Electrical resistivity tomography (ERT) and sedimentological analysis applied to investigation of Upper Jurassic limestones from the Krzeszowice Graben (Kraków Upland, southern Poland)

Woźniak, T.; Bania, G.; Mościcki, W. J.; Ćwiklik, M.

doi:10.7306/gq.1403

Artykuł - szczegóły

Tytuł artykułu

Electrical resistivity tomography (ERT) and sedimentological analysis applied to investigation of Upper Jurassic limestones from the Krzeszowice Graben (Kraków Upland, southern Poland)

Autorzy

Woźniak T. , Bania G. , Mościcki W. J. , Ćwiklik M.

Treść / Zawartość

Pełne teksty:

Woźniak_T_Electrical_Geol. Quart._Vol. 62_No 2_2018.pdf

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Identyfikatory

DOI

10.7306/gq.1403

Warianty tytułu

Języki publikacji

Abstrakty

This paper highlights the application of shallow non-invasive geophysics (electrical resistivity tomography) supported by sedimentological analysis applied to the investigation, description and interpretation of Upper Jurassic limestones exposed in the abandoned quarry near the village of Tomaszowice (Kraków Upland, southern Poland). Within this site, on the northern margin of the Krzeszowice Graben, a facies diversity of Upper Jurassic limestones can be observed. Field exposures were analysed to broadly characterize these Upper Jurassic limestones in terms of facies and microfacies development. Three facies types, including pelitic limestones, bedded limestones and carbonate gravity-flow deposits, composed of numerous microfacies, have been distinguished. ERT study using a dipole-dipole array has been carried out, along 5 parallel 110 m long profiles and along a perpendicular 110 m long profile, north of the Tomaszowice Quarry wall. The use of ERT in combination with the geological data allowed characterization and description of the geology at the research site as well as the determination of the lithological composition and internal architecture of the subsurface. Furthermore, the ERT interpretation results indicated the presence of a series of a secondary faults closely linked with the Krzeszowice Graben. The distribution of the gravity-flow deposits reflects the fault zone pattern of the graben and Late Jurassic fault activity.

Słowa kluczowe

electrical resistivity tomography ERT Upper Jurassic limestones Oxfordian Krzeszowice Graben Southern Poland

Wydawca

Państwowy Instytut Geologiczny - Państwowy Instytut Badawczy

Czasopismo

Geological Quarterly

Rocznik

2018

Tom

Vol. 62, No. 2

Strony

287--302

Opis fizyczny

Bibliogr. 78 poz., rys., tab., wykr.

Twórcy

autor

Woźniak T.

Faculty of Geology, Geophysics and Environment Protection, AGH University of Science and Technology, al. A. Mickiewicza 30, 30-059 Kraków, Poland

autor

Bania G.

Faculty of Geology, Geophysics and Environment Protection, AGH University of Science and Technology, al. A. Mickiewicza 30, 30-059 Kraków, Poland

autor

Mościcki W. J.

Faculty of Geology, Geophysics and Environment Protection, AGH University of Science and Technology, al. A. Mickiewicza 30, 30-059 Kraków, Poland

autor

Ćwiklik M.

Faculty of Geology, Geophysics and Environment Protection, AGH University of Science and Technology, al. A. Mickiewicza 30, 30-059 Kraków, Poland

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Uwagi

Opracowanie rekordu w ramach umowy 509/P-DUN/2018 ze środków MNiSW przeznaczonych na działalność upowszechniającą naukę (2018).

Typ dokumentu

Bibliografia

Identyfikator YADDA

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