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EN
In this paper are shown selected results of both sedimentary and structural interpretation in following geological regional units: Lublinian Synclinorium, Pomorian Synclinorium, Fore-Sudetic Monocline, Pomorian Anticlinorium, Carpathian Mountains and Carpathian Foredeep.
EN
Interpretation of dip log supply information in field of: geology of mineral deposits, sedimentology, structural geology, and regional geology. In this paper following problems were presented: — three-dimensional model of both: vertical and deviated boreholes; — three-dimensional model of rock, where petrophysical parameters are measured; — three-dimensional model of internal sediments structure; — three-dimensional model of horizontal borehole; — types of graphical presentation; — three-dimensional distribution of internal structure sediments model in micro, medium and macro scales; dip log interpretation methods.
EN
In Reńsko-1 well for first time in Poland were done wide well log set: conventional well logs, dip logs, LSS logs (long space sonic), and EMI logs. For doing the last one log EMI tool was used (property of Halliburton Logging Services). EMI logs were done gratis by HLS for ZZGNiG in Zielona Góra.
EN
Since some years Geofizyka Toruń has been doing dip log on Kościan Structure as a standard log in lower parts of Zechstein (usually Main Dolomite, and under Zechstein basement). Dip log were done in following boreholes: Bonikowo-1. Kościan-7, 8,9, 10, 11, 12, 13, 14. 15, 16, 17, 22 and 24 also Kokotzyn-1. Thanks to the comprehensive interpretation it was possible to: — split profiles into different lithophysical units; — characterize internal structure of Main Dolomite, Werra Anhydrite, Zechstein Limestone, and drilled parts of Carboniferous; — locate faults and characterize their parameters; — suggest origin of Zechstein Limestone sediments; identification of Carboniferous fold structures; presentation of selected interpretation results in structure scale.
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