ALBERT

All Library Books, journals and Electronic Records Telegrafenberg

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
  • 1
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical prospecting 41 (1993), S. 0 
    ISSN: 1365-2478
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences , Physics
    Notes: Conventional velocity analysis can handle a horizontally stratified medium well. There is no indication, though, that it will be as successful when applied to a more complicated geological structure. In fact, a small angle of incidence may transform to a wide-angle reflection event for a dipping interface. In this case, conventional velocity analysis may lead to large errors and thus cannot be applied. Seismic tomography is attractive as it is virtually free from any restrictions imposed on the velocity distribution in the model space or on the setup of a seismic experiment. It is important, however, to recall that seismic tomography yields results of inferior quality compared to medical tomography. This paper investigates the reason for this and how to suppress a significant blurring of seismic tomograms. Unlike medical tomography, one cannot provide full angular coverage of the model space in a typical seismic experiment: the sources and the receivers cannot surround an unknown object inside the earth to provide a complete spectrum of view angles. Incomplete angular coverage may lead to the occurrence of large inaccuracies in the computed tomograms especially when the initial model is poorly chosen. We demonstrate a method of suppressing the adverse effects related to an incomplete angular recording. This is ‘compensation tomography’ which can be used efficiently in the case of a limited angular aperture. Numerical experiments illustrate the theory.
    Type of Medium: Electronic Resource
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 2
    ISSN: 1573-157X
    Keywords: Sicily ; seismotectonics ; rupture kinematics ; macroseismic intensity ; synthetic intensity ; Tessellation ; Voronoi polygons
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract Seismotectonic information and interpretations available for SE Sicily suggest three groups of possible sources for the M=7.1-7.5 mainshock of 1693 and its strong foreshock: (1) normal faults belonging to the Ibleo Maltese Escarpment (also: Malta Escarpment); (2) normal faults associated with the two adjacent Simeto and Scordia-Lentini structures; (3) a transfer structure between the Sicily Straits rift system and the two grabens to the north. We use a new kinematic model to invert the data sets of macroseismic intensities of the two earthquakes to retrieve information on their sources. For this, we invert point observations, or intensities tessellated with the Voronoi polygons technique, and treat residuals of inversion in the matrix of points, or in the tessellated plane. Our inversions of the regional intensity patterns using this technique show that family N°3 is a good candidate for the foreshock of 9 January, 1693. For the mainshock of 11 January, 1693, an almost perfect synthesis of its intensity IX area was obtained with our model and a source belonging to family N°3. However, all information considered (tsunami included), this earthquake could have been produced either by (3) or by a fault located along the Ibleo-Maltese Escarpment, and tangential to the Augusta and Siracusa promontories.
    Type of Medium: Electronic Resource
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 3
    Publication Date: 2011-12-01
    Description: We present a case history of the complicated strong-motion responses at a site with an almost 1D structure (Buia) in the near field of four Mw 5.2–6.0 earthquakes in the Friuli Plain of Italy. In one case (15 September 1976, 09:21 UTC, Mw 6.0), the 47-m alluvial cover of Buia experienced spectral amplitudes lower than its reference site on rock due to the different back azimuths from the source. The largest peaks at Buia occurred during an Mw 5.6 event. For practical purposes, we tested (1) subjectivity when preparing the 1D models (using a blind test with three experts); (2) 1D linear, linear-equivalent, or nonlinear modeling in common practice; and (3) the current seismic regulations. We also used noise recordings and the weak-motion velocities recorded for local events (with digital triplets on the top and the bottom of the alluvial cover). Buia’s response to weak events was more stable than its response to strong ones. A simple 1D model (five-layer) under linear conditions with good knowledge of the propagation velocities was able to reproduce the frequencies of the two relative strong-motion maxima with an average amplitude underestimation of 1.5. The nonlinear approach simulated the two recorded maxima with slight shifts in frequency. Because the disaggregation of the seismic hazard showed that the four destructive shocks studied represent the magnitude and distance ranges that dominate the hazard of Buia, we can conclude that the response spectra of the new Italian (and European) rules were sufficiently preventive, notwithstanding the aforementioned complications in the near field.
    Print ISSN: 0037-1106
    Electronic ISSN: 1943-3573
    Topics: Geosciences , Physics
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 4
    Publication Date: 2016-11-25
    Description: We analyse how intrinsic attenuation and bedrock elasticity affect the amplitude and frequency of the resonance peaks of the S -wave amplification function. The Zener model (with a single relaxation peak) and the constant- Q model are used to describe attenuation. We consider two different cases, namely, the soil is softer than the bedrock (the usual situation, that is, a sediment overlying a stiff formation) and the upper layer is stiffer than the lower half-space (e.g. basalt over sediment). The presence of Zener loss in the upper layer causes a shift of the fundamental peak towards the low frequencies, while no shift is observed due to the non-rigid (viscoelastic) character of the half-space. In the constant-Q case, the shift to the low frequencies is not significant implying that it is difficult to estimate the attenuation parameters on the basis of the location of the resonance peaks. However, attenuation affects the amplitude of the higher modes, while these modes have the same amplitude of the fundamental mode no matter the degree of elasticity of the half-space. Attenuation of the layer and non-rigidity of the half-space affect the peaks, with the latter having a stronger effect. Examples are given, considering two real cases representing a glacier in Northern Italy and an ice stream in the Antarctic continent.
    Keywords: Seismology
    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).
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 5
    Publication Date: 2019
    Description: 〈p〉The permanent GNSS station located at the Everest Pyramid Laboratory of EvK2CNR recorded its position coordinates during the Gorkha (25〈sup〉th〈/sup〉 of April 2015) and Chennai zone (12th of May 2015) earthquakes at an interval of every 30". The data recorded for a period of three days before and after the earthquakes were analyzed and the movement pointed out the shifting of the GNSS station point from its original position every 30'. From an accurate analysis of the coordinates of the station determined with the help of scientific GNSS Bernese software, it is possible to detect the movements of the station during the seismic events.〈/p〉 〈p〉The shifts of the GNSS point were added up providing an integral function (called PIF – Pyramid Integral Function) that can be computed for each of the three components. Comparing them with the displacement record of the GURALP broadband seismic station (IO-EVN) of the OGS (Istituto Nazionale di Oceanografia e di Geofisica Sperimentale – OGS – Trieste), located at the Pyramid, it is possible to establish a correlation especially with the Vertical and North components, and the maxima of the PIF function coincide with the time of occurrence of the earthquakes.〈/p〉
    Print ISSN: 0375-6440
    Electronic ISSN: 2041-4927
    Topics: Geosciences
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 6
    Publication Date: 2017-09-25
    Print ISSN: 0037-1106
    Electronic ISSN: 1943-3573
    Topics: Geosciences , Physics
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 7
    Publication Date: 2009-09-23
    Description: On 23 October 1904, the area of the Oslofjord was struck by an M (sub S) 5.4 earthquake that was felt over much of northern Europe. We collected information available from seismological bulletins of the time and also seismogram copies from a number of seismic stations in Europe. This allowed, for the first time for this earthquake, an instrumental epicentral location, even if the observation capabilities at that time were poor due to low seismograph amplification and timing problems. After a careful selection and weighting of published onset times, the reported observations from the seismic stations in Uppsala, Hamburg, Potsdam, Gottingen, Leipzig, and Tartu could be used for this instrumental location of the event. We also performed an inversion of the available macroseismic observations, based on the kinematic function (KF) for the radiation of body waves from a line source. Because the problem is nonlinear and also bimodal for pure dip-slip mechanisms, we used a sharing niching genetic algorithm to perform the inversion. The new epicenter obtained from the KF intensity inversion is consistent with the new instrumental solution, giving a location in the lower crust (25-30 km) and close to the eastern coast of the Oslofjord, near the junction of two major fault zones. The KF inversion was moreover able to constrain the fault-plane mechanism with an almost vertical rupture plane striking north-northeast-south-southwest (206 degrees -212 degrees ) with a mixed mechanism (approximately 64 degrees rake angle), the ambiguity of which is resolved by the polarities of the Pn onset observed on the horizontal components of the Uppsala Wiechert seismograph. The magnitude of the event has previously been assessed to M (sub S) 5.4, based on the size of the felt area observations, and a value of M (sub S) approximately 5.4 has now been independently confirmed both through the new intensity inversion and through the instrumental data.
    Print ISSN: 0037-1106
    Electronic ISSN: 1943-3573
    Topics: Geosciences , Physics
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 8
    Publication Date: 2011-05-01
    Print ISSN: 0895-0695
    Electronic ISSN: 1938-2057
    Topics: Geosciences
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 9
    Publication Date: 2009-11-01
    Print ISSN: 0895-0695
    Electronic ISSN: 1938-2057
    Topics: Geosciences
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 10
    Publication Date: 2019-01-01
    Print ISSN: 0305-8719
    Electronic ISSN: 2041-4927
    Topics: Geosciences
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...