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Masena spektrometrija izotopnih omjera×Radiokarbonsko datiranje×
PodručjeGeofizikaGeofizika
ObiteljProcess / pipelineProcess / pipeline
Godina nastanka19941949
TvoracThomas Coplen and othersWillard Libby
VrstaMeasurement of stable and radiogenic isotope ratiosChronometric method based on ¹⁴C decay
Temeljni izvorCoplen, T. B. (1994). Reporting of stable hydrogen, carbon, and oxygen isotopic abundances. Pure and Applied Chemistry, 66(2), 273-276. DOI ↗Libby, W. F. (1949). Radiocarbon dating. University of Chicago Press. link ↗
Drugi naziviIRMS¹⁴C dating, Carbon-14 dating
Srodne33
SažetakIsotope Ratio Mass Spectrometry (IRMS) is an analytical technique that measures the relative abundance of stable isotopes (H, C, N, O, S) and some radiogenic isotopes (e.g., ⁸⁷Sr/⁸⁶Sr) in samples with high precision. Standardized by Coplen and colleagues, IRMS enables paleoclimate reconstruction, source tracing (diet, water origin), geochemical fingerprinting, and age dating through radiogenic isotopes.Radiocarbon dating is a radiometric technique that determines the age of organic materials by measuring the radioactive decay of ¹⁴C (carbon-14), a rare isotope produced in the atmosphere by cosmic ray interactions. Developed by Willard Libby in 1949, radiocarbon dating became a foundational method in archaeology, paleoclimate studies, and geology, enabling dating of organic materials from the past ~50,000 years with typical precision of ±50–100 years.
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ScholarGateUsporedite metode: Isotope Ratio Mass Spectrometry · Radiocarbon Dating. Preuzeto 2026-06-20 s https://scholargate.app/hr/compare