作者: F. Roure , J. P. Brun , B. Colletta , R. Vially
DOI: 10.1007/978-3-642-78849-9_18
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摘要: Jurassic and Oligocene extensional structures are still well preserved in the compressional basin of southeastern France. Due to occurrence numerous potential decollement levels (i. e., Carboniferous coal measures, Triassic evaporites, blackshales, or Neocomian marls), these frequently independently involve crystalline basement sedimentary cover, thus illustrating various structural styles that clearly imaged seismic profiles.