Application of resistivity imaging method for investigation of geologic structure of pleistocene sediments

This paper presents the results of geophysical survey performed in the Pilawa River valley in the area of Middle Pomerania (Poland). The resistivity imaging method was applied. Resistivity profile measuring eight hundred metres allowed to investigate the geologic structure to the depth of 150 metres...

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Bibliographic Details
Main Authors: Żogała, Bogdan, Dubiel, Ryszard, Lewandowski, Józef, Zuberek, Waclaw M., Gąska, Grzegorz
Format: Article in Journal/Newspaper
Language:unknown
Subjects:
Geologie. Meteorologie. Klimatologie
pleistocén
pleistocene
resistivity imaging
eologic structure
7
551
Ice Sheet
Online Access:https://kramerius.lib.cas.cz/view/uuid:3478c4d2-9c77-479f-ac6f-c44b251ec16e
Description
Summary:This paper presents the results of geophysical survey performed in the Pilawa River valley in the area of Middle Pomerania (Poland). The resistivity imaging method was applied. Resistivity profile measuring eight hundred metres allowed to investigate the geologic structure to the depth of 150 metres. The resistivity cross section shows the structure of Pleistocene sediments and the depth of Miocene - Pleistocene boundary. The significant lowering of the boundary is related to assumable ice-sheet margin range of Pomeranian phase of North Polish Glaciation. The lowering of the boundary may be a result of sediments compaction and the subglacial tunnel slope as well. Bogdan Żogała, Ryszard Dubiel, Józef Lewandowski, Waclaw M. Zuberek and Grzegorz Gąska. Obsahuje bibliografické odkazy

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