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Analiza paleomagnetizma×Analiza sleganja basena×
OblastGeonaukeGeonauke
PorodicaProcess / pipelineProcess / pipeline
Godina nastanka19061978
TvoracBernard Brunhes and Motonori MatuyamaMcKenzie and Sclater
Tiptemporal constraint pipelinetectono-sedimentary analysis pipeline
Temeljni izvorButler, R. F. (1992). Paleomagnetism: Magnetic Domains to Geologic Terranes. Blackwell Scientific Publications. link ↗Sclater, J. G., & Christie, P. A. F. (1980). Continental stretching: An explanation of the post-mid-Cretaceous subsidence of the Central North Sea Basin. Journal of Geophysical Research, 85(B7), 3711–3739. DOI ↗
Drugi nazivipaleomagnetic dating, magnetostratigraphy, paleomagnetic remanencetectonic subsidence, backstripping, thermal history analysis
Srodne34
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.Basin subsidence analysis is the quantitative study of how sedimentary basins deepen over geological time, driven by tectonics, isostasy, and load. Formalized by McKenzie (1978) and Sclater and Christie (1980), this method reveals the mechanical causes of basin development, predicts subsurface temperature and pressure histories, and constrains petroleum generation. Analysis integrates well stratigraphy, seismic geometry, gravity data, and thermal models to reconstruct basin evolution.
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ScholarGateUporedite metode: Paleomagnetism Analysis · Basin Subsidence Analysis. Preuzeto 2026-06-18 sa https://scholargate.app/sr/compare