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 ruleThe 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