Linked from

The 39 pages that link to Geochronology, each with the reason it gives.

• PaleogeographyRelated: Reliable ages place reconstructed coastlines and landmasses at specific times.

• GeothermobarometryRelated: It supplies timing that pressure–temperature estimates alone cannot establish.

• Pilbara CratonRelated: Radiometric dating establishes the timing of Pilbara crust formation and later events.

• UnconformityRelated: Dating rocks on either side can constrain, but not directly fill, the missing interval.

• HadeanRelated: Hadean chronology depends on dating scattered mineral and meteorite evidence.

• Potassium-40Related: Potassium-40 dating helps place volcanic rocks and geological events on an absolute timescale.

• PetrologyRelated: Minerals in rocks can preserve dates that anchor their formation histories.

• Geological mapRelated: Age measurements help establish the sequence and labels of mapped rock units.

• Global Boundary Stratotype Section and PointRelated: Numerical dating complements the relative time boundary fixed by a GSSP.

• Dresser FormationRelated: Radiometric dating underpins estimates of the formation’s age and its place in Earth history.

• Huronian glaciationRelated: Improved dating could resolve how many glacial episodes occurred and how they aligned with oxygenation.

• Igneous intrusionRelated: Minerals crystallized in intrusions can date magma emplacement and related events.

• History of EarthRelated: It supplies the dates that turn a sequence into a timed history.

• Geological history of EarthRelated: Dating methods assign ages to events in the geological record.

• Geologic recordRelated: It assigns numerical ages to evidence whose order stratigraphy establishes.

• PaleocontinentRelated: Dating records establishes when paleocontinents formed, collided, or fragmented.

• Terra Australis OrogenRelated: Dating separates the belt’s prolonged episodes of magmatism and deformation.