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The Basque-Cantabrian basin of northern Spain was formed by Mesozoic extension of the North Atlantic margins and opening of the Bay of Biscay. The preorogenic history of the basin included two phases of rifting (Early Triassic and Late Jurassic-Early Cretaceous), and two periods of relative quiescence and broad regional subsidence (Middle Triassic-Middle Jurassic and Late Cretaceous-early Tertiary).

The Aptian-Albian interval was characterized by an extensional structural pattern of troughs and highs related to major northwest-southeast fault lineaments. This structural pattern was dominated by a major left-lateral strike-slip system that reactivated Early Triassic structures, and can be related to opening...

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