Powiadomienia systemowe
- Sesja wygasła!
Identyfikatory
Warianty tytułu
Języki publikacji
Abstrakty
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.
Wydawca
Czasopismo
Rocznik
Tom
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.
- Thybo, H., L. Nielsen and E. Perchuc, 2003, Seismic scattering at the top of the mantle transition zone. Earth Planet. Sc. Let. 216, 259-269.
- 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