構造地層學
構造地層學（英語：techtonostratigraphy）是指在逆衝構造區由推覆體堆疊的岩石層序，典型的例子為斯堪地那維亞的加里東岩（英語：Caledonides）。[1]沉積物通常能反應在同時的地質構造事件。[2]
參考文獻
[編輯]- ^ 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.