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Tytuł artykułu

Upper mantle seismic model of Central Europe (including the Alpine orogen) based on seismic events from the Lubin Copper Basin

Autorzy
Identyfikatory
Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
The Lubin Copper Basin in Poland is situated in the vicinity of the Trans- -European Suture Zone, in the region of the Variscan orogen. It is characterized by high seismicity, mainly induced by mining. The epicentral location is particu-larly suitable for the determination of lithospheric velocity structure for the two tectonic units in Central Europe: Alpine orogen and Variscides. We analyze traveltime curves constructed on the basis of the P-wave arrival times reported by European stations and listed in the International Seismic Bulletins for the pe-riod 1985-2000. The dense azimuthal coverage of the stations situated around the Alps and in the Variscides enables the determination of 1-D velocity struc-ture down to 180 km depth. Corrections for origin times, focal depths and station elevation were applied. The main feature visible in the obtained traveltime and velocity-depth distributions is the considerable difference in the upper mantle seismic structure between the two tectonic regions. The delay of P-wave arrivals is by about 3 s larger at the Alpine stations than at the stations located in the Variscides. We at-tribute this delay to differences between "fast" and "slow" structures in the "cold" and "hot" upper mantle, respectively. The 8° discontinuity can be clearly distinguished in the proposed models by a distinct delay at the offsets around 800-900 km from the source.
Rocznik
Strony
127--141
Opis fizyczny
Bibliogr. 20 poz.
Twórcy
autor
  • Institute of Geophysics, Polish Academy of Sciences, Księcia Janusza 64, 01-452 Warszawa, Poland
autor
  • Geological Institute, University of Copenhagen Øster Voldgade 10, DK-1350 Copenhagen, Denmark
Bibliografia
  • Artemieva, I.M., W.D. Mooney, E. Perchuć and H. Thybo, 2002, Processes of lithospher evolution: new evidence on the structure of the continental crust and uppermost mantle, Tectonophysics 358, 1-15.
  • Babuska, V., J. Plomerova and J. Sileny, 1987, Structural model of the subcrustal lithosphere in Central Europe. In: C. Froidevaux and K. Fuchs (eds.), "The Composition, Struc¬ture and Dynamics of the Lithosphere-Asthenosphere System", Geodynamics Series 16, 239-251, American Geophysical Union, Washington D.C.
  • Babuska, V., J. Plomerova and M. Granet, 1990, The deep lithosphere in the Alps: a model inferred from P residuals, T&ctonophysics 176, 137-165.
  • Blundell, D., R. Freeman and S. Mueller (eds.), 1992, A Continent Revealed, the European Geotraverse, Cambridge University Press, Cambridge.
  • Dezes, P., and P. A. Ziegler, 2001, European Map of the Mohorovicic discontinuity, 2nd EU-COR-URGENT Workshop (Upper Rhine Graben Evolution and Neotectonics), Mt. St. Odile, France.
  • Draber, D., B. Guterch, H. Lewandowska-Marciniak and J. Niewiadomski, 2003, Local earthquakes recorded by the Polish seismological stations 2000, Pubis. Inst. Geophys. Pol. Acad. Sc. B-32 (362), 3-8.
  • Gibowicz, S.J., and A. Kijko, 1994, An Introduction to Mining Seismology, Academic Press, San Diego-New York.
  • Grad, M., S.L. Jensen, G.R. Keller, A. Guterch, H. Thybo, T. Janik, T. Tiira, J. Yliniemi, U. Luosto, G. Motuza, V. Nasedkin, W. Czuba, E. Gaczyński, P. Środa, K.C. Miller, M. Wilde-Piórko, K. Komminaho, J. Jacyna and L. Korabliova, 2003, Crustal structure of the Trans-European suture region along POLONAISE'97 seismic profde P4, J. Geophys. Res. 108, В11, 2541, doi:10.1029/2003JB002426.
  • ISC, 1985-2000, Bulletins of the International Seismological Centre, Intern. Seism. Centre, Berkshire.
  • Kennett, B.L.N., and E.R. England, 1991, Traveltimes for global earthquake location and phase identification, Geophys. J. Int. 105, 429-465.
  • Kissling, E., 1993, Deep structure of the Alps-what do we really know? Physics Earth Planet. Inter. 79, 87-112.
  • Lippitsch, R., 2002, Lithosphere and upper mantle P-wave velocity structure beneath the Alps by high-resolution teleseismic tomography, Diss. ETH Zurich, No. 14726.
  • Orlecka-Sikora, B., 2002, Clustered structure of seismicity from the Legnica-Głogów cooper district. Pubis. Inst. Geophys. Pol. Acad. Sc. M-24 (340), 105-119 (in Polish with English abstract and English figures and tables captions).
  • Seismological Bulletins, 1986-1998, Local earthquakes recorded by the Polish seismological stations. Pubis. Inst. Geophys. Pol. Acad. Sc.: B-13 (223), B-16 (282), B-17 (283), B-21 (316), B-22 (331), B-24 (336), B-26 (338).
  • Spakman, W., 1991, Delay-time tomography of the upper mantle below Europe. The Mediterranean, and Asia Minor, Geophys. J. Int. 107, 309-332.
  • Spakman, W, S. van der Lee and R. van der Hilst, 1993, Travel-time tomography of the European-Mediterranean mantle down to 1499 km, Phys. Earth. Planet. Inter. 79, 3-74.
  • Thybo, H., and E. Perchuc, 1997, A partially molten zone beneath the global 80 discontinuity at -100 km depth. In: K. Fuchs (ed.), "Upper Mantle Heterogeneities from Active and Passive Seismology", 343-350.
  • Thybo, H., E. Perchuc and S. Zhou, 2000, Intraplate earthquakes and a seismically defined lateral transition in the upper mantle, Geophys. Res. Let. 27, 23, 3953-3956.
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  • Wilde-Pidrko, M., M. Grad and POLONAISE Working Group, 1999, Regional and teleseismic events recorded across the TESZ during POLONAISE'97, Tectonophysics 314, 161-174.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BSL7-0009-0011
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