Abstract

The present study analyzes spectral gamma ray data of low-radioactivity rock cores from Rotliegend Basin. The main goal of this research was standardization of archival gamma ray logs measured in counts per minute to American Petroleum Institute units. Selected core intervals, log data, and additional crushed samples covered three different boreholes: J-1, L-7, and K-2 from Zielona Góra Basin, localized in western Poland, where J-1 was a reference borehole. Core measurements were performed on the sandstone and conglomerate formations by Gamma Logger GT spectrometer, which uses two scintillation detectors containing bismuth germanate crystals. In the cores, real concentrations of potassium, uranium, and thorium were acquired what enabled to calculate total content of radioactive elements and total uninfluenced by uranium. Delivered new total GR_GLGT curve from cores allowed accurate standardization of archival GR curves from L-7 and K-2 boreholes. Presented results showed a very good correlation between logs, core data, and laboratory analyses. These data allow precise shale volume reinterpretation.

Highlights

  • The gamma ray measurements (GR) are used as a foundation in quantifying shale volume, what allows for lithological interpretation and zone correlation from well to well (DíazCuriel et al 2019)

  • Signal from the sum of K, U, and Th counting rates allows the calculation of total GR, converted to American Petroleum Institute (API) units

  • Data acquired by gamma ray logging tools are not affected by background noise, because all radiation comes from rocks nearby detector

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Summary

Introduction

The gamma ray measurements (GR) are used as a foundation in quantifying shale volume, what allows for lithological interpretation and zone correlation from well to well (DíazCuriel et al 2019). Gamma ray emission from the rocks is related with the presence of naturally radioactive clays and ions associated with them (Ellis and Singer 2007). Data acquired by gamma ray logging tools (wireline) are not affected by background noise, because all radiation comes from rocks nearby detector. Drilling mud, flushed zones, caves, and casing of the well can have a negative influence for logs quality (Rider 2000). Spectrometric data from clean drilling core are not influenced by borehole effects, but surrounding radiation of the environment makes a high background noise. The wireline gamma ray, after wellbore influence corrections, should give the same results as core logging and laboratory measurements, despite different environmental conditions and geometrical settings

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