RJK Explorations Ltd. announced that Dr. Charles Fipke's lab, CF Mineral Research (CFM) in Kelowna, British Columbia, is analysing 12.2 tons of kimberlite of diamond drill core, surface excavation samples and reverse circulation drilling that Microlithics in Thunder Bay Ontario and CFM of Kelowna BC processed over the past 9 months, from 7 different kimberlites discovered. Kimberlite indicator minerals (KIMs) were concentrated and tested, returning materially important results. KIM grain determinations were identified that commonly derive from kimberlite sources originating in the diamond stability field. The diamond stability field is located from depths of about 200 km in the earth at the lower boundary of the continental lithosphere with the convecting mantle. The heavy mineral concentrates were probed and classified into 6 diamond indicator minerals: chromite, high manganese ilmenite, peridotitic pyroxene, clinopyroxene, eclogitic garnet and peridotitic garnet. Of the grains mounted for electron-microprobe analysis: diamond inclusion olivine forsterites, G10-2 peridotitic garnets, diamond inclusion G11 garnets, diamond inclusion clinopyroxenes, and diamond inclusion chromites, all formed in the diamond stability field were found. Further analysis was requested by Dr. Fipke of the picro-ilmenite chemistry to determine the degree of oxidation in the kimberlite magma to determine resorption of microdiamonds. CFM is also performing additional picking of the kimberlite indicator minerals from the company’s large kimberlite, HSM, requested by Dr. Fipke and once the picking and probing is done, RJK will receive the final report from CFM. Dr. Fipke has requested more material from the Nicol Kimberlite discovery, specifically due to the unique diamond inclusion forsterites recovered so far, which have similar whole rock chemistry to forsterites from other diamond deposits analysed by CFM. The RC sample the company recovered from Nicol Lake was only 56 kg. This particular kimberlite is of historical note, as Bernard Baruch's brothers and Richard P. Lydon, staked claims on either side of the lake, in February, 1907, shortly after it was reported that Tiffany and Co were sending a geological team to search for diamonds west of Lake Temiskaming. Considering the scale, and number of discoveries that have been made, the company is finalizing a new, detailed, interactive property map, compiled by Insidexploration to be published for shareholders in the near future.