Will see it in the next 1/4 RR as they have buried some of our drilling results from Khartoum in the 1/4ly, but we managed to get 5 holes down, but couldn't get off existing tracks as approval isn't 100% yet..
Or maybe someone else is paying our exploration costs up front?
Just an opinion,
TCG
Khartoum Tin-Silver-Tungsten Project (EVR 100% Interest)
The Khartoum Project comprises five granted Exploration Licence for Minerals (EPM) and one EPM application covering 390 square kilometres. An early-stage reconnaissance field trip has been conducted throughout the region. The aim of the work was to inspect regional access roads and tracks to finalise the upcoming proposed field work and drilling program.
The reconnaissance field trip was limited to public access tracks only whilst statutory notice period timeframes for site access are passing. The initial proposed area of focus for the field work and drilling program is the Boulder-Ahmets area which comprises a 9km by 3km zone of anomalous tin defined by surface geochemistry and geological mapping.
The Boulder-Ahmets area was the focus for detailed geological investigation by Auzex Resources for greisen-style bulk-tonnage tin mineralisation based on the presence of numerous vein- hosted historic tin mines (targeting higher-grade tin mineralisation, previous results from outcrop sampling, and the presence of numerous zones of exposed strong greisen alteration. Initial mapping and rock chip sampling identified strong greisen alteration primarily along two sub-parallel, NNW-SSE trending ridges, each zone extending for over five kilometres. Follow-up channel sampling, comprising continuous 5 metre composite rock chip samples across the extent of the more strongly identified greisen targets, returned numerous anomalous results including:
• 35m at 0.34% Sn
• 49m at 0.22% Sn
• 10m at 0.31% Sn
• 4m at 1.0% Sn
Locally, sericite alteration increases in the vicinity of greisen zones and major fault-fracture zones. Small (<0.01km2), discrete strong greisen altered zones occur throughout the BoulderAhmets prospect.
Almost all rock-chips containing high- grade tin were collected from within these zones, which is also partly reflected in the tin-in-soil data. Greisen alteration zones occur in 3 main structural styles or types:
• Type 1 - As 5-50cm fracture selvedge zones. These selvedges are relatively planar andcontinuous features, with dominantly flat-lying to shallow dips.
• Type 2 - Steeply-dipping ≤15m wide planar alteration zones. These zones all have a dominantNW trend (± local bends/kinks up to 30°and are traceable for up to 1km.
• Type 3 - Larger alteration zones form prominent topographical features throughout the Boulder-Ahmets area.
The geometries of these zones are interpreted as subvertical ‘pipes’ with average width of ~50m and average aspect ratio of 2.3. The dominant long axis is NW trending. EVR are continuing the assessment of the numerous greisen zones in the Boulder Ahmets area through rock chip sampling to determine the lateral extent of tin mineralisation and to define additional drill targets.
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