Bibliothek

feed icon rss

Ihre E-Mail wurde erfolgreich gesendet. Bitte prüfen Sie Ihren Maileingang.

Leider ist ein Fehler beim E-Mail-Versand aufgetreten. Bitte versuchen Sie es erneut.

Vorgang fortführen?

Exportieren
Filter
  • 1990-1994  (3)
  • 1
    Digitale Medien
    Digitale Medien
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical journal international 102 (1990), S. 0 
    ISSN: 1365-246X
    Quelle: Blackwell Publishing Journal Backfiles 1879-2005
    Thema: Geologie und Paläontologie
    Notizen: 5000 P-wave traveltime residuals from about 300 local and 400 teleseismic earthquakes recorded by the Athens seismological network were used to study the structure of the lithosphere in the Aegean region. Teleseismic data included readings from local stations which do not routinely report to the ISC. the large values of the residuals (up to ± 3 s) and their variation with azimuth and epicentral distance indicate significant velocity heterogeneity in the upper mantle. P-wave traveltime residuals were inverted simultaneously for both local and teleseismic earthquakes. Tomographic results, which are best resolved at lithospheric depths, reveal a heterogeneous lithosphere down to a depth of 100 km or so. A high-velocity anomaly is found dipping at an average of 45° to the NE away from the Hellenic trench, and supports the hypothesis of subduction due to a cooler descending slab of oceanic composition. an area of low velocities is observed at depths less than 80 km in the Aegean back-arc, corresponding well with observed, high heat flow values in the area. In contrast, an area of relatively higher velocity anomalies is resolved in the lithosphere underlying the Sea of Crete.
    Materialart: Digitale Medien
    Bibliothek Standort Signatur Band/Heft/Jahr Verfügbarkeit
    BibTip Andere fanden auch interessant ...
  • 2
    Digitale Medien
    Digitale Medien
    Springer
    Natural hazards 4 (1991), S. 389-419 
    ISSN: 1573-0840
    Schlagwort(e): Earthquakes ; historical seismicity ; Africa
    Quelle: Springer Online Journal Archives 1860-2000
    Thema: Energietechnik , Geographie , Geologie und Paläontologie
    Notizen: Abstract We have re-examined those earthquakes in Africa south of 20°N, in the period 1900–1930, that appear from instrumental or macroseismic evidence to have a magnitude of 5 3/4 or greater. We identify more than 50 such events, about twice as many as listed by Gutenberg and Richter (1954). We find that the combined use of early instrumental readings and macroseismic information gleaned from previously untapped sources gives the best control of location. Instrumental relocation is difficult because of the lack of stations in Africa and the very uneven global distribution. For the low-gain, medium-period instruments then in use, the best control often comes from using the maximum Airy phase of surface waves. Similarly, there is a lack of sources of macroseismic information, and the simple building practice makes it difficult to assess intensity. We have recalculated magnitude Ms uniformly using the Prague formula. We discuss these problems and show that it is likely that our list is complete only down to magnitude about 6, and that the seismic record for Africa before this century will probably remain incomplete for events of all magnitudes. Of the 54 events in our list 20 are between magnitude 6 and 7, and the largest is the Rukwa earthquake of 1910 in Tanzania (Ms 7.4). The only other African event known to rival it in size is that in southern Sudan on 20 May 1990 (Ms 7.2).
    Materialart: Digitale Medien
    Bibliothek Standort Signatur Band/Heft/Jahr Verfügbarkeit
    BibTip Andere fanden auch interessant ...
  • 3
    Digitale Medien
    Digitale Medien
    Springer
    Pure and applied geophysics 140 (1993), S. 1-14 
    ISSN: 1420-9136
    Schlagwort(e): Crustal phases ; earthquake locations ; re-identification ; first arrival ; upper mantle ; granitic layer
    Quelle: Springer Online Journal Archives 1860-2000
    Thema: Geologie und Paläontologie , Physik
    Notizen: Abstract For crustal earthquakes of moderate or large size, the first reported phases at distant stations are usually the first predicted by the crustal model used. For smaller events, however, or for stations at larger distances, the first phase detected is often a later crustal phase of larger amplitude. This may be eitherPg which travels entirely in the upper crustal layer with a velocity of about 5.6 km/s, orP * with a path mainly in the lower crustal layer at a velocity of about 6.7 km/s. Many earthquake location programs do not take account of these phases, and treat their arrivals as if they were the earlier phasePn. At the International Seismological Centre we re-identify up to 200 crustal phases each month. This often results in significant improvement in position, the direct determination of depth or even the obtaining of a formal solution where none was possible before. We find that these re-identifications are needed in most continental areas of the world, and that the original crustal model of Jeffreys and Bullen still remains a useful standard.
    Materialart: Digitale Medien
    Bibliothek Standort Signatur Band/Heft/Jahr Verfügbarkeit
    BibTip Andere fanden auch interessant ...
Schließen ⊗
Diese Webseite nutzt Cookies und das Analyse-Tool Matomo. Weitere Informationen finden Sie hier...