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    Wyświetlanie 1-3 z 3
    Tytuł:
    Field mapping of buried faults : a new approach applied in the Western Carpathians
    Autorzy:
    Marko, F.
    Dyda, M.
    Gajdoš, V.
    Rozimant, K.
    Mojzeš, A.
    Powiązania:
    https://bibliotekanauki.pl/articles/2059816.pdf
    Data publikacji:
    2015
    Wydawca:
    Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
    Tematy:
    faults
    geophysical survey
    dowsing
    Western Carpathians
    Opis:
    Fault array in an area covered by Quaternary sediments and deprived of bedrock outcrops was investigated using fault trace mapping by geophysical methods and human feedback information from dowsing. The tectonics in the study area is dominated by a ENE-WSW fault zone affecting regional-scale structures. The fault network was approximated by dowsing-enhanced mapping and subsequently confirmed by field geophysical measurements using electromagnetic and radon emanometry methods. A resultant detailed map of structural discontinuities highlighted that combined dowsing and geophysical survey is an effective and reliable tool to identify buried faults. This approach with its low costs and fast field recognition is highly recommended for construction-work planning and for mineral resources exploration and exploitation.
    Źródło:
    Geological Quarterly; 2015, 59, 1; 35--46
    1641-7291
    Pojawia się w:
    Geological Quarterly
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Direct Measurements of Arsenic and Phosphorus Evolution During Cap-Annealing of Gold-Based Metallizations on GaAs and InP
    Autorzy:
    Piotrowska, A.
    Kamińska, E.
    Guziewicz, M.
    Veresegyhazy, R.
    Mojzes, I.
    Pecz, B.
    Powiązania:
    https://bibliotekanauki.pl/articles/1891383.pdf
    Data publikacji:
    1991-09
    Wydawca:
    Polska Akademia Nauk. Instytut Fizyki PAN
    Tematy:
    73.40.Ns
    Opis:
    Evolution of arsenic and phosphorus during heat treatment of unprotected and encapsulated Au, AuZn and AuGeNi contacts on GaAs and InP has been examined and correlated with their ohmic behavior.
    Źródło:
    Acta Physica Polonica A; 1991, 80, 3; 457-460
    0587-4246
    1898-794X
    Pojawia się w:
    Acta Physica Polonica A
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
    Tytuł:
    Geokinematics of Central Europe: new insights from CERGOP-2/Environment Project
    Autorzy:
    Caporali, A.
    Becker, M.
    Fejes, I.
    Gerhatova, L.
    Ghitau, D.
    Grenerczy, G.
    Hefty, J.
    Medac, D.
    Milev, G.
    Mojzes, M.
    Mulic, M.
    Powiązania:
    https://bibliotekanauki.pl/articles/224596.pdf
    Data publikacji:
    2007
    Wydawca:
    Politechnika Warszawska. Wydział Geodezji i Kartografii
    Tematy:
    GPS
    geodezja
    geodynamika w Europie Centralnej
    tektonika w Europie Centralnej
    naprężenia i odształcenia w Europie Środkowej
    GPS Geodesy
    Central European Geodynamics
    Central European Tectonics
    Stress and Strain in Central Europe
    Opis:
    The CERGOP2 project funded by the European Union from 2003 to 2006 under the 5th Framework Programme benefits from repeated measurements of the coordinates of epoch and permanent GPS stations forming the CEGRN network in Central Europe, starting 1994. We report on the results of the systematic processing of the available data up to 2005. The analysis work has yielded the velocities of some 60 sites, covering a variety of Central European tectonic provinces, from the Adria indenter to the Tauern window, the Pannonian basin, the Vrancea Seismic Zone and the Carpathian Mountains. The estimated velocities define kinematical patterns which outline, with varying spatial resolution depending on the station density and history, the present day tectonic flow in Central Europe.The CEGRN data show that the majority of active contraction originating from the Eurasia Nubia plate boundary and the microplate between them is taken up primarily in the Eastern Alps, the Dinarides, and the Pannonian Basin. After removal from the ITRF2000 velocities of a rigid rotation accounting for the mean motion of stable Europe, the residual velocities have random orientations with 0.3 mm/yr scatter. This Iow figure provides an upper estimate for the level of rigidity of the European Platform. A 2.3 mm/yr north-south oriented convergence rate is implied by our data between Adria and the Southern Alps, and a narrow - -60 km wide- contraction zone in the Southern Alps is identified, consistently with earlier results. An eastward extrusion north of the contraction zone corresponds with the extension of the Tauern Window. In the southeastern boundary of the microplate, 4-4.5 mm/yr motion of Adria decreases to -1 mm/yr through the microplate, its boundary, and the Dinarides mountain range towards the southwestern part of the Pannonian Basin. Our data suggest that if the Pannonian Basin is subject to deformation, then it is most likely to be compressional than extensional. We conclude that compression and associated contraction due to the Adria collision with the Alps and the Dinarides is likely to fade away in the Western and Northern Carpathians, where our velocities and strain rates show no significant deformation.
    Źródło:
    Reports on Geodesy; 2007, z. 2/83; 7-46
    0867-3179
    Pojawia się w:
    Reports on Geodesy
    Dostawca treści:
    Biblioteka Nauki
    Artykuł
      Wyświetlanie 1-3 z 3

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