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Paleomagnetismin analyysi×Geokronologinen ajoitus×
TieteenalaGeotieteetGeotieteet
MenetelmäperheProcess / pipelineProcess / pipeline
Syntyvuosi19061902
KehittäjäBernard Brunhes and Motonori MatuyamaErnest Rutherford and Frederick Soddy
Tyyppitemporal constraint pipelinetemporal constraint pipeline
AlkuperäislähdeButler, 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 ↗
Rinnakkaisnimetpaleomagnetic dating, magnetostratigraphy, paleomagnetic remanenceradiometric dating, isotopic dating, age determination
Liittyvät33
TiivistelmäPaleomagnetism 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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ScholarGateVertaile menetelmiä: Paleomagnetism Analysis · Geochronological Dating. Haettu 2026-06-19 osoitteesta https://scholargate.app/fi/compare