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Палеомагнитный анализ×Геохронологическое датирование×
ОбластьНауки о ЗемлеНауки о Земле
СемействоProcess / pipelineProcess / pipeline
Год появления19061902
Автор методаBernard Brunhes and Motonori MatuyamaErnest Rutherford and Frederick Soddy
Типtemporal constraint pipelinetemporal constraint pipeline
Основополагающий источникButler, R. F. (1992). Paleomagnetism: Magnetic Domains to Geologic Terranes. Blackwell Scientific Publications. link ↗Dickin, A. P. (2005). Radiogenic Isotope Geology (2nd ed.). Cambridge University Press. DOI ↗
Другие названияpaleomagnetic dating, magnetostratigraphy, paleomagnetic remanenceradiometric dating, isotopic dating, age determination
Связанные33
СводкаPaleomagnetism 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.Geochronological 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.
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ScholarGateСравнение методов: Paleomagnetism Analysis · Geochronological Dating. Получено 2026-06-19 из https://scholargate.app/ru/compare