方法证据记录
Basin Subsidence Analysis
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.
源记录
引文逐字复制自方法源记录。这些引文不代表任何层级的验证。
Basin Subsidence Analysis
分类方法记录 · process-pipeline / geoscience
- 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 10.1029/JB085iB07p03711
- Allen, P. A., & Allen, J. R. (1995). Geology of Deltas. Ellis Horwood Limited. · URL
- McKenzie, D. (1978). Some remarks on the development of sedimentary basins. Earth and Planetary Science Letters, 40(1), 25–32. · DOI 10.1016/0012-821X(78)90071-7
精选声明
声明已持久化到证据分类账中,每个声明都有自己的评估。
尚无精选声明
当分类账中没有声明时,此视图不会自行创建声明评估。
相关方法
从方法图中生成,显示为机器建议的关系 — 不推断任何证据声明。