Each claim states how it is known and cites its evidence.
Establisheddeparea=35; deplength=0; depwidth=0; depthick=?40
Reported for this deposit
The compilation records dimensions for the Buruktal ore body: deparea 35, deplength 0, depwidth 0, depthick ?40. These describe the size of a body and place no outline on the ground; Lithoen publishes a point for this deposit and no extent.
- precision note: Dimensions of an ore body are not a boundary. No polygon is derivable from them and none is published.
- assertion basis: SOURCE_REPORTED
Evidence support: Supported by the cited evidence · 2 sources, single source
Evidence: V.I. 2011 · Primary authority
Establishedthe Mg hydrous silicate subtype
How a source classifies it
The usgs ni-co laterite database classifies Buruktal as the Mg hydrous silicate subtype.
Not stated verbatim by the source — derived: deptype 2 -> “Mg hydrous silicate subtype”The compilation records a one-character subtype code; its own metadata enumerates what the three codes mean, and that metadata was retrieved and read. The expansion comes from the authority, not from general knowledge about laterite deposits.
- definition basis: Deposit-type field of the USGS Ni-Co laterite database, whose values are enumerated in the dataset itself.
- assertion basis: SOURCE_CLASSIFICATION
Evidence support: Derived from the cited evidence · 2 sources, single source
Evidence: V.I. 2011 · Primary authority
Establishedantigorite; chlorite; chrysotile; garnierite; goethite; halloysite; hematite; illite-smectite; kerolite; lizardite; montmorillonite; Mn-hydroxide; nontronite; pyrochroite; saponite; talc; todorokite; aegirine; chalcedony; Cr-spinel; magnetite; manganocalcite; opal; quartz; tridymite
Reported for this deposit
The compilation reports 25 distinct minerals present at Buruktal, of which the first twelve alphabetically are antigorite, chlorite, chrysotile, garnierite, goethite, halloysite, hematite, illite-smectite, kerolite, lizardite, montmorillonite, Mn-hydroxide. Of these the compilation marks antigorite, chlorite, chrysotile, garnierite, goethite as nickel-bearing at this deposit. It records presence only: no abundance, no paragenesis and no assay follows from it.
- precision note: The compilation's mineral table holds 25 entries for this row, and the claim counts all 25 of them. The prose names 12 because a sentence of 25 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: V.I. 2011 · Primary authority
Established0.9 wt%m Nickel
Reported for this deposit
The usgs ni-co laterite database reports a nickel grade of 0.9 weight percent for Buruktal, stated with respect to the reported reserve tonnage.
- scope: reserveGrade
- definition basis: Grade with respect to reserve tonnage, as the compilation defines the field.
- assertion basis: SOURCE_REPORTED
- reporting framework: None stated. The compilation calls this a grade with respect to reserve tonnage and names no reporting code — no JORC, NI 43-101 or equivalent classification, and no competent-person sign-off. A reserve reported without a framework cannot be compared with one reported under a code, and Lithoen supplies no framework it was not given.
- precision note: This claim corrects the scope of claim:buruktal-deposit-nickel-grade, which published the figure as a resource grade. The compilation defines the field as a grade with respect to RESERVE tonnage, and a resource is not a reserve: the reserve is the part shown to be economically mineable, and the resource is not. The number is unchanged; what it means is not. Note also that the reserve tonnage this grade is stated against is not itself published in this corpus, so the grade is carried without the quantity it qualifies.
Evidence support: Supported by the cited evidence · 2 sources, single source
Evidence: V.I. 2011 · Primary authority
EstablishedRecorded as a deposit by the USGS Ni-Co laterite database, record 107.
How a source classifies it
Buruktal is recorded as a deposit because the USGS Ni-Co laterite database includes it, as record 107. The compilation states that it excludes occurrences and prospects that are less well known, so every row is a deposit by the compilers' own definition.
- source record: usgs-ni-co-laterite-deposits-of-the-world record 107
- assertion basis: SOURCE_CLASSIFICATION
Evidence support: Supported by the cited evidence · 2 sources, single source
Evidence: V.I. 2011 · Primary authority
EstablishedMesozoic
Reported for this deposit
The USGS laterite database places the laterite-forming weathering at Buruktal in the Mesozoic age group. What that dates is the weathering that made the deposit, not the ultramafic parent rock it formed on.
- temporal basis: Age group of the laterite-forming weathering processes, as the compilation enumerates them.
- precision note: A group, not a date. The compilation offers three periods and assigns each deposit to one; no geochronology follows from it.
- assertion basis: SOURCE_REPORTED
Evidence support: Supported by the cited evidence · 2 sources, single source
Evidence: V.I. 2011 · Primary authority