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Геохронологическое датирование×Палеомагнитный анализ×
ОбластьНауки о ЗемлеНауки о Земле
СемействоProcess / pipelineProcess / pipeline
Год появления19021906
Автор методаErnest Rutherford and Frederick SoddyBernard Brunhes and Motonori Matuyama
Типtemporal constraint pipelinetemporal constraint pipeline
Основополагающий источникDickin, A. P. (2005). Radiogenic Isotope Geology (2nd ed.). Cambridge University Press. DOI ↗Butler, R. F. (1992). Paleomagnetism: Magnetic Domains to Geologic Terranes. Blackwell Scientific Publications. link ↗
Другие названияradiometric dating, isotopic dating, age determinationpaleomagnetic dating, magnetostratigraphy, paleomagnetic remanence
Связанные33
СводкаGeochronological dating is the determination of absolute ages of rocks and minerals using the decay of radioactive isotopes. Pioneered by Rutherford and Soddy (1902), this method provides numerical anchors for geological timescales and enables quantitative understanding of geological processes. Modern techniques (K-Ar, Rb-Sr, U-Pb, 40Ar/39Ar) span from recent to ancient events and are essential for calibrating relative chronologies and assessing rates of geological change.Paleomagnetism analysis is the study of ancient magnetic properties of rocks, measuring fossil magnetization to determine paleomagnetic field history and assign geological ages. Pioneered by Brunhes (1906) and systematized by Tauxe (2010), this method reveals geomagnetic reversals, polar wander paths, and paleomagnetic chronology independent of fossil biostratigraphy. Analysis integrates laboratory rock magnetism with field sampling to build high-resolution timescales and constrain plate motion.
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ScholarGateСравнение методов: Geochronological Dating · Paleomagnetism Analysis. Получено 2026-06-20 из https://scholargate.app/ru/compare