Diamond Fields Updates on Marine Diamond Mining and Liberian Diamond and Gold Exploration

Diamond Fields International Ltd. (DFI) is progressing on its marine diamond mining project in Namibia and providing continuing results from its diamond and gold exploration in Liberia.

Marine diamond mining

The recently completed development program in the Diaz Reef section of DFI’s licences made recoveries of diamonds of larger average stone size than Marshall Fork and significantly, the grade of the area to be mined is estimated to be roughly double the previously announced grade for the company’s resource in this area. The successful trenching program in the Elephant basin and Reef Edge features has led to mv DF Discoverer returning to full mining mode. The high-grade deposit found in Elephant basin is still open to the west and south while the deposit found in Reef Edge is open to the north. Further development work is planned to expand the area of high-grade material.

Roger J. Daniel, president and chief executive officer, commented, “The successful outcome of this development program is very encouraging and improves our flexibility in mine planning and should result in improved production and revenue levels.”

The company also made sales of a total of 2,581 carats of diamonds recovered from the trenching program at an average price of $166 (U.S.), for total gross proceeds of $428,523 (U.S.). The prices received reflect traditionally thin year-end and early new year markets for rough goods. However, the overall market outlook remains strong.

Kimberlite exploration in Liberia

DFI is continuing surface evaluation of the initial two of the 10 high-priority kimberlite targets so far identified on the Grand Cape property in western Liberia. One-hundred-kilogram samples of weathered kimberlite material from three locations will be tested for the presence of diamonds. Reconnaissance stream sampling is continuing with about 65 per cent of the property sampled to date.

Microprobe analysis of kimberlite indicator minerals (KIM) from sampling and pitting indicates that the source kimberlites have sampled the diamond stability field and have a high probability of hosting diamonds. The garnet suite includes both lherzolitic and eclogitic compositions, with the lherzolitic garnets showing a well-defined trend of increasing chronium trioxide with calcium oxide. Of the 167 garnet grains analyzed, 20 per cent plot in the G10 field and a significant number of high-interest G10D garnets are also present. Kimberlitic ilmenite and rare diamond inclusion-type spinels were also found in these samples. Textures of grains recovered from pit sampling indicate proximity to source.

Gold exploration

DFI continues to explore the Henry Town and Barteajam gold targets in Liberia. Although outcrop is scarce, both prospects are believed to consist of high-grade, gold-bearing quartz veins in a mafic volcanic host rock and both are thought to be shear zone related. Artisinal miners are recovering coarse gold from regolith (weathered in situ rock) in both areas and DFI’s sampling has returned anomalous soil, rock chip and stream sediment samples, indicating mineralization is present over extensive areas on the kilometre scale. Mr. Daniel added, “Our Liberian geological team will shortly begin more detailed exploration work to better define these prospects as soon as orientation sampling is completed and the most prospective zones identified.”

KIM samples are jigged in the field to create approximately one kilogram of heavy mineral concentrate, sent to Nexo Labs in South Africa (ISO14001 accreditation has been applied for) and processed by Sophia Napier, a mineralogist with more than 10 years industry experience. Selected indicator minerals are microprobed at the analytical facility of the University of Johannesburg (a merger between Rand Afrikans University and Wits University). Gold samples are sieved and dewatered in the field and sent to Anglo American Research Labs in South Africa for fire assay and ICP analysis. Results of the sampling programs have been reviewed, verified (including sampling, analytical and test data) and compiled by the DFI geological staff supervised by Randal Cullen, PGeol, a qualified person as indicated under NI 43-101.

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