HR: 1340h
AN: T23A-1214    [Abstracts]
TI: New 3D Gravity Model of the Lithosphere and new Approach of the Gravity Field Transformation in the Western Carpathian-Pannonian Region
AU: * Bielik, M
EM: bielik@fns.uniba.sk
AF: Comenius University, Faculty of Natural Sciences, Department of Applied and Environmental Geophysics, Mlynska dolina, pav. G, Bratislava 4, Slo 842 15, Slovakia (Slovak Republic)
AU: Tasarova, Z A
EM: tasarova@geophysik.uni-kiel.de
AF: Institut für Geowissenschaften, Abt. Geophysik, Christian-Albrechts-Universität zu Kiel, Otto-Hahn-Platz 1, Kiel, Ger D 24118, Germany
AU: Goetze, H
EM: hajo@geophysik.uni-kiel.de
AF: Institut für Geowissenschaften, Abt. Geophysik, Christian-Albrechts-Universität zu Kiel, Otto-Hahn-Platz 1, Kiel, Ger D 24118, Germany
AU: Mikuska, J
EM: mikuska@gtrend.sk
AF: G-trend, s.r.o., Kolískova 1, Bratislava 4, Slo 841 05, Slovakia (Slovak Republic)
AU: Pasteka, R
EM: pasteka@fns.uniba.sk
AF: Comenius University, Faculty of Natural Sciences, Department of Applied and Environmental Geophysics, Mlynska dolina, pav. G, Bratislava 4, Slo 842 15, Slovakia (Slovak Republic)
AB: The 3-D forward modeling was performed for the Western Carpathians and the Pannonian Basin system. The density model includes 31 cross-sections, extends to depth of 220 km. By means of the combined 3-D modeling, new estimates of the density distribution of the crust and upper mantle, as well as depths of the Moho were derived. These data allowed to perform gravity stripping, which in the area of the Pannonian Basin is crucial for the signal analysis of the gravity field. In this region, namely, two pronounced features (i.e. the deep sedimentary basins and shallow Moho) with opposite gravity effects make it impossible to analyze the Bouguer anomaly by field separation or filtering. The results revealed a significantly different nature of the Western Carpathian- Pannonian region (ALACAPA and Tisza-Dacia microplates) from the European Platform lithosphere (i.e. these microplates to be much less dense than the surrounding European Platform lithosphere). The calculation of the transformed gravity maps by means of new method provided the additional information on the lithospheric structure. The use of existing elevation information represents an independent approach to the problem of transformation of gravity maps. Instead of standard separation and transformation methods both in wave-number and spatial domains, this method is based on the estimating of really existing linear trends within the values of complete Bouguer anomalies (CBA), which are understood as a function defined in 3D space. An important assumption that the points with known input values of CBA lie on a horizontal plane is therefore not required. Instead, the points with known CBA and elevation values are treated in their original positions, i.e. on the Earth surface.
DE: 8122 Dynamics: gravity and tectonics
SC: Tectonophysics [T]
MN: 2007 Fall Meeting