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LITHOEN

Deposit

Vihanti

Also known as Lampinsaari, Isoaho

A mineral deposit recorded by the USGS volcanogenic massive sulfide database, at Oulu, Finland. The compilation classifies it as a bimodal-mafic volcanic host succession. Its reported host rocks are quartz-feldspathic schist, black schist, cordierite gneiss, dolomite, skarn. Minerals reported present include antimony, arsenopyrite, barite, berthierite, bismuth, boulangerite, bournonite, breithauptite.

Classification

recognition basis
authoritativeDatabase
realm
europe

What this record is, and who says so

Recognised on the basis of

Authoritative database

A curated deposit database published by a scientific institution, in which inclusion is itself a documented editorial decision with stated criteria.

A deposit is an occurrence of sufficient size and grade that it might, under the most favourable circumstances, be considered to have economic potential. Lithoen records that a named authority made that judgement. It is not a statement that anything here is recoverable, and it is not a resource or a reserve.

How it is interpreted

A deposit is not a mineral system. A source interprets it as an example of one, and interpretations change while the rock does not.

  • Interpreted as an example of Volcanogenic massive sulfide system

    By — Membership of the USGS volcanogenic massive sulfide database, which is a compilation of deposits of this class.

    Inclusion in a compilation of this deposit class is the compilation’s own interpretation of this deposit. It is not an independent genetic study.

Commodities documented here

  • Copper (commodity)documented association

    The compilation reports a grade for this metal at this deposit. Lithoen records the documented association and infers nothing about how it would be worked.

  • Gold (commodity)documented association

    The compilation reports a grade for this metal at this deposit. Lithoen records the documented association and infers nothing about how it would be worked.

  • Lead (commodity)documented association

    The compilation reports a grade for this metal at this deposit. Lithoen records the documented association and infers nothing about how it would be worked.

  • Silver (commodity)documented association

    The compilation reports a grade for this metal at this deposit. Lithoen records the documented association and infers nothing about how it would be worked.

  • Zinc (commodity)documented association

    The compilation reports a grade for this metal at this deposit. Lithoen records the documented association and infers nothing about how it would be worked.

Reported figures, and what each one is

A sample assay, a deposit average, a compiler total and a reported reserve are different quantities. Each figure below carries which one it is; none of them is a current resource or reserve.

29.63 Mt

Compiler total, for modelling

A sum assembled by a database compiler from production plus reserves plus resources at the lowest available cut-off, so that deposits can be compared in a grade-and-tonnage model. It is not a resource, not a reserve and not production; it is a modelling quantity, and the USGS databases Lithoen reads define their tonnage exactly this way.

The usgs volcanogenic massive sulfide database reports an ore tonnage of 29.63 million tonnes for Vihanti.

28.1 Mt

Historical production

Material reported as mined over a stated period. Gone, not remaining.

The Geological Survey of Finland reports 28.1 million tonnes of ore mined at Vihanti between 1954 and 1992, on the authority of Kousa and others (1997). A separate row of the same table records a remaining resource of 9.164 million tonnes. The two are reported separately and are not added together here.

0.48 wt%m Copper

Historical production grade

The grade of material actually mined and processed over a stated period. Records what was taken, not what remains.

The Geological Survey of Finland reports a copper grade of 0.48 weight percent for the ore mined at Vihanti between 1954 and 1992, on the authority of Kousa and others (1997). The USGS volcanogenic massive sulfide database reports a lower figure for this deposit; the two compilations are independent and Lithoen publishes both rather than choosing.

0.42 wt%m Copper

Deposit average

An average grade attributed to a whole deposit by a compiler, over a tonnage defined by that compiler at a stated cut-off. Not a measurement of anything: a summary of an estimate.

The usgs volcanogenic massive sulfide database reports a copper grade of 0.42 weight percent for Vihanti.

0.3 g/t Gold

Deposit average

An average grade attributed to a whole deposit by a compiler, over a tonnage defined by that compiler at a stated cut-off. Not a measurement of anything: a summary of an estimate.

The compilation reports a gold grade of 0.3 grams per tonne of ore for Vihanti. The field is defined as the average grade of gold for the deposit, stated as grams per metric ton of ore.

0.28 wt%m Lead

Deposit average

An average grade attributed to a whole deposit by a compiler, over a tonnage defined by that compiler at a stated cut-off. Not a measurement of anything: a summary of an estimate.

The usgs volcanogenic massive sulfide database reports a lead grade of 0.28 weight percent for Vihanti.

21 g/t Silver

Deposit average

An average grade attributed to a whole deposit by a compiler, over a tonnage defined by that compiler at a stated cut-off. Not a measurement of anything: a summary of an estimate.

The compilation reports a silver grade of 21.0 grams per tonne of ore for Vihanti. The field is defined as the average grade of silver for the deposit, stated as grams per metric ton of ore.

4.68 wt%m Zinc

Deposit average

An average grade attributed to a whole deposit by a compiler, over a tonnage defined by that compiler at a stated cut-off. Not a measurement of anything: a summary of an estimate.

The usgs volcanogenic massive sulfide database reports a zinc grade of 4.68 weight percent for Vihanti.

0.49 g/t Gold

Historical production grade

The grade of material actually mined and processed over a stated period. Records what was taken, not what remains.

The Geological Survey of Finland reports a gold grade of 0.49 grams per tonne of ore for the ore mined at Vihanti between 1954 and 1992, on the authority of Kousa and others (1997). The USGS volcanogenic massive sulfide database reports a lower figure for this deposit; the two compilations are independent and Lithoen publishes both rather than choosing.

0.36 wt%m Lead

Historical production grade

The grade of material actually mined and processed over a stated period. Records what was taken, not what remains.

The Geological Survey of Finland reports a lead grade of 0.36 weight percent for the ore mined at Vihanti between 1954 and 1992, on the authority of Kousa and others (1997). The USGS volcanogenic massive sulfide database reports a lower figure for this deposit; the two compilations are independent and Lithoen publishes both rather than choosing.

25 g/t Silver

Historical production grade

The grade of material actually mined and processed over a stated period. Records what was taken, not what remains.

The Geological Survey of Finland reports a silver grade of 25.0 grams per tonne of ore for the ore mined at Vihanti between 1954 and 1992, on the authority of Kousa and others (1997). The USGS volcanogenic massive sulfide database reports a lower figure for this deposit; the two compilations are independent and Lithoen publishes both rather than choosing.

5.12 wt%m Zinc

Historical production grade

The grade of material actually mined and processed over a stated period. Records what was taken, not what remains.

The Geological Survey of Finland reports a zinc grade of 5.12 weight percent for the ore mined at Vihanti between 1954 and 1992, on the authority of Kousa and others (1997). The USGS volcanogenic massive sulfide database reports a lower figure for this deposit; the two compilations are independent and Lithoen publishes both rather than choosing.

The source records behind this

What one row of a published dataset was taken to mean, and why. The original record stays traceable after reconciliation.

  • Volcanogenic massive sulfide deposits of the world (USGS OFR 2009-1034), record 1276

    Named there
    Vihanti
    The source calls it
    deposit
    Lithoen reads it as
    deposit (stated)

    The usgs volcanogenic massive sulfide database states what one of its rows is, and this row is read as the deposit the compilers named. Its 500-metre rule means any separately named bodies within that distance are already combined here.

    Read and refused

    • grade and tonnage columns with no value — The compilation writes "(no value)" or leaves the field empty where the information was not available. Reading an empty field as zero would publish a measurement nobody made.
    • deposits within 5 km and 10 km columns — Proximity of other deposits is a fact about the compilation’s spatial density, and Lithoen refuses to publish anything that could be read as prospectivity.

How this is mapped

One published representation of where Vihanti is. Each is one interpretation, by one identified source, at one scale — not the shape of the thing itself.

  • Representative point

    Point · 1 positionspreferred for publication

    A single position standing for something that is not a point. It exists so a feature can be shown on a map or listed by location, and it asserts NOTHING about extent. A representative point for a 2,000 km province is a label anchor, not a location.

    A representative point for Vihanti from the USGS volcanogenic massive sulfide database. It marks where the compilation places the deposit; it is not a boundary, not a shaft, and implies nothing about the body's extent.

    Boundary certainty
    ApproximateThe position is known only within a distance much larger than the line width on any map that shows it. Drawing it thinner does not make it better known.
    Status of this geometry
    inferredThe status of the geometry, which need not match the status of what the entity’s claims assert.
    Dataset
    Volcanogenic massive sulfide deposits of the world (USGS OFR 2009-1034)Mosier, D.L., Berger, V.I., and Singer, D.A., 2009, Volcanogenic massive sulfide deposits of the world: Database and grade and tonnage models: U.S. Geological Survey Open-File Report 2009-1034, doi:10.3133/ofr20091034.

    What was done to this geometry

    • By Lithoen — Rounded to 4 decimal places. The compilation computed its decimal degrees from authored degrees-minutes-seconds columns, and the further digits are conversion residue rather than knowledge.
    • Before it reached Lithoen — The compilation computed these decimal degrees from the degrees-minutes-seconds columns its compilers authored.

How this record is known

19
Settled consensus
Cited as the accepted position of the discipline.
1
Interpretation
Reached by reasoning from evidence, or produced by a named model.

20 of 20 claims on this page cite at least one registered source. Counts describe how each statement is known, not how likely it is to be true.

What Lithoen records

Each claim states how it is known and cites its evidence.

Established0.48 wt%m Copper

Reported for this deposit

The Geological Survey of Finland reports a copper grade of 0.48 weight percent for the ore mined at Vihanti between 1954 and 1992, on the authority of Kousa and others (1997). The USGS volcanogenic massive sulfide database reports a lower figure for this deposit; the two compilations are independent and Lithoen publishes both rather than choosing.

  • scope: historicalProductionGrade
  • precision note: The figure is for ore mined at Vihanti between 1954 and 1992. Table 027 states this as the mined row and lists the remaining resource of 9.164 Mt on a separate row; the two are not summed here.
  • source record: Geological Survey of Finland Special Paper 53, Table 027, row "Vihanti, mined", attributed by the table to Kousa et al. (1997).
  • definition basis: Table 027 declares its units in the column headers — tonnage in Mt, Zn, Cu and Pb in per cent, Ag and Au in grams per tonne. The volume gives no analytical method for these figures and attributes them to Kousa and others (1997), which Lithoen has not retrieved. The grade is the operator’s reported average over the ore mined, not an assay of any sample.
  • assertion basis: SOURCE_REPORTED

Evidence support: Supported by the cited evidence one source

Evidence: (ed.) 2012 Primary authority

Establisheda bimodal-mafic volcanic host succession

How a source classifies it

The usgs volcanogenic massive sulfide database classifies Vihanti as a bimodal-mafic volcanic host succession, a classification of the volcanic host succession rather than of the mineralisation.

  • definition basis: Deposit-type field of the USGS volcanogenic massive sulfide database, whose values are enumerated in the dataset itself.
  • assertion basis: SOURCE_CLASSIFICATION

Evidence support: Supported by the cited evidence 2 sources, single source

Evidence: D.L. 2009 Primary authority

Established0.42 wt%m Copper

Reported for this deposit

The usgs volcanogenic massive sulfide database reports a copper grade of 0.42 weight percent for Vihanti.

  • scope: depositAverage
  • definition basis: Grade as the compilation reports it for this deposit.
  • assertion basis: SOURCE_REPORTED

Evidence support: Supported by the cited evidence 2 sources, single source

Evidence: D.L. 2009 Primary authority

Established0.3 g/t Gold

Reported for this deposit

The compilation reports a gold grade of 0.3 grams per tonne of ore for Vihanti. The field is defined as the average grade of gold for the deposit, stated as grams per metric ton of ore.

  • scope: depositAverage
  • definition basis: Grade as the compilation reports it for this deposit.
  • precision note: Unit corrected in Phase 9. An earlier version published this figure as 0.3 weight percent, because the bulk ingestion mapped every grade column to weight percent. The compilation defines augrd as “average grade of gold for the deposit, as grams per metric ton of ore” — copper and molybdenum are percentages in these files, silver and gold are grams per tonne. The published number was overstated by four orders of magnitude, and for several deposits it exceeded 100 percent, which is not a grade any rock can have.
  • assertion basis: SOURCE_REPORTED

Evidence support: Supported by the cited evidence 2 sources, single source

Evidence: D.L. 2009 Primary authority

Establishedquartz-feldspathic schist; black schist; cordierite gneiss; dolomite; skarn

Reported for this deposit

The rocks reported as hosting Vihanti are quartz-feldspathic schist, black schist, cordierite gneiss, dolomite, skarn, as named for this deposit by the USGS volcanogenic massive sulfide database.

  • precision note: The host lithologies are those the compilation names for this deposit. They are not inferred from a class description and not from a point falling inside a mapped polygon.
  • assertion basis: SOURCE_REPORTED

Evidence support: Supported by the cited evidence 2 sources, single source

Evidence: D.L. 2009 Primary authority

InferredAssociated with submarine volcanic rocks in a volcanic-sedimentary sequence.

Derived by Lithoen

Vihanti is carried by a compilation whose inclusion rule requires a deposit to be associated with submarine volcanic rocks in a sequence of volcanic and sedimentary rocks — lava flows, pyroclastics or volcaniclastic rocks, which need not be the deposit's only host. Its presence here is therefore a statement that it meets that test.

Not stated verbatim by the source — derived: inclusion rule of the compilation AND presence of this deposit as a row in it ⟹ this deposit satisfies the inclusion rule

The compilation states a test a deposit must meet to be carried, and it carries this deposit. The property is therefore not something the source reports of the deposit; it is what its inclusion implies. That step is Lithoen’s and it is a real one — a compiler can include a row in error, and a rule stated for a set is weaker evidence about any member than a statement made about that member. Recording it as a derivation is what keeps the claim from reading as an observation.

  • model: The inclusion rule of the USGS volcanogenic massive sulfide compilation.
  • precision note: This follows from membership of the compilation, not from a study of this deposit’s setting.
  • assertion basis: LITHOEN_DERIVED

Evidence support: Derived from the cited evidence 2 sources, single source

Evidence: D.L. 2009 Primary authority

Established0.28 wt%m Lead

Reported for this deposit

The usgs volcanogenic massive sulfide database reports a lead grade of 0.28 weight percent for Vihanti.

  • scope: depositAverage
  • definition basis: Grade as the compilation reports it for this deposit.
  • assertion basis: SOURCE_REPORTED

Evidence support: Supported by the cited evidence 2 sources, single source

Evidence: D.L. 2009 Primary authority

Establishedantimony; arsenopyrite; barite; berthierite; bismuth; boulangerite; bournonite; breithauptite; chalcocite; chalcopyrite; cubanite; diopside; dolomite; electrum; fluorite; freibergite; gahnite; galena; gold; graphite; gudmundite; hessite; jamesonite; limonite; magnetite; marcasite; molybdenite; nickeline; nisbite; pyrargyrite; pyrite; pyrrhotite; rutile; silver; sphalerite; stannite; tennantite; tetrahedrite; tourmaline; tremolite; ullmannite; uraninite; valleriite

Reported for this deposit

The compilation reports 43 distinct minerals present at Vihanti, of which the first twelve alphabetically are antimony, arsenopyrite, barite, berthierite, bismuth, boulangerite, bournonite, breithauptite, chalcocite, chalcopyrite, cubanite, diopside. It records presence only: no abundance, no paragenesis and no assay follows from it.

  • precision note: The compilation's mineral table holds 43 entries for this row, and the claim counts all 43 of them. The prose names 12 because a sentence of 43 mineral names is not readable; the count is stated so the list is never mistaken for the whole. Presence is not abundance, and the alphabetical order carries no paragenetic meaning.
  • assertion basis: SOURCE_REPORTED

Evidence support: Supported by the cited evidence 2 sources, single source

Evidence: D.L. 2009 Primary authority

EstablishedRecorded as a deposit by the USGS volcanogenic massive sulfide database, record 1276.

How a source classifies it

Vihanti is recorded as a deposit because the USGS volcanogenic massive sulfide database includes it, as record 1276. The compilation combines all mineralised rock within 500 metres into one deposit, so that its rows correspond to geological bodies rather than to commercial projects.

  • source record: usgs-vms-deposits-of-the-world record 1276
  • assertion basis: SOURCE_CLASSIFICATION

Evidence support: Supported by the cited evidence 2 sources, single source

Evidence: D.L. 2009 Primary authority

Established21 g/t Silver

Reported for this deposit

The compilation reports a silver grade of 21.0 grams per tonne of ore for Vihanti. The field is defined as the average grade of silver for the deposit, stated as grams per metric ton of ore.

  • scope: depositAverage
  • definition basis: Grade as the compilation reports it for this deposit.
  • precision note: Unit corrected in Phase 9. An earlier version published this figure as 21.0 weight percent, because the bulk ingestion mapped every grade column to weight percent. The compilation defines aggrd as “average grade of silver for the deposit, as grams per metric ton of ore” — copper and molybdenum are percentages in these files, silver and gold are grams per tonne. The published number was overstated by four orders of magnitude, and for several deposits it exceeded 100 percent, which is not a grade any rock can have.
  • assertion basis: SOURCE_REPORTED

Evidence support: Supported by the cited evidence 2 sources, single source

Evidence: D.L. 2009 Primary authority

Established29.63 Mt

Reported for this deposit

The usgs volcanogenic massive sulfide database reports an ore tonnage of 29.63 million tonnes for Vihanti.

  • tonnage category: compilerTotalForModelling
  • definition basis: Ore tonnage as the compilation reports it for this deposit, compiled for grade-and-tonnage modelling rather than as a resource statement under a reporting code.
  • assertion basis: SOURCE_REPORTED

Evidence support: Supported by the cited evidence 2 sources, single source

Evidence: D.L. 2009 Primary authority

Established4.68 wt%m Zinc

Reported for this deposit

The usgs volcanogenic massive sulfide database reports a zinc grade of 4.68 weight percent for Vihanti.

  • scope: depositAverage
  • definition basis: Grade as the compilation reports it for this deposit.
  • assertion basis: SOURCE_REPORTED

Evidence support: Supported by the cited evidence 2 sources, single source

Evidence: D.L. 2009 Primary authority

Established0.49 g/t Gold

Reported for this deposit

The Geological Survey of Finland reports a gold grade of 0.49 grams per tonne of ore for the ore mined at Vihanti between 1954 and 1992, on the authority of Kousa and others (1997). The USGS volcanogenic massive sulfide database reports a lower figure for this deposit; the two compilations are independent and Lithoen publishes both rather than choosing.

  • scope: historicalProductionGrade
  • precision note: The figure is for ore mined at Vihanti between 1954 and 1992. Table 027 states this as the mined row and lists the remaining resource of 9.164 Mt on a separate row; the two are not summed here.
  • source record: Geological Survey of Finland Special Paper 53, Table 027, row "Vihanti, mined", attributed by the table to Kousa et al. (1997).
  • definition basis: Table 027 declares its units in the column headers — tonnage in Mt, Zn, Cu and Pb in per cent, Ag and Au in grams per tonne. The volume gives no analytical method for these figures and attributes them to Kousa and others (1997), which Lithoen has not retrieved. The grade is the operator’s reported average over the ore mined, not an assay of any sample.
  • assertion basis: SOURCE_REPORTED

Evidence support: Supported by the cited evidence one source

Evidence: (ed.) 2012 Primary authority

Established0.36 wt%m Lead

Reported for this deposit

The Geological Survey of Finland reports a lead grade of 0.36 weight percent for the ore mined at Vihanti between 1954 and 1992, on the authority of Kousa and others (1997). The USGS volcanogenic massive sulfide database reports a lower figure for this deposit; the two compilations are independent and Lithoen publishes both rather than choosing.

  • scope: historicalProductionGrade
  • precision note: The figure is for ore mined at Vihanti between 1954 and 1992. Table 027 states this as the mined row and lists the remaining resource of 9.164 Mt on a separate row; the two are not summed here.
  • source record: Geological Survey of Finland Special Paper 53, Table 027, row "Vihanti, mined", attributed by the table to Kousa et al. (1997).
  • definition basis: Table 027 declares its units in the column headers — tonnage in Mt, Zn, Cu and Pb in per cent, Ag and Au in grams per tonne. The volume gives no analytical method for these figures and attributes them to Kousa and others (1997), which Lithoen has not retrieved. The grade is the operator’s reported average over the ore mined, not an assay of any sample.
  • assertion basis: SOURCE_REPORTED

Evidence support: Supported by the cited evidence one source

Evidence: (ed.) 2012 Primary authority

Established28.1 Mt

Reported for this deposit

The Geological Survey of Finland reports 28.1 million tonnes of ore mined at Vihanti between 1954 and 1992, on the authority of Kousa and others (1997). A separate row of the same table records a remaining resource of 9.164 million tonnes. The two are reported separately and are not added together here.

  • tonnage category: historicalProduction
  • precision note: The figure is for ore mined at Vihanti between 1954 and 1992. Table 027 states this as the mined row and lists the remaining resource of 9.164 Mt on a separate row; the two are not summed here.
  • source record: Geological Survey of Finland Special Paper 53, Table 027, row "Vihanti, mined", attributed by the table to Kousa et al. (1997).
  • definition basis: Table 027 declares its units in the column headers — tonnage in Mt, Zn, Cu and Pb in per cent, Ag and Au in grams per tonne. The volume gives no analytical method for these figures and attributes them to Kousa and others (1997), which Lithoen has not retrieved. The grade is the operator’s reported average over the ore mined, not an assay of any sample.
  • assertion basis: SOURCE_REPORTED

Evidence support: Supported by the cited evidence one source

Evidence: (ed.) 2012 Primary authority

Establishedzinc; copper; pyrite; lead-silver-gold; uranium-phosphorus

Reported for this deposit

The volume reports five types of mineralisation at Vihanti — zinc, copper, pyrite, lead-silver-gold, and uranium-phosphorus — and gives their relative order: the uranium-phosphorus type is the oldest and the lead-silver-gold and zinc ores are the youngest, on the authority of Autere and others (1991). The order is relative. No absolute age is given for any of the five and none is supplied here.

  • non uniqueness: The five types are ore types distinguished by the operator, not mineral species and not separate deposits. They occur within one mine.
  • precision note: The relative order is the source’s and rests on Autere and others (1991), which Lithoen has not retrieved.
  • assertion basis: SOURCE_REPORTED

Evidence support: Supported by the cited evidence one source

Evidence: (ed.) 2012 Primary authority

Established25 g/t Silver

Reported for this deposit

The Geological Survey of Finland reports a silver grade of 25.0 grams per tonne of ore for the ore mined at Vihanti between 1954 and 1992, on the authority of Kousa and others (1997). The USGS volcanogenic massive sulfide database reports a lower figure for this deposit; the two compilations are independent and Lithoen publishes both rather than choosing.

  • scope: historicalProductionGrade
  • precision note: The figure is for ore mined at Vihanti between 1954 and 1992. Table 027 states this as the mined row and lists the remaining resource of 9.164 Mt on a separate row; the two are not summed here.
  • source record: Geological Survey of Finland Special Paper 53, Table 027, row "Vihanti, mined", attributed by the table to Kousa et al. (1997).
  • definition basis: Table 027 declares its units in the column headers — tonnage in Mt, Zn, Cu and Pb in per cent, Ag and Au in grams per tonne. The volume gives no analytical method for these figures and attributes them to Kousa and others (1997), which Lithoen has not retrieved. The grade is the operator’s reported average over the ore mined, not an assay of any sample.
  • assertion basis: SOURCE_REPORTED

Evidence support: Supported by the cited evidence one source

Evidence: (ed.) 2012 Primary authority

EstablishedPalaeoproterozoic island arc, Raahe–Ladoga suture, NE margin of the Svecofennian domain

A property of a dataset or model, shown here for context — not an observation about this record.

Vihanti lies in the Vihanti–Pyhäsalmi metallogenic area on the north-eastern edge of the Svecofennian domain, in the north-western part of the Raahe–Ladoga suture, long known as the Main Sulphide Ore Belt of Finland. The volume describes the massive sulphide deposits of this area as hosted mainly by metavolcanic rocks in a Palaeoproterozoic island-arc environment close to the Archaean Karelian craton.

  • generality: DATASET_PROPERTY
  • precision note: The island-arc setting is stated for the massive sulphide deposits of area F028 as a group, and Vihanti is one of them. It is a statement about the area that applies to this deposit, not a separate determination made at Vihanti.

Evidence support: Supported by the cited evidence one source

Evidence: (ed.) 2012 Primary authority

Established5.12 wt%m Zinc

Reported for this deposit

The Geological Survey of Finland reports a zinc grade of 5.12 weight percent for the ore mined at Vihanti between 1954 and 1992, on the authority of Kousa and others (1997). The USGS volcanogenic massive sulfide database reports a lower figure for this deposit; the two compilations are independent and Lithoen publishes both rather than choosing.

  • scope: historicalProductionGrade
  • precision note: The figure is for ore mined at Vihanti between 1954 and 1992. Table 027 states this as the mined row and lists the remaining resource of 9.164 Mt on a separate row; the two are not summed here.
  • source record: Geological Survey of Finland Special Paper 53, Table 027, row "Vihanti, mined", attributed by the table to Kousa et al. (1997).
  • definition basis: Table 027 declares its units in the column headers — tonnage in Mt, Zn, Cu and Pb in per cent, Ag and Au in grams per tonne. The volume gives no analytical method for these figures and attributes them to Kousa and others (1997), which Lithoen has not retrieved. The grade is the operator’s reported average over the ore mined, not an assay of any sample.
  • assertion basis: SOURCE_REPORTED

Evidence support: Supported by the cited evidence one source

Evidence: (ed.) 2012 Primary authority

EstablishedZn ores in dolomite and skarn, >75% of total ore resource; U-P ore >1 Mt, never mined

Reported for this deposit

The zinc ores at Vihanti are hosted by dolomite and skarn rock and contained over 75 percent of the total ore resource, making them by far the most important ore types for the economy of the mine. The uranium-phosphorus mineralisation, over one million tonnes of low-grade ore, was never exploited.

  • precision note: "Over 75 %" and "over 1 Mt" are the volume’s own bounds. They are not measurements Lithoen can sharpen and are carried as written.
  • assertion basis: SOURCE_REPORTED

Evidence support: Supported by the cited evidence one source

Evidence: (ed.) 2012 Primary authority

In the knowledge graph

Record last updated 2026-09-07. Corrections follow the published corrections policy; superseded claims are retained, never silently edited.