构造地层学
构造地层学（英语：techtonostratigraphy）是指在逆冲构造区由推覆体堆叠的岩石层序，典型的例子为斯堪的纳维亚的加里东岩（英语：Caledonides）。[1]沉积物通常能反应在同时的地质构造事件。[2]
参考文献
[编辑]- ^ Roberts,D. & Gee,D. 1985. An introduction to the structure of the Scandinavian Caledonides. In Gee, D. G., and Sturt, B. A., eds. The Caledonide Orogen – Scandinavia and related areas.John Wiley and Sons, Chichester, 55–68
- ^ Jackson, C A L ,Gawthorpe, R L, Leppard, C W , Sharp, I R 2006. Rift-initiation development of normal fault blocks: insights from the Hammam Faraun fault block, Suez Rift, Egypt. Journal of the Geological Society, 163, 165–183.