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    DiamonEx
    Limited
    ABN 26 091 951 978
    Sky Level
    301 Coronation Drive
    Milton Qld 4064
    Australia
    Telephone: +61 7 3369-6399
    Facsimile: +61 7 3369-6077
    e-mail:
    [email protected]
    Postal Address:
    PO Box 1357
    Milton Qld 4064
    ASX ANNOUCEMENTS
    AUSTRALIAN STOCK EXCHANGE 3 February 2005
    INDICATOR MINERAL CHEMISTRY ANALYSES
    MARTIN’S DRIFT DIAMOND PROJECT
    The directors of DiamonEx Limited are pleased to present the first indicator mineral
    chemistry analyses of grains recovered from the +1mm fraction of 361 samples taken over an
    approximately 35 Hectare photographic anomaly in the Martin’s Drift Diamond Project,
    North-East Botswana.
    SUMMARY RESULTS:
    • 40 pyrope garnets recovered, 14 of which classified at G10 garnets
    • 63 ilmenites recovered. Composition of approximately 50% of these indicate that if
    diamonds are present in the source body, they are likely to be preserved
    • 11 spinels recovered. Analysis of available spinels provide high-interest trends,
    indicating a probable diamondiferous source
    Mineral chemistry analysis of the 40 pyrope garnets recovered form this size fraction indicate
    that 14 plot within the G10 field as described on the standard interpretive graph based on the
    work of Gurney (1984).
    Assessment of analyses included a comparison of the visible similarities and differences in the
    trends exhibited by the 40 pyrope grains recovered from samples over the anomaly, with the
    available mineral chemistry trends of pyrope garnets from the nearby kimberlites K003, K004
    and K006. No garnet data is available from kimberlite K005. A summary of this comparison
    is attached as Table 1.
    Given that the analyses available to DiamonEx at this juncture derive solely from grains
    recovered from the +1mm size fraction, better interpretations of the trends will be possible
    when the analyses of grains from the -1+0.5mm fraction become available. However, there
    are sufficient differences evident in the current analyses to suggest that an unknown source or
    sources is/are at least partly contributory to the population of grains recovered over the
    photographic anomaly.
    The analyses of the spinel and ilmenite populations complement the results of the pyrope
    analyses, indicating that co-existing diamonds should have been present in the source rock at
    the time of intrusion and would have been preserved at the time of emplacement.
    Approximately 50% of the ilmenites recovered contain 8% or greater weight percentage
    magnesium oxide (MgO), indicating that if diamonds are present in the source body, they are
    likely to be preserved. Only 11 spinel analyses are available from this size fraction, but highinterest
    trends, indicating a probable diamondiferous source, may be discerned in the graphs
    based on the work of Fipke et.al. (1995).
    Three diamonds were also recovered from this size fraction, as reported in an earlier
    announcement.
    These observations, coupled to the very strong indications of a nearby source, derived from
    the previously reported surface texture work on these grains, serve to heighten the interest of
    this anomaly.
    Table 1
    Trend Similarities Trend Differences
    K003
    Pyrope Garnets
    (580 grains)
    The percentages of grain
    analyses on either side the
    lherzolite line.
    A clustering of analyses around 4
    wt% Ca0, 8 wt% Cr2O3 – an
    embryonic cluster is seen in the
    grains from the anomaly at 5.2 wt%
    CaO, 8.8 wt% Cr2O3;
    No grains with <4 wt% Cr2O3;
    Grains with an eclogitic paragenesis
    (0 wt% Cr2O3)
    K004
    Pyrope Garnets
    (347 grains)
    The percentages of grain
    analyses on either side the
    lherzolite line
    No grains with <2 wt%; No grains
    with <4 wt% Cr2O3;
    Grains with <2 wt% CaO;
    No grains clustering in the G10 field.
    K006
    Pyrope Garnets
    (74 grains)
    Some clustering of G9 grains
    at 6.5 wt% CaO, 8-9 wt%;
    Grains with <4 wt% Cr2O3.
    Dissimilar distributions of grain
    analyses on either side of the
    lherzolite line.
    Paul Crawford
    Company Secretary
    For further information, please contact:
    Dan O’Neill (Managing Director) Greg King (Chairman)
    +61 7 33696399 (Office) +61 7 33696399 (Office)
    +61 7 33696077 (Fax) +61 7 33696077 (Fax)
    +61 407596942 (Mobile) +61 411473730 (Mobile)
    [email protected] (Email) [email protected] (Email)
 
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