.93 |
2 | 0.00 | 0.75 | 0.02 | 62.36 | 3.59 | 0.54 | 0.06 | 0.03 | 33.51 | 100.86 |
3 | 54.7 | 10.2 | 0.6 | 33.7 | 99.1 | |||||
4 | 60.3 | 5.5 | 0.4 | 0.4 | 33.5 | 100.1 | ||||
5 | 56.4 | 9.2 | 0.5 | 34.1 | 100.2 | |||||
6 | 58.4 | 7.4 | 0.4 | 33.7 | 99.9 | |||||
7 | 59.5 | 7.2 | 0.5 | 32.8 | 100.0 | |||||
8 | 62.4 | 2.5 | 35.1 | 100.0 |
n | Sb | Se | S | Cu | Ag | As | Bi | Zn | Pb | Fe | Hg | Total | Tetrahedrite Type |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|
1 | 29.37 | 25.12 | 35.18 | 2.16 | 0.08 | 0.19 | 4.09 | 0.05 | 2.89 | 99.12 | Zn | ||
2 | 28.74 | 24.88 | 33.88 | 2.00 | 0.13 | 1.74 | 4.04 | 1.33 | 2.73 | 99.46 | Zn | ||
3 | 29.68 | 0.03 | 25.04 | 34.77 | 2.54 | 0.10 | 0.43 | 3.72 | 0.12 | 3.17 | 99.60 | Zn | |
4 | 28.46 | 0.02 | 24.85 | 34.39 | 2.52 | 0.09 | 0.93 | 3.37 | 0.78 | 4.29 | 99.69 | Fe | |
5 | 29.41 | 0.01 | 25.37 | 34.03 | 2.61 | 0.09 | 0.23 | 3.11 | 0.16 | 5.36 | 0.03 | 100.42 | Fe |
6 | 29.07 | 0.02 | 25.81 | 33.55 | 2.50 | 0.09 | 0.37 | 2.98 | 0.16 | 5.94 | 0.02 | 100.51 | Fe |
7 | 29.22 | 0.01 | 25.27 | 35.75 | 2.16 | 0.15 | 0.15 | 3.72 | 0.06 | 3.69 | 100.18 | Fe | |
8 | 29.43 | 25.18 | 35.63 | 1.94 | 0.13 | 0.19 | 3.85 | 0.09 | 3.41 | 99.85 | Fe | ||
9 | 29.15 | 25.47 | 36.85 | 1.91 | 0.12 | 0.11 | 4.05 | 0.02 | 3.15 | 100.83 | Zn | ||
10 | 30.16 | 23.05 | 36.54 | 1.96 | 0.02 | 0.11 | 3.52 | 0.03 | 3.39 | 98.78 | Fe | ||
11 | 30.24 | 0.01 | 25.08 | 33.49 | 2.28 | 0.04 | 0.10 | 3.39 | 0.05 | 3.19 | 0.06 | 97.92 | Fe |
12 | 30.20 | 25.12 | 33.27 | 2.42 | 0.04 | 0.07 | 3.32 | 0.08 | 3.10 | 97.60 | Fe | ||
13 | 29.41 | 25.32 | 35.47 | 2.07 | 0.39 | 0.19 | 3.54 | 0.07 | 3.61 | 100.07 | Zn | ||
16 | 28.3 | 24.5 | 35.6 | 0.7 | 4.5 | 5.2 | 98.8 | Fe |
n | Sb | Se | S | Cu | Ag | As | Bi | Zn | Pb | Fe | Te | Hg | Total |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|
1 | 29.86 | 0.03 | 21.36 | 0.04 | 0.07 | 0.03 | 8.04 | 37.36 | 3.40 | 100.19 | |||
2 | 29.08 | 0.06 | 21.31 | 0.02 | 0.12 | 0.03 | 7.99 | 37.50 | 2.95 | 99.06 | |||
3 | 29.10 | 21.35 | 0.09 | 0.15 | 0.06 | 8.24 | 37.23 | 3.57 | 99.79 | ||||
4 | 29.95 | 21.27 | 0.04 | 0.04 | 0.05 | 7.91 | 0.04 | 37.91 | 3.06 | 100.25 | |||
5 | 29.51 | 0.02 | 21.28 | 0.03 | 0.06 | 8.04 | 37.74 | 2.84 | 0.04 | 99.56 | |||
6 | 28.73 | 0.01 | 21.13 | 0.08 | 0.05 | 9.01 | 37.43 | 3.30 | 99.75 | ||||
7 | 30.05 | 20.83 | 0.04 | 0.07 | 7.38 | 37.61 | 3.75 | 0.01 | 99.73 | ||||
8 | 25.68 | 20.19 | 0.04 | 13.77 | 36.91 | 3.53 | 100.11 |
Formula Units Based on (Pb + Ag + Sb + Bi + As) = 10 | |||||||||||||||
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
n | Sb | Se | S | Cu | Ag | As | Bi | Zn | Pb | Fe | Cu + Fe + Zn | Bi + Sb + As | Bi/Sb | (Pb + Ag)/(Sb + Bi) | S + Se + Te |
1 | 5.27 | 0.01 | 14.32 | 0.01 | 0.01 | 0.01 | 0.83 | 3.88 | 1.31 | 1.32 | 6.11 | 0.16 | 0.64 | 14.33 | |
2 | 5.20 | 0.02 | 14.46 | 0.01 | 0.02 | 0.01 | 0.83 | 3.94 | 1.15 | 1.16 | 6.04 | 0.16 | 0.66 | 14.48 | |
3 | 5.19 | 14.47 | 0.03 | 0.03 | 0.02 | 0.86 | 3.90 | 1.39 | 1.42 | 6.07 | 0.16 | 0.65 | 14.47 | ||
4 | 5.26 | 14.19 | 0.01 | 0.01 | 0.01 | 0.81 | 0.01 | 3.91 | 1.17 | 1.20 | 6.08 | 0.15 | 0.64 | 14.19 | |
5 | 5.22 | 0.01 | 14.31 | 0.01 | 0.02 | 0.83 | 3.93 | 1.10 | 1.11 | 6.07 | 0.16 | 0.65 | 14.31 | ||
6 | 5.13 | 14.32 | 0.03 | 0.01 | 0.94 | 3.92 | 1.28 | 1.31 | 6.08 | 0.18 | 0.65 | 14.32 | |||
7 | 5.31 | 13.99 | 0.01 | 0.02 | 0.76 | 3.91 | 1.45 | 1.46 | 6.09 | 0.14 | 0.64 | 13.99 | |||
8 | 4.64 | 13.84 | 0.01 | 1.45 | 3.91 | 1.39 | 1.40 | 6.09 | 0.31 | 0.64 | 13.84 | ||||
Formula units based on 25 atoms | |||||||||||||||
1 | 5.14 | 0.01 | 13.96 | 0.01 | 0.01 | 0.01 | 0.81 | 0.00 | 3.78 | 1.28 | 1.29 | 5.95 | 0.16 | 0.64 | 13.97 |
2 | 5.07 | 0.02 | 14.10 | 0.01 | 0.02 | 0.01 | 0.81 | 0.00 | 3.84 | 1.12 | 1.13 | 5.89 | 0.16 | 0.66 | 14.12 |
3 | 5.01 | 0.00 | 13.97 | 0.03 | 0.03 | 0.02 | 0.83 | 0.00 | 3.77 | 1.34 | 1.37 | 5.86 | 0.16 | 0.65 | 13.97 |
4 | 5.18 | 0.00 | 13.97 | 0.01 | 0.01 | 0.01 | 0.80 | 0.01 | 3.85 | 1.15 | 1.18 | 5.99 | 0.15 | 0.64 | 13.97 |
5 | 5.14 | 0.01 | 14.07 | 0.01 | 0.00 | 0.02 | 0.82 | 0.00 | 3.86 | 1.08 | 1.09 | 5.97 | 0.16 | 0.65 | 14.08 |
6 | 5.00 | 0.00 | 13.97 | 0.03 | 0.00 | 0.01 | 0.91 | 0.00 | 3.83 | 1.25 | 1.28 | 5.93 | 0.18 | 0.65 | 13.97 |
7 | 5.22 | 0.00 | 13.74 | 0.01 | 0.00 | 0.02 | 0.75 | 0.00 | 3.84 | 1.42 | 1.43 | 5.98 | 0.14 | 0.64 | 13.75 |
8 | 4.59 | 0.00 | 13.71 | 0.01 | 0.00 | 0.00 | 1.43 | 0.00 | 3.88 | 1.38 | 1.39 | 6.03 | 0.31 | 0.64 | 13.71 |
n | Sb | Se | S | Cu | As | Bi | Zn | Pb | Fe | Hg | Total |
---|---|---|---|---|---|---|---|---|---|---|---|
9 | 24.44 | 0.02 | 19.92 | 12.49 | 0.06 | 0.65 | 0.04 | 40.48 | 1.17 | 0.04 | 99.32 |
Sample | Weight, mg | He, 1010 at | 1σ, % | U, 1010 at | 1σ, % | Th, 1010 at | 1σ, % | Age, Ma | ± | U, ppm | Th/U | flowT |
---|---|---|---|---|---|---|---|---|---|---|---|---|
7k-33.3 m | ||||||||||||
1175 | 2.1 | 359 | 0.5 | 422 | 4.2 | 1117 | 4.5 | 401 | 20 | 0.8 | 2.7 | 1.6 |
1176 | 2.1 | 320 | 0.5 | 363 | 3.1 | 1040 | 2.4 | 402 | 15 | 0.69 | 2.9 | 2.7 |
1177 | 1.7 | 261 | 0.5 | 336 | 3.3 | 969 | 4.3 | 355 | 14 | 0.78 | 2.9 | 2.5 |
1204 * | 1.7 | 147 | 1.2 | 156 | 1.4 | 462 | 1.1 | 425 | 14 | 0.36 | 3.0 | 1.0 |
1206 | 1.9 | 273 | 1.3 | 341 | 1.7 | 950 | 1.4 | 370 | 12 | 0.71 | 2.8 | 1.5 |
Weighted mean | 377 | 22 | ||||||||||
7k-40.1 m | ||||||||||||
1089 | 1.1 | 170 | 0.6 | 225 | 4.0 | 521 | 2.7 | 373 | 20 | 0.81 | 2.3 | 2.8 |
1094 | 2.3 | 270 | 0.7 | 343 | 1.5 | 915 | 1.5 | 370 | 8 | 0.59 | 2.7 | 1.7 |
Weighted mean | 371 | 8 | ||||||||||
Empty quartz ampoule | ||||||||||||
28–56 | 1.1 | 37 | 1.3 | 97 | 6 | 74 |
Type | Ore Minerals | Major Vein Minerals | Main Alteration Types | Main Mineralization Styles | Sulfide Abundance | Genetically Related Volcanism and Tectonic Settings |
---|---|---|---|---|---|---|
High sulfidation | Found: pyrite (common) Not found: enargite, luzonite, famatinite, covellite, tellurides | Found: quartz Not found: alunite, barite, vuggy residual quartz | Not found: silicification, quartz-alunite/APS, quartz-pyrophyllite/dickite at depth | Found: massive sulfide bodies, stockworks, hydrothermal breccias Not found: stockwork-disseminations and veins in massive and vuggy quartz | 10–90 vol% | calc-alkaline andesitic-dacitic arcs (neutral stress to mildly extensional arc, compressive back arc during arc volcanism) |
Intermediate sulfidation | Found: pyrite (common), arsenopyrite (common), chalcopyrite, sphalerite, galena, pyrrhotite, tetrahedrite-(Zn), tetrahedrite-(Fe) Not found: tellurides | Found: quartz, Mn carbonates (common), calcite Not found: barite, rhodonite, adularia | Found: quartz-sericite, quartz-illite | Found: veins, stockworks | 5–30 vol% | calcic to calc-alkaline andesitic-dacitic volcanic-subvolcanic rocks: NC (neutral-compressional)-type and E (extensional)-type |
Low sulfidation | Found: pyrite (common), arsenopyrite 1 (common), chalcopyrite, sphalerite 2, galena pyrrhotite 1, tetrahedrite-(Zn), tetrahedrite-(Fe) Not found: selenides | Found: quartz Not found: ankerite-dolomite, adularia, fluorite, barite, celestine, chalcedony | Not found: quartz-illite/smectite-adularia | Found: veins, stockworks, disseminations | 1–5 vol% (but up to 20 vol% for basalt) | Bimodal volcanism (extensional settings: extensional intra-arc and back-arc, post-collisional orogenic belts, continental and island-arc rifts) |
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Chernykh, A.I.; Leibham, P.N.; Sokolova, L.A.; Yakubovich, O.V.; Anosova, M.O.; Naumov, E.A. The Devonian Kalarskoe Epithermal Occurrence of the Kaburchak Au-Ag Cluster in the Altai-Sayan Folded Area, Russia: Geological Setting; Mineralogical, Geochemical, and Geochronological Features. Minerals 2024, 14, 708. https://doi.org/10.3390/min14070708
Chernykh AI, Leibham PN, Sokolova LA, Yakubovich OV, Anosova MO, Naumov EA. The Devonian Kalarskoe Epithermal Occurrence of the Kaburchak Au-Ag Cluster in the Altai-Sayan Folded Area, Russia: Geological Setting; Mineralogical, Geochemical, and Geochronological Features. Minerals. 2024; 14(7):708. https://doi.org/10.3390/min14070708
Chicago/Turabian StyleChernykh, Alexander I., Polina N. Leibham, Lidia A. Sokolova, Olga V. Yakubovich, Maria O. Anosova, and Evgeny A. Naumov. 2024. "The Devonian Kalarskoe Epithermal Occurrence of the Kaburchak Au-Ag Cluster in the Altai-Sayan Folded Area, Russia: Geological Setting; Mineralogical, Geochemical, and Geochronological Features" Minerals 14, no. 7: 708. https://doi.org/10.3390/min14070708