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Brazil

Pilar Mine

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Summary

Mine TypeUnderground
StatusActive
Commodities
  • Gold
Mining Method
  • Sub-level open stoping (SLOS)
  • Mechanized Cut & Fill
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SnapshotPilar mine is a part of Caete Complex.

Ore produced from Pilar is transported to the Caeté processing plant adjacent to Roça Grande, a total distance of approximately 40 km by road.

Pilar in 2024 put significant effort into accessing the BA ore structure on 15- and 16-levels. This area was identified in 2023 and early results from the first development in Q1 2024 indicated a significant potential orebody with grades distinctly above the traditional BF mining zones. Work continued to develop additional access into the BA structure. The BA structure in 2024 produced roughly 20% of the mine’s ounces at grades above the mine average (although a significant portion of those ounces came from development work which has historically been lower grade than stoping ore).

Owners

SourceSource
CompanyInterestOwnership
Jaguar Mining Inc. 100 % Indirect
Mineração Serras do Oeste Ltda. (operator) 100 % Direct
The Caeté Mining Complex is owned and operated by Jaguar’s wholly-owned subsidiary, Mineracão Serras do Oeste (MSOL).

Contractors

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Deposit type

  • Banded iron formation hosted
  • Mesothermal
  • Paleoplacer

Summary:

The gold metallogeny in the Iron Quadrangle is complex, with gold mineralization predominately observed within three general types of deposits:
- Archean-age, invariably stratabound-like, Algoma BIF hosted deposits.
- “Quartz vein swarms-style”, clearly mesothermal deposits.
- Early-Proterozoic, Witwatersrand type paleo-placer deposits.

While the Pilar and Roça Grande deposits are examples of the Algoma BIF hosted type, Córrego Brandão is a folded and sheared deposit hosted in carbonate-quartz-chlorite schists with iron occurrences. The main geological characteristics of this group are summarized as follows:
- Main host/fertile “Algoma type” BIF Units: These units host the mineralization and are stratigraphically located at the waning stages of major volcanic cycles of the Rio da Velhas greenstone belt. They are overlain by later sedimentary rocks composed of greywackes and turbidites.

Mineralization style:
- The mineralization consists of predominately “lateral” replacements/sulphidations of the iron carbonate-rich bands of the host Algoma type BIF units. The BIF hosted gold mineralization at Pilar, however, is not syngenetic in nature (in relation to the deposition of the host rock packages), rather it is clearly an epigenetic event that has occurred after the formation of the host rock units. There is a clear temporal-spatial-genetic relationship between the replacement/sulphidation of the host BIFs and the onset of a structurally controlled, district scale silicification event at Pilar. Textural observations suggest that at least two episodes of quartz veining has occurred. The early stage veining is deformed by the regional strain and clearly pre-dates the deformation event. The later stage veins are observed to crosscut the strain-related fabrics and so are interpreted to represent a younger mineralizing event that has taken place some time after the regional deformation event.

- Dimensions of the economic orebodies:
- Economic strike lengths of only 50 m to 350 m for individual mined zones. The average thicknesses of the BIF hosted orebodies may range from two metres to 20 m.
- At Córrego Brandão the sulphide mineralization extends approximately 1,000 m along strike and 250 m down dip. The thickness of the mineralized zones may range from two metres to 20 m.

Mineralization
Economic gold mineralization at Pilar is hosted by the folded, and locally refolded, Pilar BIF Unit including the SW Limb, São Jorge, BF III, BF II, BF, LPA, and BA mineralized zones, and by the conformably folded Torre meta-volcanic sequence.

The main zones of mineralization occur as scattered, stratabound lenses (or “pods”) of sulphide-facies BIFs within the “carbonatic-oxide-facies” deposit scale Pilar BIF Unit. Economic mineralized bodies consist of stratabound, but not stratiform, concentrations of gold bearing sulphides that occur in scattered grains, seams, and irregular shaped granular aggregates located along and replacing iron carbonates-rich bands of the BIFs. Arsenopyrite and pyrrhotite are the most important sulphide minerals in mineralized bodies, with pyrite, chalcopyrite, galena, and sphalerite commonly present as accessory minerals. A direct relationship can generally be established between the amounts of arsenopyrite (percentage per volume) and the gold concentrations in mineralized BIF samples of the Pilar deposit.

There is a clear temporal-spatial-genetic relationship between the epigenetic replacement/sulphidation of the host BIFs and the onset of a structurally controlled, district scale silicification event. Carbonate-rich bands of mineralized BIFs commonly exhibit sulphide enriched alteration/replacement halos that are symmetrically distributed around swarms of quartz veins and veinlets. The sulphide minerals occur predominately as disseminations in the host rocks, but can achieve semi-massive to massive concentrations locally, over a few metres.

Individual quartz veins are typically less than one metre in width and can be observed to be of three generations. Quartz veins of the first generation are typically associated with the gold mineralization and are folded by the main tectonic event which affected the Pilar package as a whole. Quartz veins of the second generation are typically lower grade or barren and are not affected by folding. Lastly, quartz veining of the third generation is associated with the aforementioned extensional tectonic cleavage and may also be related to halos of mineralization/sulphidation where related to hinge structural domains.

At the Pilar deposit, increased average gold grades and higher sulphide/arsenopyrite concentrations (within the economic mineralized zones and orebodies) are almost everywhere (or at least very frequently) mapped in association with the deposit scale, larger, higher-amplitude fold hinge geometries. Increased average gold grades and higher sulphide/arsenopyrite concentrations have also been observed in association with a second folding event (and/or with a subsequent third folding event) in the Pilar BIF package (Tiago Souza, 2020). The second folding event would have brought mineralized quartz veins into the BIF Pilar package, however, according to Tiago Souza (2020), the third folding event was responsible for the generation of the economic mineralization hosted by the large fold hinge geometries of the Pilar package (São Jorge synform, BF II antiform, BF antiform, BF II-BF Junction synform, BA antiform, and the smaller-amplitude Torre antiforms).

Reserves

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Mining Methods

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Heavy Mobile Equipment

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EV - Electric

Comminution

Crushers and Mills

Milling equipment has not been reported.

Processing

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Commodity Production

CommodityUnits2024202320222021202020192018201720162015
Gold oz  ....  Subscribe  ....  Subscribe  ....  Subscribe  ....  Subscribe  ....  Subscribe40,68340,91834,01727,84629,242
All production numbers are expressed as metal in doré.

Operational metrics

Metrics2024202320222021202020192018201720162015
Ore tonnes mined  ....  Subscribe  ....  Subscribe  ....  Subscribe  ....  Subscribe  ....  Subscribe
Tonnes processed  ....  Subscribe  ....  Subscribe  ....  Subscribe  ....  Subscribe  ....  Subscribe433,000 t365,082 t338,000 t290,000 t309,000 t
Daily ore mining rate  ....  Subscribe  ....  Subscribe  ....  Subscribe  ....  Subscribe  ....  Subscribe1,100 t1,100 t1,000 t1,000 t1,000 t

Production Costs

CommodityUnits20242023202220212020201920182017
Total cash costs (sold) Gold USD  ....  Subscribe  ....  Subscribe  ....  Subscribe  ....  Subscribe  ....  Subscribe 811 / oz   702 / oz   937 / oz  
All-in sustaining costs (sold) Gold USD  ....  Subscribe  ....  Subscribe  ....  Subscribe  ....  Subscribe  ....  Subscribe 1,119 / oz   986 / oz   1,226 / oz  

Mine Financials

Units20242023202220212020201920182017
Sustaining costs M USD  ....  Subscribe  ....  Subscribe  ....  Subscribe  ....  Subscribe  ....  Subscribe 12.4   11.5   9.8  
Capital expenditures M USD  ....  Subscribe  ....  Subscribe  ....  Subscribe  ....  Subscribe  ....  Subscribe 13.5   11.8   11.2  
Revenue M USD 53.2   52   42.4  

Personnel

Mine Management

Job TitleNamePhoneEmailProfileRef. Date
....................... Subscription required ....................... Subscription required ........... Subscription required ........... Subscription required Jan 13, 2025
....................... Subscription required ....................... Subscription required Subscription required Dec 31, 2021
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....................... Subscription required ....................... Subscription required Subscription required Apr 15, 2025

Workforce

EmployeesContractorsTotal WorkforceYear
...... Subscription required ...... Subscription required ...... Subscription required 2021

Aerial view:

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