From Botswana Diamonds PLC, 12 April 2015
PL137/2015 contains mineralogical anomalies with kimberlite indicator minerals, namely
pyropes, ilmenites and in particular chrome diopsides. Chrome diopsides (garnets) are
relatively soft and do not travel far from the kimberlite source and it is, therefore,
considered worthwhile to conduct follow-up exploration of these indicators on this small
licence area.
This comment applies to the Gope Field, some 80 klms south of Orapa but I reckon
the comment holds true to our Botswana garnets as well......
Links in with your original thread post referring to the garnet count being one of the
main indicators.
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