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  • Articles  (2)
  • 02.01. Permafrost  (1)
  • Amatrice Central Italy  (1)
  • 113-690B; Age, maximum/old; Age, minimum/young; Age model; Age model, GPTS (geomagnetic polarity timescale), Cande and Kent (1995); Ageprofile Datum Description; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Joides Resolution; Leg113; Ocean Drilling Program; ODP; Sample code/label; Sample code/label 2; South Atlantic Ocean
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  • 1
    Publication Date: 2018-03-05
    Description: The M=6.0 earthquake that struck central Italy at 01:36 UTC (Universal Time Co- ordinated) on August 24, 2016, marked the beginning of a long, still-ongoing seismic sequence, which culminated in the Mw 6.5 event at 06:40 UTC on October 30, 2016, while this volume was already in preparation, and reactivated again when this preface was almost complete. This dramatic seismic sequence, which on January 18, 2017, released four additional events of M between 5.0 and 5.5 in a few hours, caused 298 casualties, hundreds of injuries, and the practically total destruction of several villages across a wide area of the central Apennines, cov- ering the Italian Regions of Lazio, Umbria, Marche and Abruzzo. In particular, the historical village of Amatrice was completely destroyed. This seismic sequence represents an important new case study for Earth scientists only 5 years after the Ml 5.9 destructive event in the Emilia- Romagna region in 2012 [Scognamiglio et al., 2012] and 7 years after the Mw 6.3 L’Aquila earthquake of April 6, 2009 [Chiarabba et al., 2009]. During these few years, the skill of the scientific community and its reaction to the emergencies of large destructive earthquakes have improved: the earthquake epicenter and source parameters were precisely located within a few minutes of the mainshock, while the acquisi- tion of on-site multiparametric data started just a few hours after the onset of the seismic sequence. Seismological, geodetic, geological and geochemical data were rapidly collected and analyzed to identify the features of the seis- mogenic source and the geological structures re- sponsible for these earthquakes. The level of damage, the effects on the environment and the extension of ground deformations were rapidly assessed with the ultimate goal of better under- standing earthquake characteristics in order to respond to civil protection requirements. Pre- liminary data were shared worldwide through the internet via the www.ingv.it webpages, while scientific information to the media was rapid and exhaustive, also through dedicated pages (https://ingvterremoti.wordpress.com/). Less than three months after the mainshock, the Istituto Nazionale di Geofisica e Vulca- nologia (INGV) is now publishing a collection of the first scientific results in this special issue of Fast Track papers of Annals of Geophysics, vol. 59, n. 5, 2016, entirely dedicated to The Amatrice seismic sequence: preliminary data and results, as in the case of the 2012 Emilia earth- quake [Anzidei et al., 2012]. Papers are freely available online at the web site of Annals of Geophysics (http://www.annalsof geophysics.eu/), for the rapid distribution of these scientific results. This special issue repre- sents an important goal for the INGV and the whole scientific community which was involved in the study of this seismic sequence.
    Description: Published
    Description: 1-10
    Description: 2T. Sorgente Sismica
    Description: JCR Journal
    Keywords: Amatrice Central Italy ; seismic sequence ; seismic sequence
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 2
    Publication Date: 2023-02-20
    Description: Ongoing studies conducted in northern polar regions reveal that permafrost stability plays a key role in the modern carbon cycle as it potentially stores considerable quantities of greenhouse gases. Rapid and recent warming of the Arctic permafrost is resulting in significant greenhouse gas emissions, both from physical and microbial processes. The potential impact of greenhouse gas release from the Antarctic region has not, to date, been investigated. In Antarctica, the McMurdo Dry Valleys comprise 10 % of the ice-free soil surface areas in Antarctica and like the northern polar regions are also warming albeit at a slower rate. The work presented herein examines a comprehensive sample suite of soil gas (e.g., CO2, CH4 and He) concentrations and CO2 flux measurements conducted in Taylor Valley during austral summer 2019/2020. Analytical results reveal the presence of significant concentrations of CO2, CH4 and He (up to 3.44 vol%, 18,447 ppmv and 6.49 ppmv, respectively) at the base of the active layer. When compared with the few previously obtained measurements, we observe increased CO2 flux rates (estimated CO2 emissions in the study area of 21.6 km2 ≈ 15 tons day-1). We suggest that the gas source is connected with the deep brines migrating from inland (potentially from beneath the Antarctic Ice Sheet) towards the coast beneath the permafrost layer. These data provide a baseline for future investigations aimed at monitoring the changing rate of greenhouse gas emissions from Antarctic permafrost, and the potential origin of gases, as the southern polar region warms.
    Description: Published
    Description: 161345
    Description: 6A. Geochimica per l'ambiente e geologia medica
    Description: JCR Journal
    Keywords: Antarctica; ; CO(2) output; ; McMurdo Dry Valleys; ; Permafrost; ; Soil gas survey ; 02.01. Permafrost
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
    Location Call Number Limitation Availability
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