Tanzanian Royalty Exploration Corporation

Tanzanian Royalty Reports That Laboratory Probe Results Confirm the Presence of Diamondiferous Indicator Minerals in its Nzega and Igunga Pipes South of Mwadui

    Vancouver, Canada (ots/PRNewswire) - The Company is pleased to report that a range of diamondiferous  kimberlite indicator minerals, including G10 and G3 garnets, have been  identified in four kimberlite pipes on its Nzega and Igunga Project Areas in Tanzania.

    According to Tanzanian Royalty Chairman and CEO, Jim Sinclair, "The  continuing stream of positive diamond indicator mineral results from our  exploration activities in Tanzania suggests the potential for new diamond  discoveries there is very real indeed. We are currently pulling out all the stops to capitalize on the successes we have achieved to date".


    The Nzega Project Area is known to host diamondiferous kimberlite pipes  immediately south of the Company's prospecting licenses where small-scale mining activities are presently being carried out.

    The two kimberlites discovered by the Company last year (See Dec. 8,  2005 News Release) are located about 15 kilometres north of these diamondiferous pipes. Visual results from Mineral Services in South Africa  were received in March 2006 and they proved to be very encouraging (See  April 03, 2006 news release). Visually identified grains from both  kimberlites (NZ151K1 & K2) were subsequently submitted for mineral composition analysis, producing the encouraging results described below.

    To view the discrimination plots associated with this analysis, please visit our website at: www.tanzanianroyalty.com




    A total of 156 garnet grains were submitted for electron microprobe  analysis. Of this total, 34 are eclogitic garnets (G3) while the remainder  are classified as G9 (lherzolitic) and megacrystic garnets as indicated in Figure 1a on the Company's website.

    Diamonds are generally of two types: peridotitic or "P-type" diamonds  and eclogitic or "E-type" diamonds. The former crystallize within  peridotitic source rocks in the Earth's upper mantle and are enriched in  chrome. On the other hand, E-type diamonds crystallize within eclogitic  source rocks in the earth's mantle that are essentially bi-minerallic. In  addition to providing an environment for the generation of diamonds,  peridotitic and eclogitic rocks are also the source of the indicator  minerals that typically occur in kimberlites and are the object of indicator mineral sampling programs.

    No G10 garnets were recovered from this pipe. Nonetheless, it is important to note that G3 garnets are equally as significant as G10 garnets  . While G3 garnets are transported from an eclogitic source, G10 garnets  are disaggregated from a peridotitic source. Garnet inclusions in eclogitic  diamonds are characterized by high sodium (greater than 0.07 wt% Na2O)  enrichment and elevated titanium (Danchin and Wyatt, 1979; Gurney, 1984).  G3 garnets with greater than 0.07 wt% Na2O and TiO2 are defined as Group 1 eclogitic garnets which are commonly associated with diamonds.

    NZ151K2 is mostly typified by Na2O ranging from 0.0 to 0.09 wt%, with  group 2 eclogitic garnets dominating the population as indicated in Figure  1b on the Company's website. A few grains fall within Group 1 eclogitic  garnets, suggesting the possibility of diamonds occurring within the pipe.


    A total of 31 ilmenites were probed and all of them are kimberlitic in  nature. Kimberlitic ilmenites are dominated by Mg-rich varieties (4 to 15  wt% MgO). Although the relationship between ilmenites and diamonds is not  fully understood, the former are used to determine the diamond preservation potential (DPP) of the kimberlite.

    Ilmenites with relatively high MgO and low Fe2O3 are considered to be  indicative of reducing conditions in the parental magma. As reducing  conditions prevent the oxidation of diamonds, kimberlites containing  ilmenites with relatively high MgO and Cr2O3 contents are considered to have high diamond preservation potential.

    Ilmenites from NZ151K2 are characterized by high MgO (4.79 to 14.76 wt  %) contents and elevated Cr2O3 (0.08 - 3.84 wt%) as illustrated in Figure  1c on the Company's website. Such a concentration predicts diamond  preservation if diamonds were sampled by the kimberlite magma passing through the diamond stability field.

    Based on these microprobe results, the NZ151K2 is most likely an eclogitic diamondiferous kimberlite that warrants further evaluation.



    This pipe is located approximately two kilometres north of NZ151K2.  Unfortunately, only a few kimberlitic grains were recovered from this kimberlite, the majority of which were ilmenites.


    A total of 21 ilmenites were probed and all are kimberlitic. Ilmenites  from NZ151K1 are characterized by high MgO (4.90 to 12.99wt %) contents and  elevated Cr2O3 (0.0 - 3.56 wt %) as illustrated in Figure 2 on the  Company's website. Such a concentration predicts diamond preservation if diamonds were sampled by the kimberlite.

    Based on the ilmenite microprobe results, NZ151K1 has a high preservation potential if this kimberlite sampled a diamondiferous source.  However, the lack of potential indicators such as chromites and garnets  lowers the ranking of this particular kimberlite. G10 garnets were  recovered about 400 metres west of this pipe during the Company's initial  stream sampling program. Due to its proximity to NZ151K2 and G10 garnets, further work including re-sampling has been proposed.


    Based on the probed results from the two newly discovered kimberlites  and the established presence of diamondiferous pipes in the area, the Nzega  Project Area remains prospective for the discovery of diamondiferous  kimberlites. Geotherm (thermal gradient) as well as micro diamond analysis  are proposed to further constrain these results before bulk sampling is  undertaken. The lack of mineral indicator grains from NZ151K1 precludes  drawing a firm conclusion on the diamondiferous potential of this  kimberlite. It is noteworthy, however, that G10 garnets were recovered  during the initial loam sampling program although their source has not been defined by either NZ151K1 or NZ151K2. That being the case, more samples will need to be submitted for analysis.


    Two kimberlites were discovered in this area last year during the successful drilling program mentioned earlier. Visual results from Mineral  Services were received in March 2006 and they were very encouraging (See  April 03, 2006 news release). Samples submitted for micro-probing from  these two kimberlites (IG147K1 & K2) returned encouraging results as described below:




    A total of 75 garnet grains were submitted for probing. Out of this  total, four grains (5% of the total grains analyzed) are G10 garnets. The  rest are G9 (lherzolitic) garnets as illustrated in Figure 3a on the  Company's website. In summary, this kimberlite sampled a depleted peridotitic source which may also indicate higher diamond contents.


    A total of 59 ilmenites were probed and all are kimberlitic ilmenites.  Ilmenites from IG147K2 are characterized by high MgO (4.32 to 15.56 wt%)  contents and elevated Cr2O3 (0.11 to 5.22 wt% ) as illustrated in Figure 3b  on the Company's website. Elevated values in MgO and Cr2O3 indicate good diamond preservation potential (Gurney (1984).

    Based on all the probe results, the IG147K2 is most likely a diamondiferous kimberlite where most of the diamonds should have been preserved on their way to the surface. The mineral chemistry of this particular pipe warrants more work by the Company.




    Two garnets were recovered from this kimberlite. These grains (one G9  and one G3) are not enough to assess the potential of the kimberlite with confidence. More samples are therefore needed.


    Like garnets, chromite xenocrysts are known to have formed co- genetically with diamonds. Potential chromites indicating a diamondiferous  source have a chrome content ranging from 60 to 70 wt% Cr2O3, with an  average MgO concentration of 8 to 16 wt% and a TiO2 content of less than 0.7 wt%.

    A total of 15 chromites were probed and are confirmed as kimberlitic  chromites. Chromites from IG147K1 are characterized by MgO wt% ranging from  5.99 to 13.43 and Cr2O3 wt% content of 30.78 to 63.92 wt%. TiO2 ranges from  0.00 to 4.66 wt%. A few grains from this kimberlite plot in the diamond  inclusion and intergrowth fields as illustrated in Figures 4a & b on the  Company's website. A few grains suggest the kimberlite sampled within the diamond stability field thereby upgrading this kimberlite.


    A total of 61 ilmenites were probed and all are kimberlitic ilmenites.  Ilmenites from IG147K1 are characterized by high MgO (7.87 to 15.16 wt%)  contents and elevated Cr2O3 (0.0 to 3.9 wt%) as illustrated in Figure 5 on  the Company's website. A few grains are indicating elevated values in MgO  and Cr2O3. This suggests moderate diamond preservation potential if diamonds were sampled from the first instance (Gurney, 1984).


    Based on the probed results from two kimberlites, the Igunga Project Area has the potential to host diamondiferous kimberlites.


    Mineral composition analysis was conducted by Mineral Services of South Africa.

    Qualified Person

    The Company's Qualified Person is Mr. John Deane, the President of Tanzanian Royalty Exploration, M.Sc., University of Cape Town (1993), a registered scientist with SACNASP (Reg. No. 400005/05).

    Respectfully Submitted,

    James E. Sinclair

    Chairman and Chief Executive Officer

    The Toronto Stock Exchange and American Stock Exchange have not reviewed and do not accept responsibility for the adequacy or accuracy of this release

    Cautionary Note to U.S. Investors - The United States Securities and  Exchange Commission permits U.S. mining companies, in their filings with  the SEC, to disclose only those mineral deposits that a company can  economically and legally extract or produce. We use certain terms on this  news release, such as "measured", "indicated", and "inferred" "resources"  that the SEC guidelines strictly prohibit U.S. registered companies from  including in their filings with the SEC. U.S. Investors are urged to  consider closely the disclosure in our Form 20-F, File No. 0-50634, which  may be secured from us, or from the SEC's website at http://www.sec.gov/edgar.shtml.

    To view news release with diagrams, please visit


ots Originaltext: Tanzanian Royalty Exploration Corporation
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