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Title: IDENTIFICATION OF PHYSICAL PARAMETER VARIABILITY IN PLEISTOCENE AND NEOGENE SEDIMENT WITH THE IMPLEMENTATION OF INTEGRATED GEOPHYSICAL DATA INVERSION
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IDENTIFICATION OF PHYSICAL PARAMETER VARIABILITY IN PLEISTOCENE AND NEOGENE SEDIMENT WITH THE IMPLEMENTATION OF INTEGRATED GEOPHYSICAL DATA INVERSION
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1314-2704
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English
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The central and northern parts of Poland are covered by a thick blanket of Pleistocene post-glacial sediment. Directly beneath this material lie loose, or of early diagenetic overprint, Neogene formations, mainly Miocene sediment. The thickness of Quaternary sediments in the northern part of the country locally exceeds 300 m. The loose and highly, internally diverse subsurface complex considerably hampers the completion of seismic surveys, especially those including the seismic reflection method. The basic issue on this subject is the proper solution to the issue of implementing short and long wavelength, static correction values. The completed tasks indicated the usefulness of implementing detailed gravity measurements and high-frequency magnetotelluric survey with the implementation of the artificial source of electromagnetic waves. The application of the integrated inversion and interpretation method enabled the generalization of geophysical models and proper visualization of the subsurface zone.
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conference
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17th International Multidisciplinary Scientific GeoConference SGEM 2017
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17th International Multidisciplinary Scientific GeoConference SGEM 2017, 27 ? 29 November, 2017
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Proceedings Paper
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STEF92 Technology
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International Multidisciplinary Scientific GeoConference-SGEM
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Bulgarian Acad Sci; Acad Sci Czech Republ; Latvian Acad Sci; Polish Acad Sci; Russian Acad Sci; Serbian Acad Sci & Arts; Slovak Acad Sci; Natl Acad Sci Ukraine; Natl Acad Sci Armenia; Sci Council Japan; World Acad Sci; European Acad Sci, Arts & Letters; Ac
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235-242
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27 ? 29 November, 2017
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website
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cdrom
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2875
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joint inversion; constrained inversion; static corrections; geological interpretation; integrated interpretation
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