Linganisha mbinu
Pitia mbinu ulizochagua bega kwa bega; safu zinazotofautiana zinaangaziwa.
| Isotope Ratio Mass Spectrometry× | Uchambuzi wa Paleomagnetiki× | |
|---|---|---|
| Nyanja | Jiofizikia | Jiofizikia |
| Familia | Process / pipeline | Process / pipeline |
| Mwaka wa asili≠ | 1994 | 1953 |
| Mwanzilishi≠ | Thomas Coplen and others | Ronald Fisher and contributors |
| Aina≠ | Measurement of stable and radiogenic isotope ratios | Analysis of remnant magnetization in rocks for chronology and tectonics |
| Chanzo asilia≠ | 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 ↗ |
| Majina mbadala | IRMS | Paleomagnetism |
| Zinazohusiana | 3 | 3 |
| Muhtasari≠ | 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. |
| ScholarGateSeti ya data ↗ |
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