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Following the Silk Road: Rutile in Corundum
By John I. Koivula and Richard W. Hughes
Abstract
This article discusses the role of fiber-optic lighting in gemological microscopy.
If I'd only seen through the silky veils of ardor…
– Joni Mitchell
What follows is a love story. We admit it. Our heart is on our sleeves. We are smitten, head-over-heels in love with the exotic and beguiling internal lattice that gemologists call "silk."
How do we love thee? Let us count the ways. You are the one that lets some of our rubies and sapphires sparkle like the night sky, your asterism such a wonder of nature. Not to mention your beauty as you wink up at us when the light is just so. And finally, you are our guardian, our coalmine canary, a tiny thermometer in our gems, willing to sacrifice your own life to let us know when Man’s ego has grown so large that he thinks he can play God. For this alone, we sing your praises.
Figure 1. A secret silken world
Daggers of rutile lance their way through the interior of this untreated Mogok sapphire. The presence of such perfectly formed rutile needles are proof that this sapphire has not been heated to a high temperature. Photo: John I. Koivula/microWorld of Gems |
Just what is this inclusion we call silk? It is actually composed of tiny crystals formed through a process called exsolution, the "unmixing" of a solid solution. At high temperatures, crystals have more defects and a more-expanded lattice, and thus are better able to absorb impurities. As the crystal cools, defects are reduced. This may force impurities to crystallize out. But because of the constraints placed on their movement by the solid host, impurity atoms are unable to travel large distances. Therefore, rather than forming large crystals, they migrate short distances to form multitudes of tiny needles, plates and particles, along the directions in the host where space permits.
Figure 2. Exaggerated and simplified atomic view of exsolution in corundum
During exsolution, solute atoms migrate together to form their own crystals within the host. The orientation of these crystals is governed by the host structure. As a result, they are exsolved in a specific pattern. Within corundum, rutile (TiO2) unmixes in the basal plane, parallel to the faces of the second-order hexagonal prism {1120}.
Illustration © Richard W. Hughes/RWH Publishing & Books
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One of the keys to recognizing exsolved inclusions is that they always form in a specific pattern within the host. That pattern may be different for different minerals crystallizing within the same host material (for example, rutile is exsolved in corundum in three directions crossing at 60/120° in the basal plane). Virtually all tiny, oriented needle, particle and platelike inclusions found in minerals are formed via exsolution. These inclusions give rise to asterism and cat's eye phenomena. The best manifestation of this is the concentrations of rutile and hematite-ilmenite silk and needles in corundum.
Figure 3. Gossamer…
A rutile silk spider’s web spun beneath the facets of an untreated Sri Lankan sapphire. Photo © Richard W. Hughes |
Among the most diagnostic features of corundum is the white clouds of exsolved rutile (TiO2). According to Edward Gübelin, Gustav von Tschermak was the first to identify rutile in corundum in 1878. Such clouds vary from dense concentrations, which follow, and distort, the crystals’ color zoning, to thinly-woven tapestries. At times, only slender threads or particles are visible, while in other cases knife or dart shapes appear (see Figure 1). Closer examination reveals many of these to be twin crystals with tiny v-shaped re-entrant angles visible at the broad end. They are flattened so thin in the basal plane that, when illuminated with a fiber-optic light guide from above, bursts of iridescent colors are seen, due to the interference of light from these microscopically-thin mineral lances.
The needle clouds just described are termed silk, in analogy to their threadlike pattern and are responsible for the asterism, or star effect. Not only rutile may form silk in corundum; hematite (Fe2O3), ilmenite (FeTiO3) or hematite-ilmenite mixtures have been reported. Rutile in corundum tends to unmix parallel to the faces of the second-order hexagonal prism {1120}, intersecting in three directions at 60/120° in the basal plane. Hematite-ilmenite exsolves in the basal plane parallel to the first-order hexagonal prism {1010}. Thus when both rutile and hematite-ilmenite are present in the same crystal, a 12-rayed star is possible.
Figure 4. Effects of high-temperature heat treatment on rutile silk in corundum
Left: In corundum, rutile exsolves in three directions in the basal plane, parallel to the faces of the second-order hexagonal prism {1120}. Before heating, rutile silk consists of needles which, when highly magnified, are often tiny arrow- or dart-shaped twins with small reentrant angles at the wide end. The rutile needles are extremely thin in cross-section and are generally flattened in the basal plane. Overhead fiber-optic illumination with the microscope will reveal such details.
Right: High-temperature heat treatment causes rutile to be partially dissolved into the corundum, but traces often remain behind, visible with fiber-optic lighting. Each needle, rather than coalescing into one globule, instead dissolves into a series of tiny droplets arranged in the same pattern as before heating. This partially-dissolved silk may be indicative of heat treatment. However, minute exsolved particles, which can occur naturally, may be confused with the partially-dissolved silk of heated gems. The presence of long needles and dart- and arrow-shaped rutile is a strong indication that the gem has not undergone high-temperature heat treatment.
Illustration © Richard W. Hughes |
Figure 5. Canary in a coal mine
When a ruby or sapphire is heat treated at a high temperature, rutile silk is partially resorbed into the crystal, thus clarifying it. But rutile is rarely completely pure. The more impurities present, the more visible the silk "skeletons" following treatment, as shown above. Thus rutile acts as an internal thermometer in the gem, letting us know when Man is trying to play God. Photo © Richard W. Hughes |
Figure 6. Arrows of love
Dart-shaped silken arrows of love. Can anyone not be smitten with such stunning displays? Untreated Sri Lankan ruby. Photo: John I. Koivula/microWorld of Gems |
If I'd only seen through the silky veils of ardor…
What a killing crime this love can be…
– Joni Mitchell
Some shirk battle, afraid of missiles sent their way. Not us. Like Tibetans rounding Mount Kailash, we will gladly prove our devotion on our hands and knees. We are willing pilgrims along the Silk Road. We fear no slings; we relish these god-sent daggers. Let them penetrate our hearts, infect our souls.
What is love? We have gazed at and through the silky veils of ardor. And having journeyed to the other side, we wish for nothing less than to die a sweet slow silken death. We promised you a love story. Oh what a killing crime this love can be…
About
the authors
John I. Koivula is one of the world's most famous gemologists and photomicrographers. Author of several books and more than a thousand articles, he was also the scientific advisor to the famous MacGyver television series.
Richard Hughes (left) is
the author of the classic Ruby & Sapphire and over 100 articles on various aspects of gemology. Many of his writings can be found at www.ruby-sapphire.com.
Notes
First published in May 2005, while John and I were at the AGTA GTC. Working with John was one of the greatest pleasures of my life, sadly far too brief. Looking back, I can only wonder what might have been…
Views expressed in this article are the author's opinions alone and do not necessarily reflect the opinions of any organization that employs him. Those organizations bear no responsibility and assume no liability for content on this website, nor are they liable for mistakes or omissions.
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Posted 14 October, 2011; last updated
14 October, 2011
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