Tajiri to acquire the Yono Property abutting 7.9 Moz of I+I Gold Resources

In This Article:

VANCOUVER, BC, July 18, 2024 /CNW/ - Tajiri Resources Corp. (the "Company") (TSXV: TAJ) is pleased to announce that it has entered into an agreement, subject to shareholder and Exchange approvals, to purchase a vesting 65% interest in the Yono Property, Guyana, South America, in consideration of 40,000,000 shares of the Company.

Tajiri Resources Corp. Logo (CNW Group/Tajiri Resources Corp.)
Tajiri Resources Corp. Logo (CNW Group/Tajiri Resources Corp.)

Yono is located in close proximity to the central portion of a collective 5.2Moz @ 2.3g/t Au Indicated and 2.7Moz @ 2.5g/t Au of Inferred Resources1 (Figure 2) delineated by G2 Goldfields Inc. (TSX: GTWO) and Reunion Gold Corporation (TSX: RGD) at their respective Oko and Oko West Projects.  At yesterday's closing share prices, G2 and Reunion, had combined fully diluted market capitalizations of CDN$ 1.34 billion and estimated combined project EVs of CDN$ 1.16 billion, equating to a valuation of USD108 per ounce Au.

While Yono contains no defined resources, and has not seen any modern exploration, it is at its closest point ~170m from defined resources, considerable artisanal mining has been conducted on the property, and surrounding exploration data as contained in the NI 43-101 reports of G2 and Reunion suggest the property is prospective as outlined below:

Brief Property Description.

Key Features of the Yono Property are illustrated in Figures 1-9 and elucidated below:

  1. The Yono Property is completely surrounded by the Oko (G2) and Oko West (Reunion) Projects (Figure 1);

  2. The Oko Project contains resources in two deposits Oko Main Zone "OMZ" and Ghanie, while further south Oko West hosts the Kairuni Deposit.  In closest proximity to Yono is Ghanie which strikes sub-parallel to the boundary of Yono and dips 60-70° to the east (Figure 2);

  3. From the boundary of Yono, at its southern end, Ghanie is located 170m to the east and at its northern end 390m (Figure 2);

  4. At its southern end, the Ghanie resource constraining pit shell is ~268m deep and ~306m deep at central Ghanie (Figure 3).  As documented in G2's most recent NI 43-101 report, the pit shell was calculated at a gold price of USD$1900 per ounce with slopes of 35° in saprolite and 45° in resh rock.  No plan view of the pit shell has been published by G2, but we believe from given data its western boundary will be located within tens of metres of the southern part of Yono. 

  5. As last reported, Ghanie's open pit contained resources totaled 236k + 476k ounces in indicated and inferred categories with an additional 128k of inferred underground resources;

  6. As a result of good, recently reported, gold intercepts encountered at depth and outside of  resource wireframes (See G2 press release www.globenewswire.com/news-release/2024/06/25/2903617/0/en/Drilling-Continues-to-Expand-Gold-Zones-at-OKO-10-0m-9-7-g-t-Au-52-3m-2-1-g-t-Au.html)2 drilling is being planned by G2 to test Ghanie along its entire strike to a depth of 500m by year's end (See interview from 22:44 minutes https://www.youtube.com/watch?v=JW-O7KxvNF4 ); 

  7. Between Ghanie and Yono there is a yet lightly explored zone of mineralization- Ghanie West.  The Zone lies along the western contact of the Ghanie /Karuini footwall Granitoid whose eastern contact forms the footwall to the Ghanie and Karuini deposits.  As such this zone "mirrors" the Ghanie – Karouni mineralization along the lower contact of the Granitoid  (Figure 4);

  8. Since 2016 the "Ghanie West" Zone has seen artisanal mining of in-situ mineralization and overlying colluvium over a strike length of ~ 900m.  The pace of artisanal working picked up in early 2023 after a trenching program by G2 evidently exposed gold mineralization.  However, no results for Ghanie West apart from drill hole OKD-36 (see https://www.globenewswire.com/news-release/2020/07/14/2061788/0/en/G2-Goldfields-extends-strike-length-to-1-7-km-at-Oko-and-Reports-17-8-g-t-Au-over-2-5-m-9-5-g-t-Au-over-4-4-m-21-1-g-t-Au-over-2-1-m-and-26-1-g-t-Au-over-1-6-m-in-three-separate-ho.html)3 drilled at the northern end of the zone have been reported by G2 (Figure 4).

  9. Ghanie West potentially strikes into Yono or at least "hugs" the boundary within G2's tenure in its southern ~ 400m of strike (Figure 4).

  10. Situated ~ 700m north, along a direction of 026°, of Yono lies OMZ (686koz @ 9.03g/t Au & 495koz @ 6.4g/t Au of Indicated and Inferred Resources).  The 026°direction corresponds to the mean intersection lineation (L23: 058° to 026°) of measured S2 (008°/88°W) & S3 (357°/68°E)4 surfaces at OMZ.  This intersection lineation corresponds to the major plunge direction of high-grade shoots at OMZ.  S2 is an axial planar foliation developed during a D2 event while S3 fabrics and surfaces are related to later D3 shearing (Figure 5)5.  

  11. Within Yono, and coincident with the projection of the 026° L23 lineation direction is a prominent linear ravine which has been worked by artisanal miners over a length of 550m.  This ravine potentially indicates a yet to be discovered gold source within Yono.  Workings in the upper part of the ravine have included considerable colluvial material. (Figure 5);  

  12. Soil sampling by G2 to the west of the Oko Main Zone shows elongation of 100-500ppb values in a southwesterly direction towards Yono (Figure 6);

  13. West of Yono, shallow (~10-20m) vertical geochemical RC drilling by Reunion to sample beneath duricrust cover, has outlined several zones of gold anomalism (50ppb - >500ppb Au).  One consistent trend of persistently higher anomalism is in line with the L23 direction from the Oko Main Zone, soil anomalism (reported by G2) and the 550m worked ravine within Yono (Figure7).  This zone of gold anomalism appears associated with the contact between high and low magnetic zones which is trending into Yono (Figure 8).  In addition to being structurally controlled gold mineralization within the district tends to be associated within contacts and most prominently contacts between fine grained sediments and any of andesites/mafic volcanics/granitoids or coarse-grained sediments. 

  14. Along and within the northern boundary of Yono, is an area of substantial alluvial and colluvial mining.  Of particular note, a prominent hill underlying the eastern part of Yono has seen extensive colluvial mining going upslope (Figure 9) from the valley floor for some distance.  Thus, a potential gold source within Yono up-hill of these workings is indicated.