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Geological map of the Tellaro River Valley (Hyblean Foreland, southeastern Sicily, Italy)

机译:泰拉罗河谷(Hyblean Foreland,意大利西西里岛东南部)的地质图

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The Geological map of the Tellaro River Valley, at the 1:25.000 scale, portrays the main stratigraphic and structural features that developed in a 300?km~(2) wide area of the African foreland in southeastern Sicily (Hyblean Foreland). The NW-SE-oriented Tellaro River Valley marks the transition between the eastern (Siracusa Plateau) and western (Ragusa Plateau) domains of the foreland, where a post-Tortonian structural depression, here designated as Tellaro Basin, originated. The map pictures the geometry and kinematics of the border faults and the structure affecting the basin infilling. The mapped structural pattern denounces a poliphase tectonic evolution of the region, suggesting the occurrence of a major NW-SE-oriented crustal discontinuity that, being active during the different periods of the post-Tortonian evolution of the area, could play a primary role also in the present seismotectonic picture.
机译:Tellaro河谷的地质图比例为1:25.000,描绘了西西里岛东南部(Hyblean Foreland)的非洲前陆300?km〜(2)宽阔区域中发育的主要地层和结构特征。西北偏南的泰拉罗河谷标志着前陆的东部(西拉库萨高原)和西部(拉古萨高原)之间的过渡,这里是托托尔后构造低陷的发源地,这里被称为泰拉罗盆地。该地图显示了边界断层的几何学和运动学以及影响盆地充填的结构。映射的结构模式谴责了该地区的一个政治阶段构造演化,表明发生了一个以西北西向东南为主的地壳不连续性,该地壳在该地区经历了后Tortonian演化的不同时期活跃,也可能起着主要作用。在目前的地震构造图中。

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