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| Phân tích sự lún lòng chậu× | Định tuổi địa thời học× | |
|---|---|---|
| Lĩnh vực | Khoa học Trái Đất | Khoa học Trái Đất |
| Họ | Process / pipeline | Process / pipeline |
| Năm ra đời≠ | 1978 | 1902 |
| Người khởi xướng≠ | McKenzie and Sclater | Ernest Rutherford and Frederick Soddy |
| Loại≠ | tectono-sedimentary analysis pipeline | temporal constraint pipeline |
| Công trình gốc≠ | 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 ↗ | Dickin, A. P. (2005). Radiogenic Isotope Geology (2nd ed.). Cambridge University Press. DOI ↗ |
| Tên gọi khác | tectonic subsidence, backstripping, thermal history analysis | radiometric dating, isotopic dating, age determination |
| Liên quan≠ | 4 | 3 |
| Tóm tắt≠ | 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. | 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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