Search Results - "Todrani, Alessandro"
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Paleomagnetism of the Middle Cenozoic Mula Basin (East Tibet): Evidence for km‐Scale Crustal Blocks Rotated by Midlower Crust Drag
Published in Geochemistry, geophysics, geosystems : G3 (01-09-2020)“…Abstract Existing models describing continental crust deformation require the coexistence of strike‐slip faults and crustal blocks rotating between them,…”
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Magnetostratigraphy of the Niubao Formation in the Bangong‐Nujiang Suture Zone: Constraints on the Amount of Crustal Shortening of the Tibetan Plateau Since 60 Ma
Published in Geophysical research letters (28-10-2024)“…The Early Cenozoic sedimentary archives of Tibet are crucial for elucidating the geodynamic processes related to continental collision, particularly crustal…”
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Near-Source Simulation of Strong Ground Motion in Amatrice Downtown Including Site Effects
Published in Geosciences (Basel) (01-05-2021)“…On 24 August 2016, a Mw 6.0 earthquake started a damaging seismic sequence in central Italy. The historical center of Amatrice village reached the XI degree…”
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Reconstruction of the subaerial Holocene volcanic activity through paleomagnetic and 14C dating methods: El Hierro (Canary Islands)
Published in Journal of volcanology and geothermal research (01-05-2022)“…Volcanic hazard assessment relies on the accurate knowledge of the eruptive style and recurrence of volcanic eruptions in the past. At El Hierro (Canary…”
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Paleomagnetic results from the Early–Middle Jurassic rocks in the Tethyan Himalayas and tectonic implications
Published in Journal of Asian earth sciences (15-04-2024)“…[Display omitted] •In the Early–Middle Jurassic, the Tethyan Himalayas was located at 18.9° ± 4.3°S.•The paleolatitude of the Tethyan Himalayas is consistent…”
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Tephra and cryptotephra in a ~ 60,000-year-old lacustrine sequence from the Fucino Basin: new insights into the major explosive events in Italy
Published in Bulletin of volcanology (01-03-2018)“…Two cores were sampled in the Fucino Basin (central Apennines, Italy), which represents an extensional intramountain basin filled by Pliocene to Quaternary…”
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