Variability In The Gold Grade And Spatial Structures Of Witwatersrand Reefs: The Implications For Geostatistical Ore Valuations

The Southern African Institute of Mining and Metallurgy
D. G. Krige
Organization:
The Southern African Institute of Mining and Metallurgy
Pages:
6
File Size:
544 KB
Publication Date:
Jan 1, 1993

Abstract

Recent publications have demonstrated the important role that can be played by a priori information of the grade levels, variability, and spatial patterns in adjacent or nearby areas in improving the quality of grade estimates for virgin or sparsely drilled areas. A research project was therefore conducted involving the collection and analysis of extensive sampling and borehole data from 7 reefs on some 30 Witwatersrand mines. This paper shows that the 'equivalent' log variance for the two-parameter lognormal model provides a good basis for the study and comparison of the levels and behaviour of relative variances. The trends of these against the corresponding log areas were found to form distinctive patterns, which are useful for these purposes. The patterns for the Basal, Vaal, Carbon Leader, and Main Reef Series form a reasonably close group, whereas those for the V.C.R.(particularly where the facies are mixed), B Reef, and Kimberley-Elsburg Reefs (particularly for narrow channel widths) do not always conform. The patterns shown by underground chip samples are also compared with those obtained from borehole cores. It is shown how this information can be used to improve the borehole valuation of new mines and of virgin areas in existing mines.
Citation

APA: D. G. Krige  (1993)  Variability In The Gold Grade And Spatial Structures Of Witwatersrand Reefs: The Implications For Geostatistical Ore Valuations

MLA: D. G. Krige Variability In The Gold Grade And Spatial Structures Of Witwatersrand Reefs: The Implications For Geostatistical Ore Valuations. The Southern African Institute of Mining and Metallurgy, 1993.

Export
Purchase this Article for $25.00

Create a Guest account to purchase this file
- or -
Log in to your existing Guest account