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LITHOEN

Geological region

Superior Province

Also known as Superior Craton

A large Archean craton of central and eastern Canada, made of granite-greenstone terrains including the Bird River and Sachigo greenstone belts. It is the largest area of Archean crust exposed on Earth.

Classification

region kind
craton
domain realm
northAmerica

How this record is known

1
Settled consensus
Cited as the accepted position of the discipline.
3
Interpretation
Reached by reasoning from evidence, or produced by a named model.

4 of 4 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.

InferredA drawn boundary may be observed, inferred, conventional or model-defined — and looks identical either way.

General principle, shown here for context — not an observation about this record.

Most geological boundaries are interpretations rather than observations. A line on a geological map may be a contact somebody walked, a change inferred from geophysics beneath cover, a gradation over tens of kilometres drawn where a convention says to draw it, or a model boundary that exists because the model needs one. These are not equally well known, and a map drawn at one line width cannot tell them apart.

  • method: Follows from the retrieved sources: PB2002 states that a boundary class may change along a single segment, and the chromite model places cratons and their margins by describing intrusions rather than by delimiting the cratons.
  • precision note: Lithoen therefore stores boundary certainty on each geometry, with GRADATIONAL and CONCEALED as available values, and refuses to publish a geometry that does not state one.
  • generality: GENERAL_PRINCIPLE

Evidence support: Supported by the cited evidence 2 sources, multiple sources, independence unknown

Evidence: Bird 2003 Primary authority; Schulte 2012 Primary authority

InferredTopography now and deformation then are different things, and neither implies the other.

A mountain range is present-day topography. An orogenic belt is crust that was deformed, thickened and commonly metamorphosed during a mountain-building episode, and it may have no topography left at all. The Superior Province preserves Archean crust that was once mountainous and is now flat; the reverse also occurs, where relief has causes other than orogeny.

  • method: Follows from the sources: PB2002’s subduction criteria explicitly exclude the Alps, Zagros, Pamirs, Himalaya, Tien Shan and Taiwan — all major mountain ranges — showing that relief and boundary process are separately determined.
  • precision note: Lithoen keeps MountainRange and GeologicalRegion as separate entity types for this reason and does not equate any pair of them.

Evidence support: Supported by the cited evidence 2 sources, multiple sources, independence unknown

Evidence: Schulte 2012 Primary authority; Bird 2003 Primary authority

InferredSpatial intersection is never evidence of a geological relationship.

General principle, shown here for context — not an observation about this record.

Two mapped regions overlapping is a fact about two polygons. That one region formed the other, reworked it, or hosts anything within it is a fact about the Earth, and needs evidence. Lithoen keeps computational spatial predicates in a separate vocabulary from its geological relations, and derives none of the second from the first.

  • method: Follows from how the retrieved sources establish regional relationships: by dating, by structural continuity and by rock associations, never by observing that two areas overlap on a map.
  • precision note: Enforced in code: SPATIAL_PREDICATES is a separate vocabulary from RELATION_TYPES, and no validator or projection promotes one into the other.
  • generality: GENERAL_PRINCIPLE

Evidence support: Supported by the cited evidence 2 sources, multiple sources, independence unknown

Evidence: Schulte 2012 Primary authority; Leach 2010 Primary authority

EstablishedArchean granite-greenstone terrains, some of them found by aeromagnetic survey.

The Superior Province of Canada contains Archean granite-greenstone terrains. The USGS chromite model places the Bird River Sill in the Archean supracrustal rocks of the Bird River greenstone belt in Manitoba, and the magmatic nickel model places a ring of mafic to ultramafic intrusions within the Sachigo greenstone belt, detected as a semicircular ring of magnetic highs in a regional aeromagnetic survey.

  • method: Surface mapping for the Bird River belt; regional aeromagnetic survey for the Sachigo intrusions, which were found as a magnetic pattern before they were understood as a geological one.

Evidence support: Supported by the cited evidence 2 sources, multiple sources, independence unknown

Evidence: Schulte 2012 Primary authority; Schulz 2014 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.