4. Bain (2018) however remains
positive over the long-term.
Million Cts
Marquise Capital
Middle class in China and India (millions of people)
Bain 2018
6. De Beers sales in US$ m
De Beers records lower sales amid macroeconomic uncertainty
Mining Weekly 21 May2019
De Beers May 2019
7. Polished Diamonds inventories - indexed
Edahn Golan 13 May 2019
Inventories rising – Golan/Rapnet
◊ The industry is supply and not
demand driven (Rapaport 2019)
◊ Golan (2019): Diamond industry
‘out of balance’
8. Paul Zimnisky May 2019
0.75 – 1.25 cts
0.13 – 0.42 cts
Rough Diamond price performance by size
3 – 4 cts
9. ◊ Most diamond mines produce a
range of goods including very small
low-quality stones to larger one.
◊ To make their operations
worthwhile economically most
miners need to sell the entire range.
◊ These mines will stop operating if
they cannot sell low and mid-range
goods.
◊ But only very few mines that also
produce large high-value stunning.
Run of Mine production
10. ◊ Synthetics, disclosed and undisclosed.
◊ New supply from Gahcho Kué, Renard,
Liqhobong, Ekati Misery pipe.
◊ Higher recoveries of smalls due to XRT
technology.
◊ Indian manufacturer troubles, especially
those that deal in smaller goods.
Catalysts for price dislocation
Gahcho Kué - 4.5 mct/a
Rapaport 2019
Mountain province Diamonds
Synthetic
diamond
11. Projected market share of Lab Grown Diamonds (LGD)
FT Oct2017
• By 2030 LGD will have some 10% share of the market.
• “It all comes down to consumer choice - Uber did not hurt the
taxi industry” (Amish Shah 2017).
• Producers of natural gems are unnerved by cheaper, cleaner
synthetic jewels (FT 2017).
According to Chaim Even-Zohar
(2017):
◊ Synthetics have become a real
threat to the natural diamond
producers.
◊ Exploration money will dry up
because synthetics are
increasingly considered a pure,
more affordable economic
substitute.
12. Science & Sparkle
◊ Lab-grown diamonds share the
same physical, chemical and
optical characteristics as rare,
natural diamonds.
◊ But the process to create them
is different from nature, so
while they are neither as
valuable or precious, they are
just as sparkly.
Hello, we're Lightbox (Element six – part of De Beers Group)
Lightbox 2019
‘Our diamonds are laboratory-
grown. In soft shades of pink and
blue and white’
13. Lab Grown Diamond
(LGD) prices
LGD wholesale transaction
prices % change:
Q1 2019 vs Q4 2018
◊ Compared to wholesale
transaction prices of
natural diamonds, prices
of LGD are on average 65–
84% lower (Golan 2019).
◊ Rapaport (May 2019)
shows that retailers can
make higher profit
margins selling synthetic
diamonds.
14. 88.2 ct stone (size of a
pigeon egg) sold for
US$ 13.8 M
GIA
The value of the big stones
Lesedi La Rona:
• Found 2015
• Uncut: 1,109 cts
• Sold 2017 for US$53m
Graff
15. Karowe Mine (Lucara Diamond)
Lucara 2019
Sold in 2017 for
$53 M USD
◊ 7 ha kimberlite
◊ Orapa Kimberlite field, Botswana
◊ Discovered 1970: mine opened 2012
◊ 2nd (1,758 cts) and 3rd (1,109 cts) largest
diamonds ever found in 2019 and 2015
respectively.
Apr 2019
Lesedi was cut into the
largest square emerald
cut diamond – 302.37 cts.
16. ◊ +10.8 cts (Specials), contribute ~5% by volume and 70%
by revenue.
◊ Since 2012 some 181 diamonds +100 cts, and 13 diamonds
+300 cts have been found.
◊ 187 diamonds sold for more than US$1 M each and 10
single diamond for more than US$10 M since 2012.
Lucara 2019
Karowe Mine (Lucara Diamond)
17. 121.3 ct
2016
The Cullinan Diamond
3,106.8 cts (0,62 Kg)
1905
424.9 and 209.2 cts
2019
Cullinan Mine (Petra Diamonds)
Sold for
US$15 M
19. 404 cts
2016
US$ 16 M
131 cts
129.6 ct
120.4 cts
2018
Luo mine (Lucapa Diamonds)
◊ An alluvial mining operation
◊ Exploring a large kimberlite field
within its concession
◊ Cuango drainage basin in Angola
20. ◊ Proximal to the Luo mine are numerous
kimberlites which are being tested for the
source of the large Type ll stones.
◊ In addition, Lucapa Diamond operates a second
large diamond producing mine Mothae in
Lesotho. This is next to Letšeng-la-Terae of
Gem Diamonds
173ct
2016
Luo mine (cont.) ◊ +10.8cts (Specials): 30% by weight, >85% of
revenue.
◊ +5 cts: 45% by weight, 92% of value.
◊ Recently some large stones were valued in
excess of ~25,000 US$/ct.
22. 138 cts
495 cts
Sold for
US$10.4 M
Letšeng-la-Terae (Gem Diamonds)
◊ Main pipe 17 ha, satellite pipe 5.2 ha
in the highlands of Lesotho.
◊ Highest average dollar per carat
kimberlite diamond mine.
23. Hope Diamond (Type llb)
◊ Found in the early 1600s, India
◊ Cut: 45.5 ct
◊ Insured for US$250m
◊ At Smithsonian
Blue diamonds (Type llb)
Moon of Josephine (Type llb)
◊ Found 2014 Cullinan as a 29.6 cts
◊ Cut to 12.03 cts – sold for US$48.4 M
24. 122.5 cts Blue diamond recovered
in 2014 sold for US$ 27.6 m
The Cullinan Dream
Cut into 24.18 cts fancy intense blue
sold for US$25.4 M in 2016
25. Diamond ‘Types’
◊ Type I Diamond
◊ Contain structurally bonded
nitrogen
◊ Often yellow in colour
◊ Good crystal shapes
◊ Type lla/llb Diamond
◊ No or low Nitrogen content
◊ Usually colourless - Type lla
◊ Skewed to larger sizes
◊ High proportion of white
stones (D colour)
◊ < 10% luminesce
◊ Type llb
◊ Blue (contain boron)
◊ No or low N content
◊ High value
Type llb
Type lla
Type l
Type ll producers
include:
◊ Karowe
◊ Letšeng
◊ Mothae
◊ Jagersfontein
◊ Cullinan
◊ Jwaneng
◊ Luo (Alluvial)
26. ◊ Larger diamonds are more
likely to be D colour
◊ Type ll diamonds are more
abundant in the larger sizes
◊ Type ll diamonds very
slightly included to flawless
(substantially fewer
inclusions than Type l)
Smith et al. 2017
227ct
Type ll represent a high proportion of large D colour diamonds
27. Atypical Kimberlite Processing
Plant these days would
include:
◊ Autogenous milling
◊ Hybrid Crusher
◊ XRT/BV recovery units
◊ Waste Sorting (if country
rock rich)
Autogenous milling:
◊ Self grinding of the ore
◊ Not crushing
◊ Preservation of large diamonds
◊ Installed at Cullinan and Karowe
Autogenous Milling as Opposed to Conventional Crushing
28. X-Ray Transmission (XRT)
◊ XRT – Sensor identifies the
atomic number (C)
◊ XRT can recover low
fluorescence and non-
fluorescence diamonds
◊ 200 tph machines on the
horizon
◊ Replaces DMS for + 8 mm
material, shortly +4 mm
material
◊ Recovers diamonds before
secondary or tertiary crushers
◊ Diamond breakage minimised
◊ Feed preparation is critical
29. Stachel and Harris, 2008
◊ Peridotitic: base of the thick
Lithosphere
◊ Eclogitic: subduction related
The source of the Type ll diamonds
◊ Most of Type l diamonds form at the base
of the lithosphere (150 200 km depth)
◊ The majority of the Type ll diamond form at
600 to 800 km depth and are also referred
to as ‘deep’ diamonds
31. Formation of CLIPPIR diamonds
Smith et al. 2016
CLIPPIR = Cullinan-Like, Inclusion-Poor, relatively Pure, Irregularly shaped,
Resorbed.
200 km
650 km
◊ Metallic iron segregates aided by
deformation of the subduction slab
in transition zone.
◊ Liquid metal evolved to Fe-Ni-C-S.
◊ Diamond crystallization occurs
within metallic liquid (P ~ 12 to 25
Gpa) under reducing conditions.
◊ CaSi-perovskite inclusions.
◊ C saturated by increase P, adding
more C, or increasing S.
◊ After growth diamonds are
physically separated and
transported upwards.
32. Smith et al. 2018
1. Serpentinization of seafloor introduces
Boron into oceanic lithosphere
2. Subduction and metamorphism of
serpentine to DHMS
3. Breakdown of DHMS yields hydrous
Boron-rich fluids.
4. Crystallisation of Boron-bearing
diamonds triggered by Redox reactions
5. Vertical transport by upwelling mantle
and kimberlites
Formation of Type IIb (Blue) diamonds
Asteria
33. Craton
Kimberlite intrusions
Diamond Bearing
Diamond Mines
Region
Point
Point
Point
0 1,000
kilometers
CLIPPIR diamonds are
found:
◊ Near the edges of
cratons: Luo,
Karowe,
Jagersfontein,
Letšeng, Mothae
◊ Close to major
discontinuity within
cratons: Cullinan,
Jwaneng (?)
Where to explore for CLIPPIR diamonds
34. Exploring for sources of large stones
◊ Approx. 7000 known
kimberlites
◊ Some 70 have been or are
mined (1%)
◊ Only a maximum of 10
diamond mines are
known to produce
CLIPPIR diamonds (0.1%
of total kimberlites)
◊ Mainly primary
kimberlites but also
secondary deposits
• Kimberlites with large stones are found on the margin (Letseng, Mothea, Jagersfontein, Karowe) or major tectonic
boundaries within (Cullinan, Jwaneng) the Kaapvaal Craton: and the alluvials of Luo along the Kasai Craton.
• Large diamonds form in subducted blocks pushed deep down into the lower mantle.
• Exploration will have to refocus to identify those kimberlites that contain ‘deep large diamonds’.