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It is worth noting that some of the faults that frame the Krzeszowice Graben might have been formed already in Late Jurassic or even earlier and they have been later rejuvenated, and references therein]. It is assumed that Krzeszowice Graben is a structure and product of extensional tectonics which began to affect in Cenozoic and has been generated by the overthrusting Outer Carpathian nappes. Differentiated Mesozoic formations of the homocline overlie unconformably the folded Precambrian and Palaeozoic basement that is disturbed by KrakГіw-Lubliniec Fault Zone and Krzeszowice-Charsznica Fault (1 and 2 in Fig.В 1). The homocline, composed of Mesozoic sedimentary rocks extends on the NW-SE direction and dips gently, at the low angle, towards NE. The Krzeszowice Graben, positioned within the southern part of the KrakГіw-CzД™stochowa Upland (Southern Poland), is one of the biggest tectonic structure of the regional tectonic unit of Silesian-KrakГіw Homocline ( Fig.В 1). Detailed location of the sampling site is listed in Table 1 and shown in Fig.В 1 (blue asterisk). Presented in this paper data numbered from (i) to (viii) are available in Appendix A, whereas the latter, numbered as (ix) are contained in Appendix B.

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The attached to this paper data includes: (i) Google Earth KML file with the location of ERT profiles and geological sampling area (ii) XLS file with ERT electrodes elevations (in local height system) (iii) XLS file with вЂњaвЂќ and вЂњnвЂќ parameters for dipole-dipole (DD) and Wenner-Schlumberger (WS) arrays used to collect field and forward 2D modeling data (iv) SuperSting STG files with raw ERT data collected in the field (v) Raw and processed ERT field data DAT files together with synthetic ERT data calculated during forward 2D modeling DAT files (both data sets can be used for inversion in Res2Dinv software) (vi) Res2Dinv IVP files which contains all inversion parameters used by authors in inversion process (vii) Res2Dmod MOD files with 2D resistivity models that refer to field data (viii) Res2Dinv INV files with the inversion results of field and synthetic data sets (ix) selected thin-section photomicrographs (JPG files) of examined Upper Jurassic limestones. Herein, the data sets constitute the basis for the research article entitled вЂњAnalysis of the tectonic and sedimentary features of the southern margin of the Krzeszowice Graben in Southern Poland based on an integrated geoelectrical and geological studiesвЂќ by WoЕєniak and Bania, 2019. Bania, Analysis of the tectonic and sedimentary features of the southern margin of the Krzeszowice Graben in Southern Poland based on an integrated geoelectrical and geological studies, J. Nawojowa GГіra (Winnica Hill), Krzeszowice Graben, Southern PolandДЄll the data sets are available with this article.

Geoelectrical survey involving 2D Electrical resistivity tomography (ERT), forward 2D resistivity modeling and geological survey (sampling procedure) have been conducted. The field apparent resistivity along with calculated (based on resistivity models) apparent resistivity data sets were inverted and together with geological data were analysed in order to characterise geological features. OLYMPUS SZX10 microscope (thin section analysis) and Dunham textural classification scheme with its later modifications.Geological field work (sampling procedure).Geoelectrical forward 2D ERT modeling (Res2Dmod software).Electrical resistivity tomography (ERT) using SuperStingв„ў Wi-Fi (R8 вЂ“ eight channel).Geoelectrical resistivity and sedimentary geologyДЇigure, Table, KML, XLS, STG, DAT, IVP, INV, MOD, JPG files

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