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Análise Paleomagnética×Datação Geocronológica×
ÁreaGeociênciasGeociências
FamíliaProcess / pipelineProcess / pipeline
Ano de origem19061902
Autor originalBernard Brunhes and Motonori MatuyamaErnest Rutherford and Frederick Soddy
Tipotemporal constraint pipelinetemporal constraint pipeline
Fonte seminalButler, 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 ↗
Outros nomespaleomagnetic dating, magnetostratigraphy, paleomagnetic remanenceradiometric dating, isotopic dating, age determination
Relacionados33
ResumoPaleomagnetism 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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ScholarGateComparar métodos: Paleomagnetism Analysis · Geochronological Dating. Recuperado em 2026-06-19 de https://scholargate.app/pt/compare