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- W105573575 abstract "The Ubierna fault is a major structure in the southern margin of the Cantabrian Basin. It controlled the subsidence during the intra-Mesozoic extensional event allow ing the deposit of progressively to the north thicker syn-rift Upper Jurassic-Lower Cretaceous sediments in the Polients trough. Later it was inverted as a reverse fault during the main Tertiary compression changing to a strike-slip behaviour in the latest compressive movements." @default.
- W105573575 created "2016-06-24" @default.
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- W105573575 date "1994-01-01" @default.
- W105573575 modified "2023-09-24" @default.
- W105573575 title "La falla de Ubierna (margen SO de la cuenca Cantábrica)." @default.
- W105573575 hasPublicationYear "1994" @default.
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