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Paleomagnetická analýza×Rádiouhlíková metóda×
OdborGeofyzikaGeofyzika
RodinaProcess / pipelineProcess / pipeline
Rok vzniku19531949
TvorcaRonald Fisher and contributorsWillard Libby
TypAnalysis of remnant magnetization in rocks for chronology and tectonicsChronometric method based on ¹⁴C decay
Pôvodný zdrojFisher, R. A. (1953). Dispersion on a sphere. Proceedings of the Royal Society of London, 217(1130), 295-305. DOI ↗Libby, W. F. (1949). Radiocarbon dating. University of Chicago Press. link ↗
Ďalšie názvyPaleomagnetism¹⁴C dating, Carbon-14 dating
Príbuzné33
ZhrnutiePaleomagnetic analysis is the study of remnant magnetization in rocks and sediments to determine the direction and magnitude of the Earth's ancient magnetic field and to establish the ages and tectonic histories of crustal rocks. Formalized by Fisher (1953) and Butler (1992), paleomagnetism underpins plate tectonics plate reconstruction, magnetostratigraphic dating, and paleoclimate studies.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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ScholarGatePorovnať metódy: Paleomagnetic Analysis · Radiocarbon Dating. Získané 2026-06-19 z https://scholargate.app/sk/compare