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- Q3661541 subject Q8621270.
- Q3661541 abstract "Thermochronology is the study of the thermal evolution of a region of a planet. Thermochronologists use radiometric dating along with the closure temperatures that represent the temperature of the mineral being studied at the time given by the date recorded, to understand the thermal history of a specific rock, mineral, or geologic unit. It is a subfield within geology, and is closely associated with geochronology.A typical thermochronological study will involve the dates of a number of rock samples from different areas in a region, often from a vertical transect along a steep canyon, cliff face, or slope. These samples are then dated. With some knowledge of the subsurface thermal structure, these dates are translated into depths and times at which that particular sample was at the mineral's closure temperature. If the rock is today at the surface, this process gives the exhumation rate of the rock.Common isotopic systems used for thermochronology include fission track dating in zircon and apatite, potassium-argon and argon-argon dating in apatite, uranium-thorium-helium dating in zircon and apatite, and 4He/3He dating.".
- Q3661541 wikiPageWikiLink Q1068405.
- Q3661541 wikiPageWikiLink Q1069.
- Q3661541 wikiPageWikiLink Q1420956.
- Q3661541 wikiPageWikiLink Q178397.
- Q3661541 wikiPageWikiLink Q178928.
- Q3661541 wikiPageWikiLink Q213891.
- Q3661541 wikiPageWikiLink Q214753.
- Q3661541 wikiPageWikiLink Q331055.
- Q3661541 wikiPageWikiLink Q4789695.
- Q3661541 wikiPageWikiLink Q5135533.
- Q3661541 wikiPageWikiLink Q8621270.
- Q3661541 comment "Thermochronology is the study of the thermal evolution of a region of a planet. Thermochronologists use radiometric dating along with the closure temperatures that represent the temperature of the mineral being studied at the time given by the date recorded, to understand the thermal history of a specific rock, mineral, or geologic unit.".
- Q3661541 label "Thermochronology".