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Morphotectonic map of the Aventino-Lower Sangro valley (Abruzzo, Italy), scale 1:50,000

机译:Aventino-Lower Sangro山谷(意大利阿布鲁佐)的形态构造图,比例为1:50,000

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This work presents the Morphotectonic map of the Aventino-Lower Sangro valley, located in the southern Abruzzi area, and extending from the Apennines chain to the eastern piedmont, from the Maiella Mountain to the Adriatic coast. It is the result of an extensive drainage basin scale geomorphological analysis carried out in the Abruzzi area and incorporates four main sections: orography and hydrography (upper right on the map); morphotectonic section (centre and left on the map); quaternary fluvial deposits and terraces section (right on the map) and the long morphotectonic profile (lower right on the map). The map presented in this work provides a basis for the recognition of morphotectonic features at basin scale, the detection of tectonic control on landscape, and the reconstruction of paleo-landscapes. It contributes to defining the main phases of the post-orogenic landscape evolution of the transition zone between the Apennines chain and the eastern piedmont area, resulting from the combination of alternating morphotectonics and surface processes, due to rock uplift processes, local tectonics and slope and fluvial processes.
机译:该作品展示了位于阿布鲁佐南部地区,从亚平宁山脉到东部山麓,从迈耶拉山到亚得里亚海海岸的阿文蒂诺-下桑格罗山谷的形态构造图。它是在阿布鲁齐地区进行的大规模流域规模地貌分析的结果,它包括四个主要部分:地形学和水文学(在地图右上方);构造剖面(中心和地图左侧);第四纪河流沉积和阶地剖面(在地图上右侧)和长构造构造剖面(在地图上右下方)。这项工作中提供的地图为盆地规模上的构造特征的识别,景观构造控制的检测以及古景观的重建提供了基础。它有助于确定亚平宁山脉链与东部山前地区之间过渡带的造山后景观演化的主要阶段,这是由于岩石隆升过程,局部构造,斜坡和坡向的交替构造和地貌过程的结合而产生的。河流过程。

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