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Geochronologické datovanie×Analýza poklesu panvy×
OdborVedy o ZemiVedy o Zemi
RodinaProcess / pipelineProcess / pipeline
Rok vzniku19021978
TvorcaErnest Rutherford and Frederick SoddyMcKenzie and Sclater
Typtemporal constraint pipelinetectono-sedimentary analysis pipeline
Pôvodný zdrojDickin, A. P. (2005). Radiogenic Isotope Geology (2nd ed.). Cambridge University Press. DOI ↗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 ↗
Ďalšie názvyradiometric dating, isotopic dating, age determinationtectonic subsidence, backstripping, thermal history analysis
Príbuzné34
ZhrnutieGeochronological 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.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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ScholarGatePorovnať metódy: Geochronological Dating · Basin Subsidence Analysis. Získané 2026-06-20 z https://scholargate.app/sk/compare