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The course objective is to demonstrate the evolution from continental through shallow marine to slope and submarine fan sedimentation during formation of a foreland basin with syntectonic sedimentation in adjacent but sequential sub-basins associated with evolving thrust fronts during the Pyrenean orogeny.
Starting and finishing in Barcelona, the following basins are visited in turn: the Upper Palaeocene-Lower Eocene Ager Basin; the Eocene Tremp-Grauss and Ainsa Basins; Upper Eocene-Oligocene Jaco Basin; and finally the Oligo-Miocene Ebro Basin. Impressive panoramic views are available of the various sedimentary sequences to be observed in detail. Large-scale tectonic elements that controlled the sedimentation are evident. The clastic dominated sequences essentially record the westwards deepening and progressively marine influenced foreland basin evolving as the Pyrenean range developed from Eocene onwards, although the more southerly and younger Ebro Basin succession is spectacularly dominated by alluvial fan and fluvial sediments.
Course bases: Barcelona, Tremp, Grauss, Ainsa, Broto, Barcelona.
Petroleum geologists, geophysicists, reservoir engineers, sedimentologists, stratigraphers
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