I took a look at the historical hole MTDD008's (~300m south of MTJV001) graphic log and in my view there are some important similarities in the mineralisation described in the recent MTJV001 hole. These similarities include descriptions of heavily disseminated sulphides in similar rock types to those in MTJV001, which suggest that the sulphides described by the field geologist on MTJV001 extend at least south to MTDD008. The perplexing observation I have, is the considerable thickness of peridotite (solid purple) encountered in MTJV001 sandwiched between the mafic basalt/dolerite (green) and altered ultramafic. Also, in the MTDD008 well, sediment (chert), was encountered in two separate intervals while MTDD026 and MTJV001 encountered only one sediment horizon.
Kind regards OldGeo
GSR Price at posting:
7.8¢ Sentiment: Buy Disclosure: Held
