Zobrazeno 1 - 9
of 9
pro vyhledávání: '"Nicolò Bertone"'
Autor:
Lorenzo Bonini, Nicolò Bertone
During the last decades, analog models have taken extraordinary advantage of new technologies. High-resolution cameras, analytical methods to extract quantitative data from the experiments (e.g., Digital Image Correlation), and new analog materials a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a89a3027dc70c28d78db377e7ffa0b00
https://doi.org/10.5194/egusphere-egu23-6125
https://doi.org/10.5194/egusphere-egu23-6125
Autor:
Michelle Vattovaz, Nicolò Bertone, Claudia Bertoni, Lorenzo Bonini, Angelo Camerlenghi, Anna Del Ben, Richard Walker
The eastern Mediterranean has been the locus of catastrophic earthquakes and related tsunamis (e.g., the 365 Crete and 1222 Cyprus earthquakes). The primary sources of these seismic events are structures related to the subduction of the Nubian Plate
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8189db04165d4b59e3ff08aabea5ce24
https://doi.org/10.5194/egusphere-egu23-7674
https://doi.org/10.5194/egusphere-egu23-7674
Autor:
Lorenzo Bonini, Umberto Fracassi, Nicolò Bertone, Francesco Emanuele Maesano, Gianluca Valensise, Roberto Basili
The development of structurally controlled basins is frequently dominated by inherited geological and tectonic structures, especially when the affected region has undergone multiple tectonic phases. In this study we use physically scaled analog model
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e150c3785a3b52e8c74bc350da968cef
https://hdl.handle.net/11368/3041778
https://hdl.handle.net/11368/3041778
Autor:
Nicolò Bertone, Lorenzo Bonini, Eugenia Colin, Anna Del Ben, Giuseppe Brancatelli, Angelo Camerlenghi, Edy Forlin, Gian Andrea Pini
The eastern Mediterranean is shaped by the interaction between the African, Arabian, and Eurasian plates resulting in a complex tectonic framework. The Hellenic subduction is well documented and studied but, the northeast corner of the eastern Medite
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::85fa266f774e8e7c8ce994e406dc14ab
https://doi.org/10.5194/egusphere-egu22-8675
https://doi.org/10.5194/egusphere-egu22-8675
Autor:
Edy Forlin, Giuseppe Brancatelli, Dirk Klaeschen, Anna Del Ben, Gian Andrea Pini, Lorenzo Bonini, Nicolò Bertone, Angelo Camerlenghi
The present‐day tectonic setting of the Eastern Mediterranean Sea results from a long deformation history, characterized by an alternation of extensional and contractional phases: from Mesozoic rifting to Late Cretaceous-present-day compression. Th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cb5fa5ab09d1f8bf53cde47abafbb3bf
https://doi.org/10.5194/egusphere-egu21-12428
https://doi.org/10.5194/egusphere-egu21-12428
Nowadays depth imaging of seismic data, using different migration schemes (rays tracing or waves equation methods) and different techniques for velocity model building (i.e. grid or layer-based tomography, isotropic or anisotropic velocity field) is
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::74c19ee01586286cd83f7f862a92ea61
https://doi.org/10.5194/egusphere-egu2020-7164
https://doi.org/10.5194/egusphere-egu2020-7164
Autor:
Nicolò Bertone, Roberto Basili, Gianluca Valensise, Umberto Fracassi, Lorenzo Bonini, Francesco Emanuele Maesano
Most of the present-day extensional systems formed in areas that already experienced an older phase of tectonic activity. Therefore, understanding how a pre-existing structural setting may affect the development of an extensional basin is a crucial i
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bb270fe53b66194ee03fa29226f94c32
https://doi.org/10.5194/egusphere-egu2020-8516
https://doi.org/10.5194/egusphere-egu2020-8516
Autor:
Nicolò Bertone, Gian Andrea Pini, Lorenzo Bonini, Francesco Emanuele Maesano, Anna Del Ben, Mara Monica Tiberti, Roberto Basili
Tear faults are common structures in subduction zones, especially at slab edges, where they origin from differential forces applied to a subducting slab in areas close to the trench. Presence and geometry of tears have been sometimes inferred from ba
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4966d2373718162847e61b87551ecf66
https://meetingorganizer.copernicus.org/EGU2020/EGU2020-7608.html
https://meetingorganizer.copernicus.org/EGU2020/EGU2020-7608.html