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
    Springer
    Journal of seismology 4 (2000), S. 267-284 
    ISSN: 1573-157X
    Keywords: infinite-space synthetics ; inversion of near-source data ; near-field seismograms
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract We have implemented and tested a simple inversionscheme to retrieve source parameters of small andmoderate earthquakes recorded at close distances. Theinversion assumes that such events may be approximatedby a point-source shear dislocation, and the mediummay be considered an infinite space. Theoreticalseismograms used in the inversion include near- andintermediate-field contributions. The effect of freesurface is approximately taken into account bymultiplying the infinite-space synthetics by two. Thelocation of the event is assumed to be known. Based onan examination of the data, the user chooses thelength of the record and the weight of each trace tobe used in the inversion. The shape of the source-timefunction is estimated from the observed seismograms.A grid search is performed to determine the focalmechanism and the seismic moment which minimizes theerror between the observed and the syntheticseismograms. For two or more recordings, the inversiongives a solution which is consistent with thefirst-motion data and/or the moment tensor inversionof regional seismic waves. If only a singlethree-component recording is available then theinversion yields more than one equally acceptablefocal mechanisms. In such cases, the first-motionpolarities or a prior knowledge of the tectonics ofthe region is essential to constrain the solution. Thetest of the method on near-source broadband recordingsof small and moderate earthquakes in Mexico and theaftershock sequence of 1997 Umbria-Marche, Italy showsthat it gives fast, and surprisingly robust andreliable estimation of source parameters.
    Type of Medium: Electronic Resource
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 2
    Publication Date: 2008-08-02
    Description: We study source characteristics of two small, local earthquakes which occurred in Delhi on 28 April 2001 (Mw3.4) and 18 March 2004 (Mw2.6). Both earthquakes were located in the heart of New Delhi, and were recorded in the epicentral region by digital accelerographs. The depths of the events are 15 km and 8 km, respectively. First motions and waveform modeling yield a normal-faulting mechanism with large strike-slip component. The strike of one of the nodal planes roughly agrees with NE-SW orientation of faults and lineaments mapped in the region. We use the recordings of the 2004 event as empirical Green's functions to synthesize expected ground motions in the epicentral region of a Mw5.0 earthquake in Delhi. It is possible that such a local event may control the hazard in Delhi. Our computations show that a Mw5.0 earthquake would give rise to PGA of ∼200 to 450 gal, the smaller values occurring at hard sites. The estimate of corresponding PGV is ∼6 to 15 cm/s. The recommended response spectra, Sa, 5% damping, for Delhi, which falls in zone IV of the Indian seismic zoning map, may not be conservative enough at soft sites for a postulated Mw5.0 local earthquake. © Springer Science+Business Media B.V. 2008.
    Print ISSN: 1383-4649
    Electronic ISSN: 1573-157X
    Topics: Geosciences , Physics
    Published by Springer
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 3
    Publication Date: 2000-01-01
    Description: We have implemented and tested a simple inversion scheme to retrieve source parameters of small and moderate earthquakes recorded at close distances. The inversion assumes that such events may be approximated by a point-source shear dislocation, and the medium may be considered an infinite space. Theoretical seismograms used in the inversion include near- and intermediate-field contributions. The effect of free surface is approximately taken into account by multiplying the infinite-space synthetics by two. The location of the event is assumed to be known. Based on an examination of the data, the user chooses the length of the record and the weight of each trace to be used in the inversion. The shape of the source-time function is estimated from the observed seismograms. A grid search is performed to determine the focal mechanis m and the seismic moment which minimizes the error between the observed and the synthetic seismograms. For two or more recordings, the inversion gives a solution which is consistent with the first-motion data and/or the moment tensor inversion of regional seismic waves. If only a single three-component recording is available then the inversion yields more than one equally acceptable focal mechanisms. In such cases, the first-motion polarities or a prior knowledge of the tectonics of the region is esse ntial to constrain the solution. The test of the method on near-source broadband recordings of small and moderate earthquakes in Mexico and the aftershock sequence of 1997 Umbria-Marche, Italy shows that it gives fast, and surprisingly robust and reliable estimation of source parameters.
    Print ISSN: 1383-4649
    Electronic ISSN: 1573-157X
    Topics: Geosciences , Physics
    Published by Springer
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
  • 4
    Publication Date: 2012-07-29
    Print ISSN: 0921-030X
    Electronic ISSN: 1573-0840
    Topics: Energy, Environment Protection, Nuclear Power Engineering , Geography , Geosciences
    Published by Springer
    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...