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The Sant Llorenc del Munt fan-delta succession forms a clastic wedge (ca. 3My duration) that built out into the NE Ebro Basin in response to transpression and uplift along the Paleogene Catalan Coastal Range. This fan-delta succession is arranged in a series of transgressive-regressive sequences of different scales. A large-scale composite megasequence (the Milany megasequence) includes the whole...
The effects of high rates of subsidence and sediment supply, associated with orogenic uplift and loading, on the sequence-stratigraphic organization of two Middle Eocene, fan-delta clastic wedges on a foreland basin margin are highlighted. Specific topics addressed are: (1) the relevance of different key stratigraphic surfaces to the development of basic depositional cycles or sequences; (2) the stacking...
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