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Analiza paleomagnetizma×Геохронолошко датирање×
OblastGeonaukeGeonauke
PorodicaProcess / pipelineProcess / pipeline
Godina nastanka19061902
TvoracBernard Brunhes and Motonori MatuyamaErnest Rutherford and Frederick Soddy
Tiptemporal constraint pipelinetemporal constraint pipeline
Temeljni izvorButler, 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 ↗
Drugi nazivipaleomagnetic dating, magnetostratigraphy, paleomagnetic remanenceradiometric dating, isotopic dating, age determination
Srodne33
SažetakPaleomagnetism 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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ScholarGateUporedite metode: Paleomagnetism Analysis · Geochronological Dating. Preuzeto 2026-06-19 sa https://scholargate.app/sr/compare