THE ARGYLE MINE AND ITS DIAMONDS
Australia’s first commercial diamonds

Adapted from Chapman, J. et al. (1996)
Australian Gemmologist. 19, 339-346

Introduction
Western Australia’s Argyle lamproite pipe, the world’s largest producer of diamond by volume, yields brown, yellowish brown, colourless and red to pink diamonds that have a dominantly eclogitic paragenesis. Fancy coloured Type 1a Argyle diamonds typically have a low nitrogen content, mostly in the B-aggregated form. These diamonds are highly strained, colour zoned parallel to {111}, and mostly contain proto/syngenetic inclusions that reveal an eclogitic paragenesis.

The Discovery
Systematic exploration for diamondiferous diatremes in the West Kimberley region of Western Australia commenced in 1969, following the recovery of nine diamonds from the Leonard River by Oilmin N.L. exploration geologists. By 1972 the Kalumburu Joint Venture - consisting of Tanganyika Holdings Ltd, A.O. (Australia) Pty Ltd, Northern Mining Corporation N.L., Jennings Mining Ltd, and Sibeka Societe D’Enterprise et D’Investissements SA - had been formed for the express purpose of exploring the Kimberley Region for diamonds above latitude 19° N.

Early 1976 saw the first successful recovery of kimberlite indicator minerals from routine stream samples taken from the region. This discovery led CRA Exploration to join with the Kalumburu Joint Venturers to form the Ashton Joint Venture (AJV).

In August 1979, the AJV laboratory in Perth reported that two diamonds had been discovered in a sample of gravel collected from Smoke Creek, a small creek that drained north easterly into Lake Argyle. Further progressive sampling upstream led to the subsequent discovery of the Lower and Upper Smoke Creek alluvial deposits, and ultimately, on 2nd October 1979, geologists walked onto and recognised the potentially diamondiferous AK-1 (Argyle Kimberlite No. 1) olivine lamproite pipe. Today this pipe is commonly referred to as the Argyle pipe.

The Argyle Pipe
The Argyle pipe (Fig. 1) is located at the headwaters of Smoke Creek, in a small valley near the eastern end of the Matsu Range. The pipe is located some 120 km from the nearest town, Kununurra, 25 km upstream from Lake Argyle, and 2,200 km north-east of Perth. When first discovered, the Argyle pipe occupied the whole valley floor and had a surface area of about 45 ha. It had a distinctively linear outcrop with a length of 1,600 m, and a width that varied from 150 to 600 m.

Subsequent petrological investigations revealed that the Argyle pipe contained both tuffaceous and magmatic varieties of lamproite. While the predominantly eclogitic diamonds of the Argyle pipe have been dated at an estimated 1,580 million years old, these diamonds were emplaced hydrovolcanically shortly after their formation between 1,100 and 1,200 million years ago. This relatively short storage time (~ 400 m.y.) and the dominance of B-aggregated nitrogen indicates the diamonds experienced relatively high temperatures during this time⁵. Haggerty hypothesised⁶

That the existence of a complex plumbing system below the mobile belt into which the Argyle pipe is emplaced, and a complex annealing history, could account for the dominantly small, highly modified (by dissolution), poor quality B-aggregate rich diamonds that commonly occur in the Argyle pipe.

Having initial proven reserves of 61 million tonnes or ore, with an average grade of 6.8 ct/tonne, and further estimated reserves of 14 million tonnes, at a grade of 6.1 ct/ tonne, the Argyle pipe became the world’s largest volume producer of diamond⁷. Exploration of the Argyle pipe and its surrounds was completed when in 1981 a second high-grade deposit of alluvial diamonds was located on Limestone Creek, a non perennial stream that drains the Argyle pipe to the south-east.

Rapid evaluation and development of the Argyle pipe followed; with mining of the diamondiferous Smoke Creek and Limestone Creek gravels commencing in 1983, and open cut mining of the Argyle pipe commencing in December 1985. Ten years later, a drilling program, initiated to assess diamond grade below the planned open pit bottom to about 300 m, revealed a possible diamondiferous resource of up to 100 million tonnes of ore having an average in situ diamond content of 3.7 ct/tonne.

Continuing studies into the future of the Argyle open pit have led to a decision, during June 1998, not to proceed with underground mining, Instead, a decision was made to cut back the west ridge of the mine to access additional ore (64 million tonnes with a diamond content of 2.58 ct/tonne) suitable for open cut mining. Further it has been suggested that underground mining, by sub-level caving, may come on stream later in the first decade of the 21st century.

Argyle Diamonds
Over the first fifteen years of the Argyle pipe’s exploitation as an open cut mine, annual production has increased substantially and to such an extent that annual production peaked in 1996 at 42 million carats of which almost 2.7 million carats were derived from associated alluvial deposits. Despite a small drop in production to 40.8 million carats in 1998, this rate of production has assured that Australia continues to be the world’s leading producer of diamonds, by volume, but not by value. The reasons for this apparent contradiction are quite simple. First, the average mix of diamonds in the Argyle pipe consists of 55 per cent industrial quality diamond, 45 per cent near gem quality diamond, and only 5 per cent gem quality diamond¹¹. Second, of the small percentage of the gem quality diamonds recovered from the Argyle mine about 95 per cent are brown and brownish yellow hued, some 4 per cent are either colourless or grey, and much less than 1 per cent have the very desired pink to red hues. While Argyle diamond sales has little problem marketing its popular pinks and reds, persistent and innovative marketing has resulted in ever increasing acceptance for champagne and cognac browns, as well as markets for small sized diamonds that are cut from near gem rough by labour intensive Indian manufacturers.

Gemmological Characteristics
After more than a decade of intensive marketing, and following more than a decade of intensive research, it is indeed surprising that so little has been published in the gemmological literature on the characteristics of Argyle’s brown to yellow, pink and colourless diamonds.

It is clear that a significant feature of diamonds from the Argyle pipe is that the majority of them have suffered deformation of their crystal lattice. In instances where diamonds are plastically deformed, and their nitrogen content is low, a brown or pink colour is produced.

In an attempt at collating readily available information on the gemmological characteristics of Argyle diamonds, for the benefit of gemmologists world-wide, a summary of the typical gemmological characteristics of Argyle diamonds has been compiled and is presented as table 1.

Table 1
THE TYPICAL GEMMOLOGICAL
CHARACTERISTICS OF ARGYLE DIAMONDS

References:

• Argyle Diamond Mines Joint Venture (1983) Project briefing. 102 p. ADMJV: Perth.

• Argyle Diamond Mines Joint Venture (1985) Project briefing. 95 p. ADMJV: Perth.

• Argyle Diamonds (1987) From the diamonds of Argyle to the champagne jewels of Stewart Devlin. Argyle Diamond Sales: Perth.

• Ashton Mining Limited (1995) Half yearly report to 30 June, 1995.

• Atkinson, W.J. (1989) Diamond exploration philosophy, practice, and promises: a review.

• In Ross, J. Ed., Kimberlites and related rocks. vol. 2, Proceedings of the Fourth International Kimberlite Conference, Perth, 1986. Geological Society of Australia Special Publication No 14. pp. 1075-1107. Blackwell Scientific Publications: Oxford.

• Chapman, J. and Humble, P. (1991) The cause of colour in Argyle pink and champagne diamonds. In A.S. Keller Ed. Proceedings of the International Gemological Symposium 1991 p. 159-160. GIA: Santa Monica.

• Fardy, J.J. and Farrar, Y.J. (1992) Trace-element profile of Argyle diamonds using instrumental neutron activation analysis. Radioanalytical Nuclear Chemistry, Letters. 164 (5), 337-345.

• Fritsch, W. and Scarratt, K. (1992) Natural-color nonconductive gray-to-blue diamonds. Gems & Gemology. 28, 35-42.

• Haggerty, S.E. (1986) Diamond genesis in a multiply-constrained model. Nature. 320, 34-38.

• Hall, A.E. and Smith, C.B. (1984) Lamproite diamonds - are they different? In Glover, J.E. & Harris, P.G. Eds. Kimberlite occurrence and origin. pp. 167-212. Geology Department, University of Western Australia Publication No. 8. pp. 167-202.

• Hofer, S.C. (1985) Pink diamonds from Australia. Gems & Gemology. 21, 147-155.

• Jaques, A.L., Lewis, J.D. and Smith, C.B. (1986) The kimberlites and lamproites of Western Australia. Geological Survey of Western Australia Bulletin No. 132. pp. 35, 38-59, 239-246.

• Manigan, R. (1983) Diamond exploration in Australia. Indiaqua. No. 38. pp. 27-38.

• Mendelssohn, M.J. and Millidge, H.J. (1995) Geologically significant information from routine analysis of the mid-infrared spectra of diamonds. International Geology Review. 37, 95-110.

• Richardson, S.H., Gurney, J.J., Erlank, A.J. and Harris, W.J. (1984) Origin of diamonds in old enriched mantle. Nature. 310, 198-202

• Rio Tinto Zinc-Consolidated Rutile Australia (1996) RTZ-CRA production report for the quarter ending 31 December, 1995.

• U.S.A. Bureau of Mines (1995) Annual review of gemstones. Mineral Industry Reviews. Table 11.

• Wilks, J. and E. (1991) Properties and applications of diamond. pp. 62-94. Butterworth: Heinemann.