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构造地层学

维基百科,自由的百科全书

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

  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.