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,典型的例子為斯堪的納維亞的加里東岩(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
  1. ^ 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
  2. ^ 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.