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Borehole Spectral Gamma-Gamma Density Log Calibration in Massive Sulfides

机译:大量硫化物中的井孔光谱Gamma-Gamma密度测井校正

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摘要

The Geological Survey of Canada acquired spectral γ-γ density logging data in several underground boreholes at a Pb-Zn-Cu massive sulfide deposit, in order to field-calibrate the density logging tool for use in high-density/high-atomic-number (Z) base metal sulfide zones. Density determinations were always underestimated with the standard calibration procedure incorporating one energy window in the Compton scattering region of the spectrum. Core densities were also measured in the field on several drill core sections that were selected to represent waste rock, massive pyrite and Pb-Zn-Cu sulfide mineralization. A non-linear, multiple regression of core density against three energy windows covering the backscatter γ-ray energy spectrum from 50 to 500 keV provided a calibration equation that gave fairly accurate density estimates within the low-effective-Z (country rock) and high-effective-Z (base metal sulfide) media.
机译:加拿大地质调查局在Pb-Zn-Cu块状硫化物矿床的几个地下钻孔中获取了γ-γ光谱光谱数据,以便现场校准用于高密度/高原子序数的密度测井工具(Z)贱金属硫化物区。密度测定总是被标准校准程序低估的,该标准校准程序在光谱的康普顿散射区域中结合了一个能量窗口。在现场还测量了几个钻芯段的岩心密度,这些岩心段被选为代表废石,块状黄铁矿和Pb-Zn-Cu硫化物矿化。核心密度相对于覆盖从50到500 keV的反向散射γ射线能谱的三个能量窗口的非线性多元回归提供了一个校准方程,该方程在低有效Z(乡村岩石)和高有效Z范围内给出了相当准确的密度估计-有效的Z(贱金属硫化物)介质。

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