Superposition of different stress orientations in the western sector of the northern Apennines (Italy) |
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Authors: | Email author" target="_blank">E?EvaEmail author G?Ferretti S?Solarino |
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Institution: | (1) Istituto Nazionale di Geofisica e Vulcanologia, Via di Vigna Murata 605, 00143 Roma, Italy;(2) Dipartimento per lo Studio del Territorio e delle sue Risorse, Università di Genova, Viale Benedetto XV, 5, 16132 Genova, Italy |
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Abstract: | Previous studies of the stress regime in the northern Apennines report compression in the outer sector and extension in the
inner sector. In this study we focus on the relationships between the two regimes and, by making use of 54 focal mechanism
solutions, we try to shed some more light on a tectonic setting that appears more complex than the previous models. The focal
mechanisms, computed using the first onset technique, are inverted for stress parameters. The method applied requires subdividing
the volume to be investigated into homogeneous sectors: to comply with the complexity of the area under study, we included
depth as a parameter for sub-zoning. Our results show that the shallow regime (0–10 km of depth) is transtensive even in the
sector previously reported to be compressive. In fact, at a shallow depth, very few thrust focal solutions lie in a spatially
limited sector in the eastern part of the area under study. Just below 10 km in depth, the stress regime converts to transpressional:
stress axes are approximately inverted. Deeper than 45 km, thrust solutions are found. They are not numerous enough to perform
an inversion but indicate the existence of a compressional regime at depth. It is worth noting that a gap of seismicity is
observed in the layer 30–45 km. |
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Keywords: | fault plane solution (FPS) northern Apennines seismicity seismotectonic stress distribution |
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