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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| Veröffentlicht in: | Acta geodynamica et geomaterialia 2008-01, Vol.5 (2), p.177 |
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| container_title | Acta geodynamica et geomaterialia |
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| creator | Zogala, Bogdan Dubiel, Ryszard Lewandowski, Jozef Zuberek, Waclaw M Gaska, Grzegorz |
| description | 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. KEYWORDS: resistivity imaging, Pleistocene, geologic structure |
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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. 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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. 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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. KEYWORDS: resistivity imaging, Pleistocene, geologic structure</abstract><pub>Akademie Ved Ceske Republiky, Ustav Struktury a Mechaniky Hornin</pub></addata></record> |
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| ispartof | Acta geodynamica et geomaterialia, 2008-01, Vol.5 (2), p.177 |
| issn | 1214-9705 |
| language | eng |
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| source | Elektronische Zeitschriftenbibliothek - Frei zugängliche E-Journals; Alma/SFX Local Collection |
| subjects | Environmental aspects Geodynamics Geological structures Glacial epoch Imaging systems Methods Natural history Sediments (Geology) |
| title | Application of resistivity imaging method for investigation of geologic structure of Pleistocene sediments |
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