Formation and Persistence of Extensional Internally Drained Basins: The Case of the Fucino Basin (Central Apennines, Italy)
Résumé
Role of tectonics and drainage systems in the evolution of extensional basins Extensional fault network and sedimentary loading keep the Fucino Basin internally drained during its evolution. Sediment load contributes to incrementing of max 30% the faults total geological throw and locally reorganizes the stress field.
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