Strain Diffusion from the 30 October 2016 Norcia (Central Italy) Earthquake

Viti, Marcello

doi:10.1029/2018tc005464

Cited by 5 publications

(1 citation statement)

References 79 publications

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“…In the short-term the northward displacement of Adria does not develop continuously over time. Each seismic decoupling along the Adria lateral boundaries (Dinaric and Apennine belts) triggers the acceleration of the involved Adriatic sector e.g., [52][53][54]. These local accelerations induce an increase of stress at the other still blocked Adria boundaries, where consequently the probability of earthquake occurrence gets higher.…”

Section: Short-term Kinematics Of Adria and Spatio-temporal Distribution Of Seismicity In The Surrounding Beltsmentioning

confidence: 99%

Tectonics and Seismicity in the periAdriatic Zones: Implications for Seismic Hazard in Italy

Mantovani¹,

Tamburelli²,

Babbucci³

et al. 2021

Earthquakes - From Tectonics to Buildings

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The recognition of the seismic zones most prone to next major earthquakes in Italy would considerably help the choice of the most efficient prevention plan. This work describes an attempt to gain reliable information about that problem by exploiting the knowledge about the short-term development of the ongoing tectonic processes in the study area and its influence on the spatio-temporal distribution of major shocks. In the periAdriatic zones, such distribution is connected with the progressive northward displacement of the Adria plate, that is controlled by the progressive activation of the decoupling fault systems in the surrounding belts (Dinarides, Apennines and Eastern Southern Alps). The reliability of this hypothesis is evaluated by analysing the seismic histories of the periAdriatic zones. The regularity patterns that are tentatively recognised in such histories are used to identify the most probable location of next major shocks. Further insights into the present seismic hazard in the Southern Apennines and Calabria are tentatively inferred from tectonic connections between these regions and other periAdriatic zones, suggested by the seismic histories in the last 2–4 centuries and the geodynamic/tectonic context in the central Mediterranean area.

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Section: Short-term Kinematics Of Adria and Spatio-temporal Distribution Of Seismicity In The Surrounding Beltsmentioning

confidence: 99%

Tectonics and Seismicity in the periAdriatic Zones: Implications for Seismic Hazard in Italy

Mantovani¹,

Tamburelli²,

Babbucci³

et al. 2021

Earthquakes - From Tectonics to Buildings

Self Cite

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Tectonics and Spatio-temporal Distribution of Seismicity

Mantovani,

Viti,

Babbucci

et al. 2024

Neogenic Evolution of the Mediterranean Region

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Regional labor markets after an earthquake. Short-term emergency reactions in a cross-country perspective. Cases from Chile, Ecuador, Italy

2020

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Disasters can generate different economic effects in the short run in local economies. Our goal is to reveal how natural disasters reshaped labor markets in three countries that faced massive earthquakes in the past decade: Italy (2009 L'Aquila earthquake), Chile (2010 Concepción earthquake-tsunami) and Ecuador (2016 earthquake in the coast of Manabí and Esmeraldas). These three countries present a mix of heterogeneity and homogeneity in observable characteristics of the individuals, socio-economic structure of the affected areas, institutional factors and macroeconomic characteristics, as well as the actions and budgets allocated by different governments for reconstruction and recovery in the affected areas. Using three short run labor surveys and different regression models (wage estimations and a double difference approach), we show an increase in labor income and worked hours (in average) in Ecuador for males and females, while in Italy we found an increase only in worked hours for females but not for males. In Chile no significant earthquake effects were found, neither in labor income, nor in worked hours. Our results suggest that the short run is critical to describe how regional labor markets will perform, differences and particularities of each country could be explained by institutional differences, economic trends, and how governments responded to their particular catastrophes.

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Strain Diffusion from the 30 October 2016 Norcia (Central Italy) Earthquake

Cited by 5 publications

References 79 publications

Tectonics and Seismicity in the periAdriatic Zones: Implications for Seismic Hazard in Italy

Tectonics and Seismicity in the periAdriatic Zones: Implications for Seismic Hazard in Italy

Tectonics and Spatio-temporal Distribution of Seismicity

Regional labor markets after an earthquake. Short-term emergency reactions in a cross-country perspective. Cases from Chile, Ecuador, Italy

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