Zobrazeno 1 - 10
of 45
pro vyhledávání: '"Luigi Passarelli"'
Publikováno v:
Nature Communications, Vol 15, Iss 1, Pp 1-8 (2024)
Abstract Earthquake swarms may be driven by fluids, through hydraulic injections or natural fluid circulation, but also by slow and aseismic slip transients. Understanding the driving factors for these prolific sequences and how they can potentially
Externí odkaz:
https://doaj.org/article/bbca7d0196ef42bca6f0648c134e7ff6
Publikováno v:
Frontiers in Earth Science, Vol 11 (2023)
Externí odkaz:
https://doaj.org/article/7380889a51b94dcd90d20aa4582f69aa
Autor:
Derek Keir, Luca De Siena, Cécile Doubre, Jessica H. Johnson, Francesco Maccaferri, Luigi Passarelli
Publikováno v:
Frontiers in Earth Science, Vol 9 (2021)
Externí odkaz:
https://doaj.org/article/eec4d0b6b31c45aba8584a66ae1f0648
Autor:
Joël Ruch, Derek Keir, Luigi Passarelli, Domenico Di Giacomo, Ghebrebrhan Ogubazghi, Sigurjón Jónsson
Publikováno v:
Frontiers in Earth Science, Vol 9 (2021)
Earthquake swarms occur sporadically at divergent plate boundaries but their recurrence over multiple decades and relation to magmatic spreading activity remain poorly understood. Here we study more than 100 earthquake swarms over a 60-year period in
Externí odkaz:
https://doaj.org/article/54862bd19ce3456d8e36c9cc3ed78541
Autor:
Marina Pastori, Lucia Margheriti, Pasquale De Gori, Aladino Govoni, Francesco Pio Lucente, Milena Moretti, Alessandro Marchetti, Rita Di Giovambattista, Mario Anselmi, Paolo De Luca, Anna Nardi, Nicola Piana Agostinetti, Diana Latorre, Davide Piccinini, Luigi Passarelli, Claudio Chiarabba
Publikováno v:
Frontiers in Earth Science, Vol 9 (2021)
In the years between 2011 and 2014, at the edge between the Apennines collapsing chain and the subducting Calabrian arc, intense seismic swarms occurred in the Pollino mountain belt. In this key region,
Externí odkaz:
https://doaj.org/article/89153a9cf88b47dbbaa4537487b4ac40
Autor:
Luigi Passarelli, Nova Heryandoko, Simone Cesca, Eleonora Rivalta, Rasmid, Supriyanto Rohadi, Torsten Dahm, Claus Milkereit
Publikováno v:
Frontiers in Earth Science, Vol 6 (2018)
Seismic swarms close to volcanoes often signal the onset of unrest. Establishing whether magma is the culprit and the unrest can be flagged as magmatic may be challenging. Here we analyze the spatio-temporal pattern of a seismic swarm that occurred i
Externí odkaz:
https://doaj.org/article/b9c5915b51884abf8bc2642b83486734
Autor:
Luigi Passarelli, Antonio Pio Rinaldi
The Adaptive Traffic Light System (ATLS) is a seismic risk mitigation tool that can be used during geoenergy exploitation projects such as in the creation of Enhanced Geothermal Systems (EGS). In real-time applications, ATLS needs to include a data a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::60ac66e50b086ab4c6a21b4879587b8d
https://doi.org/10.5194/egusphere-egu23-12783
https://doi.org/10.5194/egusphere-egu23-12783
Bathymetric highs resist subduction producing large- to small-scale change in the morphology of the subduction zone: Increase of the outer-rise curvature, trench indentation and large-scale slides and slumps in the fore-arc region. At the plate inter
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::32da5c8dc9d8d70d7a83ac66f8f6a6c7
https://doi.org/10.5194/egusphere-egu23-4944
https://doi.org/10.5194/egusphere-egu23-4944
Autor:
Lorenzo Mantiloni, Eleonora Rivalta, Timothy Davis, Luigi Passarelli, Kyle Anderson, Virginie Pinel
Forecast of vent opening locations in volcanic regions is typically performed on the basis of the spatial density of past eruptive vents, without accounting for the physics of magma propagation. As sophisticated as the statistical analysis can be, su
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6c1b4741c2ca487f923dfc2f810deceb
https://doi.org/10.5194/egusphere-egu23-13438
https://doi.org/10.5194/egusphere-egu23-13438
Publikováno v:
Geophysical Research Letters
The resistance of bathymetric highs to subduction results in large-scale morphological distortions of the outer-rise, trench, and fore-arc regions. Once subducted, bathymetric highs induce frictional segmentation along the plate interface that may re