HAL (France)
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Long‐Term Tectono‐Stratigraphic Evolution of a Propagating Rift System, L’Aquila Intermontane Basin (Central Apennines)
Understanding the long‐term tectono‐stratigraphic evolution of active extensional faulting is crucial for unraveling the mode through which continental rifting propagates in space and time. The Pliocene‐Quaternary L’Aquila Intermontane Basin (AIB) in central Apennines offers a natural laboratory for
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