Palabras en English para 'Relating to, or dated using radiocarbon'
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- a chemical analysis used to determine the age of organic materials based on their content of the radioisotope carbon 14; believed to be reliable up to 40,000 years
- (physics, archaeology, paleontology) A method of estimating the age of an artifact or biological vestige based on the relative amounts of the different isotopes of carbon present in a sample.
noun
- (geology, geochronology) Any of several techniques used to measure the age of rock, especially any technique of radiometric dating, the measuring of the relative abundance of particular radioactive or radiogenic isotopes in order to evaluate the progress of radioactive decay.
- Any of several crystalline minerals that remain stable over geologic time and that when formed contained radioisotopes whose abundance relative to their decay products can be measured to calculate the age of the crystal (and thus that of the surrounding rock).
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- Initialism of to be dated.
- Initialism of to be deducted.
- Initialism of to be declared.
- Initialism of to be decided.
- Initialism of to be developed.
- Initialism of to be discovered.
- Initialism of to be done.
- Initialism of to be destroyed.
- Initialism of to be disclosed.
- Initialism of to be delivered.
- Initialism of to be derived.
- Initialism of to be discussed.
- Initialism of to be defined.
- Initialism of to be documented.
- Initialism of to be determined.
- Initialism of to be designed.
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noun
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- a chemical analysis used to determine the age of organic materials based on their content of the radioisotope carbon 14; believed to be reliable up to 40,000 years
- (physics, archaeology, paleontology) A method of estimating the age of an artifact or biological vestige based on the relative amounts of the different isotopes of carbon present in a sample.
noun
- (geology, geochronology) Any of several techniques used to measure the age of rock, especially any technique of radiometric dating, the measuring of the relative abundance of particular radioactive or radiogenic isotopes in order to evaluate the progress of radioactive decay.
- Any of several crystalline minerals that remain stable over geologic time and that when formed contained radioisotopes whose abundance relative to their decay products can be measured to calculate the age of the crystal (and thus that of the surrounding rock).