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  • 1
    Series available for loan
    Series available for loan
    Kjeller
    Associated volumes
    Call number: S 99.0085(1-2013)
    In: Semiannual technical summary
    In: NORSAR Scientific Report
    Type of Medium: Series available for loan
    Pages: 85 S. : farb. graph. Darst.
    Series Statement: 1-2013
    Classification:
    Seismology
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 2
    Series available for loan
    Series available for loan
    Kjeller
    Associated volumes
    Call number: S 99.0085(2-2012)
    In: Semiannual technical summary
    In: NORSAR Scientific Report
    Type of Medium: Series available for loan
    Pages: 77 S.
    Series Statement: 2-2012
    Classification:
    Seismology
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 3
    Series available for loan
    Series available for loan
    Kjeller
    Associated volumes
    Call number: S 99.0085(2-2013)
    In: Semiannual technical summary
    In: NORSAR Scientific Report
    Type of Medium: Series available for loan
    Pages: 56 S.
    Series Statement: 2-2013
    Classification:
    Seismology
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 4
    Series available for loan
    Series available for loan
    Kjeller
    Associated volumes
    Call number: S 99.0085(2-2014)
    In: Semiannual technical summary
    In: NORSAR Scientific Report
    Type of Medium: Series available for loan
    Pages: 82 S. : farb. Ill., graph. Darst., Kt.
    Series Statement: 2-2014
    Classification:
    Seismology
    Location: Lower compact magazine
    Branch Library: GFZ Library
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  • 5
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    In:  Bulletin of the Seismological Society of America, Luxembourg, Conseil de l'Europe, vol. 89, no. 2, pp. 342-347, pp. 1006, (ISSN: 1340-4202)
    Publication Date: 1999
    Keywords: Radiation pattern ; Magnitude ; Data analysis / ~ processing ; Fault plane solution, focal mechanism ; BSSA
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  • 6
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    Unknown
    In:  J. Geophys. Res., Berlin, Pergamon, vol. 111, no. B4, pp. 531-565, pp. B04306, (ISSN: 1340-4202)
    Publication Date: 2006
    Keywords: Seismology ; Nuclear explosion ; Modelling ; Source ; Rock mechanics ; Detectors ; Discrimination ; JGR ; decoupling ; chemical ; explosion ; 7219 ; Seismology: ; Seismic ; monitoring ; and ; test-ban ; treaty ; verification ; 7260 ; Theory ; 7290 ; Seismology: ; Computational ; seismology ; CTBT
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  • 7
    Publication Date: 2012-04-27
    Description: SUMMARY Correlation detectors are becoming a standard method for identifying seismic signals from repeating sources. These highly sensitive, source-specific detectors frequently facilitate a reduction in the detection threshold by around an order of magnitude. Detections are typically declared when the value of the correlation coefficient (CC), or a related statistic, exceeds significantly some measure of the variability of values over a longer time window. The performance of correlation detectors is often compromised by the presence of short duration, high-amplitude signals, which influence excessively the value of the CC. We suggest replacing the original seismograms with waveforms in which the value of each sample is replaced by the ratio of that value to a centred moving average of absolute values of the original waveform. These ratio-to-moving-average (RMA) seismograms are relatively featureless over long time intervals, but resemble greatly the original waveforms over short time windows and hence still capture the characteristic seismic fingerprint of a given source. We demonstrate a correlation detection calculation, which fails due to the presence of a high-amplitude signal interfering with part of the correlation window, but which succeeds when RMA seismograms are used due to the diminished influence of the interfering signal. We also demonstrate an example from an aftershock sequence where the CC traces are heavily modulated due to the high dynamic range of the original waveforms. This makes the setting of detection thresholds difficult and results in multiple peaks, which do not correspond to events in the vicinity of the master event. Repeating the calculation using RMA seismograms results in CC traces with a more well-defined detection threshold and most of the spurious detections are lost. The ability to set lower detection thresholds without increasing greatly the number of false alarms facilitates the robust detection of lower magnitude events.
    Print ISSN: 0956-540X
    Electronic ISSN: 1365-246X
    Topics: Geosciences
    Published by Oxford University Press on behalf of The Deutsche Geophysikalische Gesellschaft (DGG) and the Royal Astronomical Society (RAS).
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  • 8
    Publication Date: 2011-03-30
    Description: The April–May 2010 summit eruption of Eyjafjallajökull, Iceland, was recorded by 14 atmospheric infrasound sensor arrays at ranges between 1,700 and 3,700 km, indicating that infrasound from modest-size eruptions can propagate for thousands of kilometers in atmospheric waveguides. Although variations in both atmospheric propagation conditions and background noise levels at the sensors generate fluctuations in signal-to-noise ratios and signal detectability, array processing techniques successfully discriminate between volcanic infrasound and ambient coherent and incoherent noise. The current global infrasound network is significantly more dense and sensitive than any previously operated network and signals from large volcanic explosions are routinely recorded. Because volcanic infrasound is generated during the explosive release of fluid into the atmosphere, it is a strong indicator that an eruption has occurred. Therefore, long-range infrasonic monitoring may aid volcanic explosion detection by complementing other monitoring technologies, especially in remote regions with sparse ground-based instrument networks.
    Print ISSN: 0094-8276
    Electronic ISSN: 1944-8007
    Topics: Geosciences , Physics
    Published by Wiley on behalf of American Geophysical Union (AGU).
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  • 9
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical journal international 111 (1992), S. 0 
    ISSN: 1365-246X
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Continuous threshold monitoring is a technique for using a seismic network to monitor a geographical area continuously in time. The method provides, at a given confidence level, a continuous assessment of the upper magnitude limit of possible seismic events that might have occurred in the target area. Two approaches are presented in this paper. Site-specific threshold monitoring: by ‘focusing’ a seismic network on a specific target site, continuous threshold monitoring of that site is achieved. We optimize the monitoring capability by tuning the frequency filters and array beams to known characteristics from previously recorded events at the site. We define the threshold trace for the network as the continuous time trace of computed upper magnitude limits of seismic events in the target area, at a 90 per cent confidence level. As an example, we have conducted a one-week monitoring experiment of the northern Novaya Zemlya nuclear test site, using the Fennoscandian regional array network (NORESS, ARCESS, FINESA). We find that the threshold trace is below mb= 2.5 more than 99 per cent of the time. 34 peaks exceed mb= 2.5. All of these peaks correspond to interfering seismic events that have been independently located by a teleseismic or regional network. During the entire one-week time period, the threshold trace exceeded mb= 2.5 only for 43 min. Regional threshold monitoring: this involves conducting site-specific monitoring of a dense grid of geographical aiming points and requires the development of generic phase attenuation relationships for covering an extended geographical region. Using again the Fennoscandian regional array network, we illustrate the regional threshold monitoring approach by maps with colour contour displays. We demonstrate that the network thresholds in Fennoscandia and adjacent regions show strong regional dependence. The thresholds are below mb= 0.5 close to each array (〈300 km distance) and range from mb= 2.0 to 2.5 in parts of the Norwegian Sea and Barents Sea. The thresholds also vary significantly under different background noise conditions, and an increase of about 1.0 mb units is observed during a large teleseismic earthquake. These regional threshold maps have advantages over standard network capability maps in being more accurate during time intervals when interfering seismic events occur. They can also more easily reflect special conditions such as particularly favourable source-station propagation paths, and have the advantage of not being tied to specific event detection criteria.The paper concludes that continuous threshold monitoring offers a valuable supplement to traditional seismic techniques used in nuclear test ban monitoring. The method may also be useful for monitoring earthquake activity at low magnitudes for sites of special interest, as well as for monitoring earthquake aftershock sequences.
    Type of Medium: Electronic Resource
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  • 10
    Publication Date: 2024-04-20
    Description: We provide a GIS data inventory of confirmed and proposed glacially-induced faults. Stresses, perturbated as a response to the advance and retreat of continental ice sheets and glaciers, can reactivate pre-existing faults. Previously referred to as "PostGlacial Faults" (PGFs), these faults are now called "Glacially-Induced Faults" (GIFs). More than a dozen kilometre-long and several metre-high fault-scarps have been identified in northern Fennoscandia since extensive investigations started in the 1960s and 1970s. Similar faults, but by far not of such dimensions, have also been described in eastern Canada. In other formerly glaciated areas in Europe, e.g., the southern parts of Sweden, Norway and Finland, the southern Baltic Sea, Denmark, northern Germany and Poland, and the Baltic countries, GIFs have rarely been observed and discussed in the literature. However, the number of studies with reliable field evidence for proposing such faults has increased considerably in recent years. The estimated fault movements are of minor magnitude, though, as compared with those in northern Fennoscandia. The database contains the confirmed GIFs in northern Fennoscandia including north-western Russia. The geological surveys in Norway, Sweden and Finland analysed recent LiDAR (Light Detection And Ranging) data from their countries, which helped uncover new faults and revise the geometry of the existing ones. In addition, we include several proposed GIFs outside this area, e.g., in southern Sweden, Denmark and Germany. Ongoing work suggests the occurrence of GIFs in Iceland, Canada and Antarctica. The database will be continually updated, considering new results. A summarized description of the GIF in this database is given in: Steffen, H., Olesen, O., and Sutinen, R. (2021). Glacially-Triggered Faulting. Cambridge University Press, Cambridge, UK, ca. 450 pp., expected publication February 2021.
    Keywords: Glacially induced faults; Post-Glacial faults (PGF)
    Type: Dataset
    Format: application/zip, 161.1 kBytes
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