The interaction between sedimentation/erosion and faulting represents one of the most intriguing topics in landscape and tectonics evolution. Only few studies have been able to document the feedback between faulting and sedimentary loading from field observations. Here, we focus on how sediment loading/unloading influences the dynamics of fault systems in the Fucino basin, in the Central Apennines (Italy). The Fucino basin represents a remarkable case study with respect to the other main extensional basins in the Apennines because of its large dimension, square shape, significant sediment thickness, and its endorheic nature throughout its evolution.

中文翻译：

---

张性内干盆地的形成和持续存在：以 Fucino 盆地为例（意大利中部亚平宁山脉）

沉积/侵蚀和断层作用之间的相互作用是景观和构造演化中最有趣的话题之一。只有少数研究能够记录现场观测中断层和沉积载荷之间的反馈。在这里，我们关注沉积物装载/卸载如何影响中部亚平宁山脉（意大利）富奇诺盆地的断层系统动力学。Fucino 盆地代表了亚平宁山脉其他主要伸展盆地的非凡案例研究，因为它具有大尺寸、方形、显着的沉积物厚度以及在整个演化过程中的内陆性质。