Salīdzināt metodes
Apskatiet izvēlētās metodes blakus; rindas, kas atšķiras, ir izceltas.
| Izotopu masas spektrometrija× | Paleomagnētiskā analīze× | |
|---|---|---|
| Nozare | Ģeofizika | Ģeofizika |
| Saime | Process / pipeline | Process / pipeline |
| Izcelsmes gads≠ | 1994 | 1953 |
| Autors≠ | Thomas Coplen and others | Ronald Fisher and contributors |
| Tips≠ | Measurement of stable and radiogenic isotope ratios | Analysis of remnant magnetization in rocks for chronology and tectonics |
| Pirmavots≠ | Coplen, T. B. (1994). Reporting of stable hydrogen, carbon, and oxygen isotopic abundances. Pure and Applied Chemistry, 66(2), 273-276. DOI ↗ | Fisher, R. A. (1953). Dispersion on a sphere. Proceedings of the Royal Society of London, 217(1130), 295-305. DOI ↗ |
| Citi nosaukumi | IRMS | Paleomagnetism |
| Saistītās | 3 | 3 |
| Kopsavilkums≠ | Isotope Ratio Mass Spectrometry (IRMS) is an analytical technique that measures the relative abundance of stable isotopes (H, C, N, O, S) and some radiogenic isotopes (e.g., ⁸⁷Sr/⁸⁶Sr) in samples with high precision. Standardized by Coplen and colleagues, IRMS enables paleoclimate reconstruction, source tracing (diet, water origin), geochemical fingerprinting, and age dating through radiogenic isotopes. | Paleomagnetic analysis is the study of remnant magnetization in rocks and sediments to determine the direction and magnitude of the Earth's ancient magnetic field and to establish the ages and tectonic histories of crustal rocks. Formalized by Fisher (1953) and Butler (1992), paleomagnetism underpins plate tectonics plate reconstruction, magnetostratigraphic dating, and paleoclimate studies. |
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