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The tectonic puzzle of the Messina area (Southern Italy): Insights from new seismic reflection data

机译:墨西拿地区(意大利南部)的构造难题:来自新地震反射数据的见解

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The Messina Strait, that separates peninsular Italy from Sicily, is one of the most seismically active areas of the Mediterranean. The structure and seismotectonic setting of the region are poorly understood, although the area is highly populated and important infrastructures are planned there. New seismic reflection data have identified a number of faults, as well as a crustal scale NE-trending anticline few km north of the strait. These features are interpreted as due to active right-lateral transpression along the north-eastern Sicilian offshore, coexisting with extensional and right-lateral transtensional tectonics in the southern Messina Strait. This complex tectonic network appears to be controlled by independent and overlapping tectonic settings, due to the presence of a diffuse transfer zone between the SE-ward retreating Calabria subduction zone relative to slab advance in the western Sicilian side.. ? 2012 Macmillan Publishers Limited. All rights reserved
机译:墨西拿海峡将意大利半岛与西西里岛分隔开来,是地中海地震最活跃的地区之一。尽管该地区人口稠密,并且计划在该地区规划重要基础设施,但对该地区的结构和地震构造背景了解甚少。新的地震反射数据已经确定了许多断层,以及海峡以北数公里处的地壳尺度的东北向背斜。这些特征被解释为是由于西西里东北部近海沿岸活跃的右倾作用,与墨西拿海峡南部的伸展和右倾伸展构造共存。这种复杂的构造网络似乎受独立和重叠的构造环境控制,这是由于在西西里西侧向东南退缩的卡拉布里亚俯冲带相对于板前移之间存在着一个扩散转移带。 2012 Macmillan Publishers Limited。版权所有

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