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Massimiliano Rinaldo Barchi

Researcher at University of Perugia

Publications -  114
Citations -  4042

Massimiliano Rinaldo Barchi is an academic researcher from University of Perugia. The author has contributed to research in topics: Fault (geology) & Active fault. The author has an hindex of 31, co-authored 109 publications receiving 3587 citations. Previous affiliations of Massimiliano Rinaldo Barchi include National Institute of Geophysics and Volcanology.

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Aftershocks driven by a high-pressure CO2 source at depth.

TL;DR: It is proposed that aftershocks of large earthquakes in such geologic environments may be driven by the coseismic release of trapped, high-pressure fluids propagating through damaged zones created by the mainshock, which may provide a link between earthquakes, aftershock, crust/mantle degassing and earthquake-triggered large-scale fluid flow.
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Seismotectonic zoning in east-central Italy deduced from an analysis of the Neogene to present deformations and related stress fields

TL;DR: In this article, the space-time evolution of the late Miocene to present contractional and extensional deformations within east-central Italy, with an analysis of the pattern and orientation of the related stress field, an insight into the cover-basement relations, and a discussion of the seismotectonic implications.
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A low-angle normal fault in the Umbria region (Central Italy): a mechanical model for the related microseismicity

TL;DR: In this article, the geometry of the Altotiberina Fault (ATF) was reconstructed matching surface geology with seismic reflection profiles and borehole data, and the fault can be reactivated for low values of differential stress ( σ 1 − σ 3 T ∼10 MPa).
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The crustal structure of the northern apennines (Central Italy): An insight by the crop03 seismic line

TL;DR: In this article, the CROP03-deep seismic reflection profile in the Northern Apennines is described and re-considered in light of new geophysical data and interpretations made available in the last five years.
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The development and behaviour of low-angle normal faults during Cenozoic asymmetric extension in the Northern Apennines, Italy

TL;DR: In this article, the authors investigated three normal fault systems active at distinct times during the regional extension of the Northern Apennines, with each showing different degrees of crustal exhumation.