1887

Abstract

We present a gamma-spectrometric profile carried out on gold-bearing quartz veins in Poconé region, Western Brazil. Along mineralized zones, uranium and potassium elements are added by hydrothermal percolating solutions in a sufficient quantity to be detected by surface gamma ray spectrometric measurements. Extension of mineralized pits are clearly identified by an 800 meters gamma ray profile crossing a known gold deposit covered by almost 3 m thick soil and lateritic layer.

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/content/papers/10.3997/2214-4609-pdb.215.sbgf252
1999-08-15
2021-10-24
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http://instance.metastore.ingenta.com/content/papers/10.3997/2214-4609-pdb.215.sbgf252
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