Hong Kong, March 2010
Spinel: A Gemstone on the Rise
Dr. Michael S. Krzemnicki
Swiss Gemmological Institute SSEF Switzerland
Spinel of 110 ct from Tajikistan
© Swiss Gemmological Institute SSEF
1 What is Spinel? Spinel as a gemstone is mainly magnesium-aluminium-oxide
MgAl2O4
More general: the spinel group
2+ 3+ (Me ) (Me )2 O4
Me2+ tetrahedral coordination Me3+ octahedral coordination
Cubic
© Swiss Gemmological Institute SSEF
Colours of Spinel
Pure MgAl2O4 is colourless.
Trace elements such as chromium, vanadium, iron, cobalt produce many different shades of colours such as red, pink, orange, purple, blue, black...
© Swiss Gemmological Institute SSEF
2 Crystal Shape of Spinel
Most spinel crystals are octahedral, but also other cubic forms exist such as rhombic dodecahedra...
© Swiss Gemmological Institute SSEF
Crystal Shape of Spinel
Spinel octahedron
But remind: Rubies may also have a pseudo-octahedral “shape”
© Swiss Gemmological Institute SSEF
3 Crystal Shape of Spinel
Spinel octahedron
Spinel crystals are often twinned.
© Swiss Gemmological Institute SSEF
Formation of spinel
Many gemquality spinels are formed in marbles, similar to rubies. - Spinel in dolomite marble (Mg-Ca-carbonate) - Ruby in calcite marble (Ca-cabonate)
© Swiss Gemmological Institute SSEF
4 Formation of spinel
Chondrodite © H.A. Hänni. SSEF
This 6.76 ct clinohumite is a fine example of the "sunflower stone" from Kuh-i-Lal. © Wimon Manorotkul / Pala International Pargasite © C.Hauzenberger
Often occurring together with magnesium minerals such as clinohumite and chondrodite (Mg-Fe-silicates), phlogopite (K-Mg mica), pargasite (Na-Ca- Mg-Fe amphibole).
© Swiss Gemmological Institute SSEF
History of spinel
In ancient times, spinel was not known as a mineral and many of the large historic „balass rubies“ from Central Asia and Persia were later identified mineralogically as spinels.
One of the finest examples of a Badakhshan spinel is the Black Prince “ruby“ (~ 140 ct) which is mounted in the front of the Imperial State Crown of Great Britain.
These large and often just slightly polished and engraved spinels went through the hands of the kings and shas of central Asia, Persia and India and were only described by a few adventurous European travellers such as Jean-Baptiste Tavernier and others at that time.
© Swiss Gemmological Institute SSEF
5 Crystal Shape of Spinel
© Swiss Gemmological Institute SSEF
Exceptional historic spinel necklace certified at SSEF
© Swiss Gemmological Institute SSEF
6 Properties of Spinel Spinel is cubic,
RI for natural gem quality spinels usually approx. 1.718
SG 3.60
Lustre: High vitreous
Hardness: 8 (Mohs scale)
Clarity: Often clean stones, no cleavage
Colour: by trace elements in many shades from red, pink, orange, purple, to blue and black no pleochroism, usually no colour zoning red spinels often with Cr-luminescence, resulting in bright red colour
© Swiss Gemmological Institute SSEF
Properties of Spinel
© M.S. Krzemnicki, SSEF
Most spinel crystals are octahedral, bFaucte atelds ore do tshpeinre lc (u2.b2i4c c fto) wrmiths s epixniesl tc rsyustcahl (15 ct), both from Burma. a© sPh ortho: oMmia Dbixiocn, Pdaolagdeemsc Iantehrneatdionral ...
Octahedral shape perfect fitting for cutting proportions
© Swiss Gemmological Institute SSEF
7 Properties of Spinel
Pure spinel from Pamir (Tajikistan) of approx. 40 cts. Rubies from Vatomandry, Madagascar (above) and Mong Hsu, Burma (below)
Spinels are generally rather pure gemstones without distinct colour zones, in contrast to rubies, which are often quite included and fractured and colour zoned !
© Swiss Gemmological Institute SSEF
Spinel is usually not treated!
A 1.17 ct spinel from Tanzania before (left) and after heating for 5 hrs at 1400 °C, in oxidizing conditions (right). Ruby heated and with © S. Saeseaw et al., GIA (2009) glassy residues in healed fissures. © H.A. Hänni, SSEF Heating experiments on spinels show no or only limited enhancement, apart from clarifying some turbidity in spinel. Heated spinels are detected by microscopy and Raman-microspectrometry (Photoluminescence) at SSEF.
© Swiss Gemmological Institute SSEF
8 Synthetic spinel
Most are produced by a flame-fusion process (Verneuil).
Visit at Djevahirdian SA, Monthey, Switzerland
© Swiss Gemmological Institute SSEF
Verneuil synthetic spinel
Large quantities are produced for technical purposes (e.g. scratch resistant glasses for watches).
Usually these synthetic spinels are highly pure, and often show a colour range from blue - light blue, green, and colourless.
Verneuil synthetic spinel. Experiences gemmologists generally can separate them easily from natural spinels based on microscopy, UV fluorescent reactions and slightly increased values for RI (1.725 instead of 1.718) and SG ( 3.65 instead of 3.60).
The difference in these physical properties is due to a non-stochiometric chemical composition of these Verneuil synthetic spinels, i.e. they contain too much aluminium. Airbubbles in a Verneuil synthetic spinel. As a consequence, there crystal structure is slightly deformed, resulting in strain double refraction under the polariscope and in broadening of the peaks in the Raman spectrum.
© Swiss Gemmological Institute SSEF
9 Flux-melt synthetic Spinel
Flux-melt synthetic spinels are known since the 90ies, but quite rare. As a consequence of the increased interest and value of red and intense blue spinels, the SSEF has tested recently a number of such synthetic spinels from the market.
Flux residue in synthetic spinel
Flux-melt synthetic spinel form as nice octahedral crystals, mostly in saturated red and blue colours. These stones are not easy to separate from natural spinel.
© Swiss Gemmological Institute SSEF
Raman spectra of flux-melt synthetic spinel
© Swiss Gemmological Institute SSEF
10 Luminescence spectra of flux-melt synthetic spinel
© Swiss Gemmological Institute SSEF
Sources of spinel
As for ruby and sapphire, spinel of fine quality is often certified. The clients often require an origin determination of the spinel, especially for stones from Burma, Tajikistan (Pamir), Vietnam and Tanzania.
At SSEF, origin determination is based on microscopy (inclusions), trace element distributions and UV-Vis and Raman spectroscopy. The origin of spinels can not be determined in all cases due to overlapping properties of spinels from different sources.
LA-ICP-MS, for analysis of trace elements and isotopes.
© Swiss Gemmological Institute SSEF
11 Major sources of spinel
Tajikistan
Afghanistan Vietnam Burma (Myanmar) Siam (Thailand)
Ceylon (Sri Lanka)
Tanzania
Madagascar
© www.mygeo.info
© Swiss Gemmological Institute SSEF
Tajikistan (Pamir)
Tajikistan is a classical source for large spinels since ancient times. they usually show a pinkish red to pink colour.
© Swiss Gemmological Institute SSEF
12 Tajikistan (Pamir)
Pierre Lefèvre, gemmologist at SSEF with a superb spinel of 110 cts from Tajikistan.
© Swiss Gemmological Institute SSEF
Burma (Myanmar)
Spinel from Burma is highly appreciated in the market especially for its outstanding saturated red colour.
© Swiss Gemmological Institute SSEF
13 Burma (Myanmar)
But Burma is also the source of spinels in many pastel colours.
© Swiss Gemmological Institute SSEF
Madagascar
Colour changing spinel (84 ct) from Madagascar
© Swiss Gemmological Institute SSEF
14 Vietnam
Apart from red and pink spinels, Vietnam has recently produced fine spinels in light purple, light blue and saturated cobalt blue.
© Swiss Gemmological Institute SSEF
Vietnam
Characteristic crossed inclusions in spinel from Vietnam.
© Swiss Gemmological Institute SSEF
15 Tanzania
Main sources for spinel in Tanzania are Matombo, Mahenge and Tunduru in the south.
Matombo
Mahenge Tunduru
© Swiss Gemmological Institute SSEF
Tanzania, Mahenge
© Swiss Gemmological Institute SSEF
16 Tanzania, Mahenge
© H.A. Hänni, SSEF Oriented planes of fine „dust“ precipitates in spinel from Tanzania
© Swiss Gemmological Institute SSEF
Tanzania, Mahenge
Matombo
Mahenge
© Swiss Gemmological Institute SSEF
17 Tanzania, Mahenge
© Swiss Gemmological Institute SSEF
Tanzania, Mahenge
Spinel from Mahenge (3.4 ct), showing a characteristic attractive bright red colour.
Geological map of the Mahenge fold nappe. Indicated in blue are the marble rocks. The spinels (and rubies) are found at different spots in these marbles or near-by eluvial and aluvial gravels.
© Swiss Gemmological Institute SSEF
18 Tanzania, Mahenge
In 2007, a 52 kg (260‘000 cts) spinel was discovered in Mahenge. Although only partly of gem quality, this resulted in a sudden supply of large (up to 50 cts) and many small vibrant pinkish red spinels (totally several
© W. Spaltenstein and D. Weinberg, Multicolour, Thailand thousand carats) in the market.
© Swiss Gemmological Institute SSEF
Trip to Mahenge, October 2009
© Swiss Gemmological Institute SSEF
19 Tanzania, Mahenge
© Swiss Gemmological Institute SSEF
Tanzania, Mahenge
Mahenge Morogoro Province
© Swiss Gemmological Institute SSEF
20 Going to the mine: Epangko, south of Mahenge
© Swiss Gemmological Institute SSEF
Epangko, Spinel mines
Gemmologist Walter Balmer at the Epangko spinel mines.
© Swiss Gemmological Institute SSEF
21 Epangko, Spinel mines
© Swiss Gemmological Institute SSEF
Epangko, Spinel mines
© Swiss Gemmological Institute SSEF
22 Epangko, Spinel mines
© Swiss Gemmological Institute SSEF
23 © Swiss Gemmological Institute SSEF
Epangko, Spinel mines
© Swiss Gemmological Institute SSEF
24 © Swiss Gemmological Institute SSEF
Epangko, Spinel mines
© Swiss Gemmological Institute SSEF
25 26 Thank you for your attention...
High Noon in Mahenge...
27