Gemology Books Bibliography

Gemology Books Bibliography

Explore books on gems, gemology, jewelry and mineralogy in Four Treasures, the Lotus Gemology reference database. This bibliography brings together matching book records from the collection, with publication details, abstracts and cover images where available.

Gemology Book References

The list below matches books concerning gemology and related subjects in the database's searchable fields. Some works cover several branches of gems, jewelry or mineralogy.

2,461–2,480 of 3,675 matching references

The gemological properties of the Sumitomo gem-quality synthetic yellow diamonds

Journal Article
Shigley, J.E., Fritsch, Emmanuel, Stockton, C.M., Koivula, John I., Fryer, C.W. and Kane, Robert E. (1986) The gemological properties of the Sumitomo gem-quality synthetic yellow diamonds. Gems & Gemology, Vol. 22, No. 4, Winter, pp. 192–208.
Record No. 2007  |  ISBN/ISSN: 0016626X  |  Sinkankas/Born No.: NIS/NIB  |  RWHL
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The distinctive gemological properties of gem-quality synthetic yellow diamonds produced by Sumitomo Electric Industries are described; these commercially grown deep yellow single crystals reach sizes up to 2 carats, though they are currently marketed for industrial use only, typically in pieces up to about 0.40 carat. These synthetic diamonds can be identified by their ultraviolet fluorescence (inert to long-wave, greenish yellow or yellow to short-wave), unusual graining, veining, and color zoning visible under magnification, as well as the absence of distinct absorption bands in their spectra.

Gem minerals from the Embilipitya and Kataragama areas in Sri Lanka

Journal Article
Zwaan, P.C. (1986) Gem minerals from the Embilipitya and Kataragama areas in Sri Lanka. Australian Gemmologist, Vol. 16, No. 2, pp. 35–40.
Record No. 1930  |  Sinkankas/Born No.: NIS/NIB  |  RWHL
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Gem minerals from Embilipitiya and the Kataragama region of southern Sri Lanka are described through field observations, gemological measurements, microscopy, X-ray diffraction, and selected electron-microprobe analyses. Unlike the predominantly alluvial deposits around Ratnapura, both areas yield minerals from residual soils worked in shallow pits. Chemical corrosion is common, but the preservation of crystal faces, especially near Kataragama, indicates proximity to source rocks and contrasts with the rounded pebbles produced by prolonged transport. Embilipitiya is notable for substantial quantities of several unusual gem minerals, including orthopyroxene, cordierite, kornerupine, and reported scheelite, together with garnet and spinel. Nearly colorless orthopyroxene is identified as exceptionally magnesium-rich enstatite, with quartz inclusions and a strong ferrous-iron absorption line near 506 nm providing useful diagnostic evidence. Reddish brown orthopyroxene contains appreciably more iron and commonly exhibits liquid and two-phase inclusions. Nearly colorless cordierite has weak pleochroism, low refractive indices, and a magnesium-rich, iron-poor composition; its similarity to enstatite in appearance makes density and optical testing important. Kornerupine occurs abundantly as corroded or fractured material ranging from light brownish yellow to grayish green, with strong dichroism and variable iron contents. Its identification is supported by density, optical properties, and characteristic X-ray diffraction patterns. Unusually shaped quartz crystals resemble apophyllite because of strongly developed rhombohedral faces, while two purchased scheelites were reported to originate from Embilipitiya but were not confirmed by direct collection there. The Kataragama region contains more familiar gem assemblages, including sapphire and other corundum, spinel, almandine, hessonite, and brown tourmaline. Amarawewa spinels display well-developed octahedral faces and a strong absorption band near 549 nm. Scapolite contains marialite-rich inclusions interpreted as exsolution products, while hessonite from Tikiriyawewa contains numerous small transparent crystals that produce a granular appearance. Kochipadana yields relatively large corundum crystals, well-formed spinels, tourmaline, and less common apatite, titanite, actinolite, diopside, and green spodumene identified as hiddenite. The latter is characterized by strong dichroism, chromium absorption lines, a reddish Chelsea-filter reaction, and fluid inclusions. The account emphasizes the mineralogical diversity of these residual deposits, the diagnostic importance of combined testing, and the potential of Kochipadana as a source of sapphire, geuda, and additional gem-quality hiddenite.

On the problem of using the gallium content as a means of distinction between natural and synthetic gemstones

Journal Article
Schrader, H.-W. (1986) On the problem of using the gallium content as a means of distinction between natural and synthetic gemstones. Journal of Gemmology, Vol. 20, No. 2, April, pp. 108–113.
Record No. 1562  |  ISBN/ISSN: 221252  |  Sinkankas/Born No.: NIS/NIB  |  RWHL
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Gallium concentrations in emerald, corundum and chrysoberyl are evaluated as a proposed means of distinguishing natural from synthetic gemstones. Because gallium and aluminium have similar ionic radii and the same valence, gallium can substitute for aluminium in these minerals, but its abundance depends on geological conditions and the materials used in synthesis. The study tests earlier suggestions that gallium concentrations above approximately 50–200 ppm establish natural origin in corundum, that lower concentrations indicate synthesis, and that measurable gallium identifies natural alexandrite. Neutron activation analysis results obtained by the authors and incorporated from an earlier investigation cover 32 emeralds, comprising 22 natural and 10 synthetic specimens; 18 corundums, comprising eight natural and 10 synthetic specimens; and 16 chrysoberyls, comprising six natural alexandrites, two synthetic alexandrites and eight other natural chrysoberyls. The results demonstrate overlap and important exceptions to the proposed criteria. Natural and synthetic emeralds have similar gallium ranges, with several synthetic samples containing concentrations comparable to natural stones. Four natural corundums contain less than 50 ppm gallium, while only one of the eight natural samples exceeds 200 ppm. A synthetic alexandrite contains 480 ppm, exceeding the concentrations measured in the natural alexandrites examined, whereas one natural chrysoberyl contains only 2 ppm. The paper also assesses analytical limitations that complicate interpretation. Several electron-beam and X-ray methods lack sufficient sensitivity for reliable determination of low gallium concentrations, and surface measurements may fail to represent variations associated with internal zoning or structure. Neutron activation analysis is regarded as the most suitable available technique, with a detection limit of approximately 0.5 ppm and reported accuracy of 3–10% of the measured concentration. Its routine use is nevertheless restricted by cost, lengthy analytical procedures and the slow decay of induced radioactivity. The authors conclude that gallium content alone cannot reliably establish natural or synthetic origin in the gemstone groups investigated. Proposed concentration thresholds require caution, and any identification suggested by gallium analysis must be corroborated by additional tests.

Gemmological studies in ancient India

Journal Article
Murthy, S.R.N. (1986) Gemmological studies in ancient India. Quarterly Journal of the Mythic Society, Vol. 77, No. 4, Oct.–Dec., pp. 393–397.
Record No. 1317  |  Sinkankas/Born No.: NIS/NIB  |  RWHL
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Some gemmological observations made on heat-treated yellow sapphires

Journal Article
Gunawardene, M. (1986) Some gemmological observations made on heat-treated yellow sapphires. Journal of the Gemmologists Association of Sri Lanka, No. 3, pp. 25–29.
Record No. 874  |  Sinkankas/Born No.: NIS/NIB  |  RWHL
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Gunawardene reports observations on yellow sapphires produced by heat treatment, particularly material from Sri Lanka. The paper examines changes in colour resulting from heating and the gemmological features that may assist in recognizing treated stones. Of particular interest is the behaviour of the induced yellow to orange-yellow colour under subsequent heating and illumination, together with microscopic evidence of thermal alteration. The study contributes to the developing understanding during the 1980s of how heating could produce or modify yellow coloration in corundum and of the practical difficulties involved in distinguishing such stones from naturally coloured yellow sapphire.

Gem Trade Lab Notes: Sapphire, pinkish-orange (“Padparadscha”)

Journal Article
Fryer, C.W. (1986) Gem Trade Lab Notes: Sapphire, pinkish-orange (“Padparadscha”). Gems & Gemology, Vol. 22, No. 1, Spring, pp. 52–53.
Record No. 796  |  ISBN/ISSN: 0016626X  |  Sinkankas/Born No.: NIS/NIB  |  RWHL
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Attracting a great deal of attention during the February 1983 Tucson Gem & Mineral Show was the 1,126 ct pinkish orange sapphire crystal from Sri Lanka shown in figure 23. The firm displaying the crystal expected it to yield a cut stone weighing at least 200 ct. This unusual crystal was illustrated and discussed in the article “Padparadscha: What’s in a Name?” by Robert Crowningshield (Gems & Gemology, Spring 1983). Discussed in this article was the term padparadscha and the fact that the precise hue represented by this term is often a subject of controversy and discussion. Most of the gem dealers who saw this spectacular crystal agreed that the color was aptly referred to as padparadscha. Because of the subjectivity of the term, however, GIA Gem Trade Laboratory, Inc., does not use it on GTL identification reports, treating it in the same manner as the trade grades “Burma ruby,” “Kashmir sapphire,” and “Siberian amethyst.” Although this crystal was remarkable and many felt that it should be kept intact as a mineral specimen, everyone was curious as to what color of faceted gems it would yield, since it seemed inevitable that the crystal was going to be cut.

Gemstones in China—Especially jade and similar stones

Journal Article
Chikayama, A. (1986) Gemstones in China—Especially jade and similar stones. Australian Gemmologist, Vol. 16, No. 2, May, pp. 60–63.
Record No. 507  |  Sinkankas/Born No.: NIS/NIB  |  RWHL
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A. Chikayama surveys China’s gemstone resources, concentrating on nephrite and the diverse ornamental materials traditionally used for carving and sold under regional jade names. The article presents a nationwide locality map and a comparative table linking Chinese stone names with mineralogical identities, colours, transparency, lustre, hardness, specific gravity, refractive index and principal sources. Hotan Yu from Xinjiang is identified as nephrite, while Xin Yu from Liaoning and Nan Yu from Guangdong are serpentine; Dongbei Yu from Liaoning contains serpentine and tremolite. Dushan Yu, also called Nanyang Yu, is described as a mixed rock consisting chiefly of plagioclase and zoisite, with mica and sphene. Several other materials bearing jade names are quartzites: Mi Yu from Henan is green, Guizhou Yu is blue, and Jing Bai Yu from the Beijing area is white, with dyed colours also recorded. The survey further includes tiger’s-eye from Henan, rhodonite from Beijing, turquoise from Hubei, Shaanxi and Henan, malachite from Hubei, and fluorite from several provinces. Rose quartz and amazonite are recorded from Xinjiang, with amazonite also occurring in Yunnan. Ju Hua Shi is listed as a celestine-and-calcite material with a radial structure. Pyrophyllite carving stones receive particular attention through locality-based names, including Changhua Shi, Qingtian Shi, Shoushan Shi, Mira Han Yu and Bairin Shi; Changhua material also contains cinnabar responsible for blood-red mottling. Rock crystal, agate, jasper and additional serpentine occurrences are noted more generally. Beyond carving materials, the author reports Chinese deposits of diamond, ruby, sapphire, aquamarine, beryl, peridot, pyrope garnet, zircon and topaz, highlighting blue sapphire and red zircon from Hainan Island and noting that further deposits had not yet been publicly disclosed. Institutional developments accompanying increased economic interest in gemstones include the establishment of the Gem Mineral Corporation in Beijing in June 1984 to promote resource exploitation, processing, identification, valuation and sales, and a gemmological laboratory within the Ministry of Geology and Mineral Resources in 1982. The article provides a compact reference to the geographical distribution and physical properties of Chinese carving stones while demonstrating the mineralogical diversity concealed by traditional jade nomenclature.

The Jade Kingdom

Book
Desautels, P.E. (1986) The Jade Kingdom. New York, Van Nostrand Reinhold, 118 pp.
Record No. 140  |  Sinkankas/Born No.: 1667; NIB  |  RWHL
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Jade towers above all other hardstone carving materials—rose quartz, aventurine, agate, rock crystal, bloodstone, lapis lazuli, turquoise, and the rest—in both long-term popularity and sustained value, yet despite its intensive exploitation by widely diverse cultures, little authoritative work exists in the English language. When books on jade do appear, they are usually no more than cursory surveys of some of the more exotic carvings that have flowed, generation after generation, from the lapidary shops of China. But jade’s history, lore, mineralogy, gemology, and art cannot be confined to the ideas of “green” and “China”: the material has been known for thousands of years, is widely distributed across the Earth’s surface, and has been extensively used by several ancient and modern civilizations. Nonetheless, the Chinese have had the most enduring and sophisticated association with jade, especially the green varieties, which have consistently been the most highly prized. Over time, Chinese jade carving developed into a highly refined art form, incorporating a vast repertoire of designs and symbols, many of whose meanings are either lost to history or distorted through transmission. Given this richness and complexity—ancient and modern, primitive and sophisticated, sacred and secular, symbolic and utilitarian—it is no surprise that the study of jade has largely been undertaken by artists, art historians, anthropologists, and archaeologists. The systematic study of jade is still relatively recent, and its development has been hindered by various obstacles. Art historians and archaeologists have struggled to identify and date jade objects that were removed from their original contexts by unscientific collecting methods; when written records exist, they are often vague or inaccurate. It is remarkable that researchers have managed to sketch out a tentative chronology of styles and periods spanning thousands of years, despite the uncertainties surrounding many questions—such as when diamond-cutting tools were introduced into China or where the high-quality jade used in ancient Mesoamerica was originally mined. Nonetheless, efforts to synthesize evidence from different scientific fields are beginning to bear fruit. Misguided theories, like ancient commerce between China and the Americas or the Asiatic origins of European jade, have now been discredited with the discovery of jade deposits in Europe itself. Slowly but steadily, records of jade use across various civilizations are being clarified as raw data yield to sustained scientific scrutiny. One central challenge has always been defining what jade actually is. “Jade” is a gemological rather than a mineralogical term, and for much of history, it was identified on the basis of qualities such as toughness, workability, edge-holding ability, and beauty—rather than chemical composition. Only in the 1860s did Alexis Damour succeed in distinguishing the two principal varieties, nephrite and jadeite, through chemical analysis. Since then, accumulated analytical results, new deposit discoveries, and artifact sampling have refined but also complicated these definitions. New findings, such as the chromium-bearing jadeite known as ureyite, and the growing understanding of jade as a heterogeneous rock rather than a pure mineral, have further muddied the waters. As a result, public confusion remains high, and authoritative facts are difficult to find, scattered as they are across obscure and highly technical sources. This book attempts to remedy that fragmentation by compiling a coherent body of information on the nature of jade, its geological distribution, its historical use by major cultures, the ways in which those cultures worked and valued it, and the technologies they developed to master it.

Popol Vuh: The Definitive Edition of the Mayan Book of the Dawn of Life and the Glories of Gods and Kings

Book
Tedlock, D. (1985) Popol Vuh: The Definitive Edition of the Mayan Book of the Dawn of Life and the Glories of Gods and Kings. New York, Simon & Schuster, 388 pp.
Record No. 28683  |  ISBN/ISSN: 9780680000000  |  Sinkankas/Born No.: NIS/NIB  |  RWHL
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The Popol Vuh tells the story of the emergence of light in the darkness, from primordial glimmers to brilliant dawns, and from rainstorms as black as night to days so clear that the very ends of the earth can be seen. A revised edition of this translation of the Popol Vuh has become necessary because the world of Maya studies is itself a constantly brightening one. Advances in the understanding of Maya languages, literature, art, history, politics, and astronomy have required changes in the introduction, notes, commentaries, glossary, and illustrations. There are also changes in the translation itself, some of them subtle refinements and others that readers of the previous edition may find surprising. Finally, an index has been added. Newly available sources on Maya languages have made it possible to give meaning to proper names that were left untranslated before. For example, Xbaquiyalo, the wife of Seven Macaw, now becomes Egret Woman. The temptresses Xtah and Xpuch are now Lust Woman and Wailing Woman, and they stand revealed as the predecessors of a dangerous phantom known all the way from Guatemala to northern New Mexico by her Spanish name, La Llorona. And Tecum, Keeper of the Mat in the ninth generation of Quiché lords, becomes Black Butterfly. In other cases, new sources have made it possible to correct errors of translation that were caused by imprecise spellings or slips of the pen in the Popol Vuh manuscript, which often leave words and phrases open to multiple interpretations. What was once “the emergence of all the sky-earth” now becomes “the lighting of all the sky-earth,” a reference to the astronomical aspect of the story. The name of the first human woman, given as Celebrated Seahouse in the previous edition, now changes to Red Sea Turtle. The term for the rubber used by the Hero Twins to heal a falcon’s eye is no longer “sorrel gum” but rather “blood of sacrifice.” And the image of the god Hacauitz is no longer located “above a great red river” but rather “at the top of a great pyramid.”

Maya: Treasures of an Ancient Civilization

Book
Claney, F.S., Coggins, C.C., Culbert, T.P., Gallencamp, C., Harrison, P.D. and Sabloff, J.A. (1985) Maya: Treasures of an Ancient Civilization. New York, Harry N. Abrams, 240 pp.
Record No. 28575  |  Sinkankas/Born No.: NIS/NIB  |  RWHL
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This exhibition was organized by The Albuquerque Museum in association with the Instituto Nacional de Antropología e Historia in Mexico, the Instituto de Antropología e Historia de Guatemala, and the Department of Archaeology in Belize. The history of Pre-Columbian America is largely unknown. For many years historians considered only those aspects of history which related to the Old World as worthy of study, ignoring or scorning all that was not already recognized as important by European scholars. The “scientific” interest in Pre-Columbian cultures was stimulated by two amateurs—John Lloyd Stephens and Frederick Catherwood—when they travelled to Central America in 1839 in search of answers to intriguing questions posed by the written accounts of their predecessors. Since then, archaeologists have brought to light important information concerning these cultures. With regard to Guatemala, archaeological evidence and findings document the great cultural and scientific advances made by the past inhabitants of that land. Even so, this information has not yet yielded a complete and orderly record of the events, personalities, and circumstances which make up its history. As is the case today, ancient Guatemala was inhabited by diverse peoples, each with distinct customs, beliefs, traditions, and commercial, social, and political relationships that eventually underwent drastic changes, probably caused by the struggle for power, which culminated in crisis and institutional breakdown. The MAYA exhibition organized by The Albuquerque Museum presents a fascinating panorama of Maya culture, which developed primarily in the Petén lowlands and the southern highlands, where evidence has been found that speaks eloquently of the artistic and scientific activities which flourished there—products of deeply rooted religious beliefs and of a complex politico-religious structure.

Editorial Forum: Foil-backing still a popular treatment

Journal Article
Tatiwala, N.K. (1985) Editorial Forum: Foil-backing still a popular treatment. Gems & Gemology, Vol. 21, No. 2, Summer, p. 115.
Record No. 26776  |  Sinkankas/Born No.: NIS/NIB  |  RWHL
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The Gem Trade Lab Notes section (Winter 1984, p. 228) reported on emerald imitations made from colorless rock crystal quartz backed with green foil—a technique still commonly used today, even in enameled jewelry. Similarly, colorless beryl or corundum is often backed with red or green foil to mimic emerald or ruby, while silver foil may be applied behind colorless synthetic or natural sapphire to enhance its brilliance.

Altering the color of topaz

Journal Article
Nassau, K. (1985) Altering the color of topaz. Gems & Gemology, Vol. 21, No. 1, Spring, pp. 26–34.
Record No. 26775  |  Sinkankas/Born No.: NIS/NIB  |  RWHL
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The various techniques in use today to alter colorless topaz to produce brown, pink and, most commonly, blue stones are discussed. Special attention is given to the three irradiation sources—gamma rays, high-energy electrons, and neutrons—used to convert the colorless stones to hues in the yellow to brown range and the subsequent heat treatment required in most cases to turn the irradiated stones blue. The blue color produced by irradiation and subsequent heat treatment is stable to light. Currently, no routine gemological tests are available that can definitively determine whether the color of the topaz is natural or the result of treatment.

Gem Trade Lab Notes: Oiled lapis lazuli

Journal Article
Crowningshield, G.R. (1985) Gem Trade Lab Notes: Oiled lapis lazuli. Gems & Gemology, Vol. 21, No. 4, Winter, p. 235.
Record No. 26752  |  Sinkankas/Born No.: NIS/NIB  |  RWHL
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An importer of fine lapis lazuli beads from Afghanistan noticed a variation in luster among the beads and suspected that some had been oiled to enhance their appearance. After confirming the beads as genuine lapis lazuli, the New York laboratory used a thermal reaction tester and magnification to investigate the presence of oil or paraffin. All beads exhibited the typical reaction of oil being drawn to the surface by the heated probe, with some showing heavy oil concentrations in drill holes and surface cracks. The lack of whitening upon cooling indicated the presence of oil rather than paraffin. Microscopic examination and acetone testing revealed no evidence of blue dye. While oil or paraffin treatments have historically been used to “set” dyes in stones like jade, lapis lazuli, and amazonite, the beads in question were not dyed, and the reason for oiling alone remains unclear—possibly done to mask a poor polish.

A proposed new classification for gem-quality garnets

Journal Article
Stockton, C.M. and Manson, D.V. (1985) A proposed new classification for gem-quality garnets. Gems & Gemology, Vol. 21, No. 4, Winter, pp. 205–218.
Record No. 26745  |  Sinkankas/Born No.: NIS/NIB  |  RWHL
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Existing methods of classifying garnets have proved to be inadequate to deal with some new types of garnets discovered recently. A new classification system based on the chemical analysis of more than 500 gem garnets is proposed for use in gemology. Chemical, optical, and physical data for a representative collection of 202 transparent gem-quality stones are summarized. Eight garnet species are defined—grossular, andradite, pyrope, pyrope-almandine, almandine-spessartine, spessartine, and pyrope-spessartine—and methods of identification are described. Properties that can be determined with standard gem-testing equipment (specifically, refractive index, color, and absorption spectrum) can be used to identify a garnet as one of the eight species and, where appropriate, more precisely as one of several varieties that are also defined.

Materials and Manufacture in Ancient Mesopotamia: The Evidence of Archaeology and Art | Metals and Metalwork, Glazed Materials and Glass

Book
Moorey, P.R.S. (1985) Materials and Manufacture in Ancient Mesopotamia: The Evidence of Archaeology and Art | Metals and Metalwork, Glazed Materials and Glass. Oxford, B.A.R., 302 pp.
Record No. 26474  |  ISBN/ISSN: 9780860000000  |  DOI: https://doi.org/10.30861/9780860543060  |  Sinkankas/Born No.: NIS/NIB  |  RWHL
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The following studies serve as the archaeological foundation for a history of craft and technology in ancient Mesopotamia, though they are not intended as an attempt to write that history. The goal has been to provide what Leo Oppenheim called a “systematic and critical inventory of the technological achievements of Mesopotamian civilization” in areas such as metalwork, glazed materials, and glass, as a preliminary step toward broader surveys. Integrating this material with the relevant documentary evidence to understand the wider socio-economic environment in which these technologies developed and thrived—a necessary framework for any true history of technology—is a task of a wholly different scale. With few exceptions, the data on material culture and documentary sources from Mesopotamia remain only partially published, scattered, and often accessible only to specialists. Even in Classical Studies, where the documentation is far richer and more thoroughly examined, the history of technology has until recently held a relatively low academic status, likely due to a persistent tendency to treat the subject in isolation, divorced from its social context and economic processes.

Some aspects of identification of Kashan synthetic rubies

Journal Article
Henn, U. and Schrader, H.-W. (1985) Some aspects of identification of Kashan synthetic rubies. Journal of Gemmology, Vol. 19, No. 6, pp. 469–478.
Record No. 17045  |  ISBN/ISSN: 221252  |  Sinkankas/Born No.: NIS/NIB  |  RWHL
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Synthetic rubies by Kashan are characterized by inclusions of melt residues. Cryolite was used as flux. The inclusions can be divided into four types. Even in samples looking apparently free of inclusions, these inclusions can be found by microprobe analysis (15 samples). The increased amounts of sodium found with the help of neutron activation analysis (NAA) in two analysed samples are caused by these inclusions of cryolite.

A Second Paradise: Indian Courtly Life 1590–1947

Book
Patnaik, N., Welch, S.C. and Bannu (1985) A Second Paradise: Indian Courtly Life 1590–1947. Garden City, NY, Doubleday & Co., 192 pp.
Record No. 4934  |  Sinkankas/Born No.: NIS/NIB  |  RWHL
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Naveen Patnaik’s A Second Paradise: Indian Courtly Life 1590–1947, with an introduction by Stuart Cary Welch and illustrations by Bannu (Ved Pal Sharma), presents an illustrated account of the splendor, customs, artistic patronage, and ceremonial traditions of India’s princely courts from the Mughal period to independence in 1947. Published in association with the Metropolitan Museum of Art and the 1985 Festival of India, the book combines historical narrative, Mughal and Rajput miniature paintings, early photographs, and contemporary illustrations to reconstruct the material and cultural world of Indian rulers. Jacqueline Kennedy Onassis served as editor, while Welch contributes an introduction examining Indian painting and the development of Mughal, Rajput, and British-period artistic traditions. Patnaik’s narrative describes the education of princes, court ceremonies, royal processions, marriages, festivals, hunting, music, dance, architecture, clothing, and the elaborate etiquette governing the lives of maharajas, nawabs, begums, and courtesans. Gemstones and jewelry figure prominently as symbols of sovereignty, wealth, divine favor, and personal adornment. Indian rulers wore elaborate necklaces, jeweled armbands, anklets, rings, and turban ornaments, including the sarpej, while royal horses and elephants were adorned with gold and precious stones. Particular attention is given to the navaratna tradition, in which nine gemstones represented the celestial bodies and were believed to confer auspicious planetary influences. Rubies were associated with the sun and sapphires with Saturn, illustrating the intersection of gemology, astrology, and royal ceremonial practice. The book discusses India’s historical gemstone sources, including the diamond mines of Golconda, Kashmir sapphires, Burmese rubies, and pearls from the Persian Gulf, while also mentioning emeralds associated with Tonk. The Koh-i-Noor diamond receives attention through the account of its seizure by Nadir Shah and its subsequent acquisition by the British following the annexation of Punjab. Maharaja Duleep Singh’s dispossession and exile provide a particularly revealing example of how exceptional gemstones became symbols of political conquest and imperial authority. The Mughal court of Shah Jahan is portrayed as a center of extraordinary luxury, with the jewel-encrusted Peacock Throne, ceremonial daggers with carved jade and gemstone handles, and architectural decoration incorporating colored stones. The bazaars of Shahjahanabad contained workshops of goldsmiths and jewelers, alongside merchants selling carved jade, ivory, textiles, and other luxury goods. The author also describes the use of Chinese jade vessels as supposed detectors of poison, reflecting historical beliefs concerning the protective properties of precious materials. Traditional miniature painting techniques receive detailed treatment in Welch’s account of Bannu’s workshop, including the preparation of mineral pigments, the use of agate burnishers, and the application of powdered gold to create jewel-like surfaces. The illustrated sections reproduce court portraits and scenes of elaborate dress, documenting changes in jewelry fashions from Mughal and Rajput traditions to the European-influenced styles of the British period. During the late nineteenth and early twentieth centuries, Indian princes increasingly patronized European jewelers, notably Cartier, replacing some traditional enamel settings with Western designs and incorporating gemstones acquired through international trade. The volume concludes with the decline of princely authority under British rule and the dissolution of the princely states following independence. For gemologists and jewelry historians, the book provides valuable visual and historical evidence of gemstone use, royal ornamentation, traditional jewel-setting practices, the symbolic significance of precious stones, and the transformation of Indian courtly jewelry over more than three centuries.

The eyepiece pointer: A useful microscope accessory

Journal Article
Fryer, C.W. and Koivula, J.I. (1985) The eyepiece pointer: A useful microscope accessory. Gems & Gemology, Vol. 21, No. 2, Summer, pp. 105–107.
Record No. 4780  |  ISBN/ISSN: 0016626X  |  Sinkankas/Born No.: NIS/NIB  |  RWHL
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The eyepiece pointer is a highly useful microscope accessory for the gemologist, as it remains in focus and consistently indicates the center of the microscope’s field of view regardless of magnification or the focal plane within the gemstone. It greatly simplifies the task of identifying and showing microscopic features in both mounted and unmounted gems, and it can be easily adapted for use with nearly any microscope.

Polysynthetic twin lamellae in synthetic Verneuil sapphire

Journal Article
Duroc-Danner, J.M. (1985) Polysynthetic twin lamellae in synthetic Verneuil sapphire. Journal of Gemmology, Vol. 19, No. 6, April, pp. 479–483.
Record No. 3005  |  ISBN/ISSN: 221252  |  Sinkankas/Born No.: NIS/NIB  |  RWHL
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A 2.35 ct faceted sapphire is described in which conspicuous polysynthetic twin lamellae closely resembled those commonly associated with natural corundum, although further examination established a Verneuil synthetic origin. The stone’s unusually intense colour initially raised suspicion of treatment, but colour alone was considered unreliable for distinguishing natural from synthetic sapphire. Examination with a 10× lens revealed a few straight, parallel twinning lines in an otherwise particularly clean stone. The girdle lacked the pockmarked appearance sometimes associated with heating, while immersion in methylene iodide suggested that colour was concentrated near the surface. The iron absorption line near 450 nm was absent, and the stone remained inert under both long-wave and short-wave ultraviolet radiation. Immersion microscopy between crossed polarisers readily revealed the straight twin lamellae, including interference rings along the twin planes. Because such twinning can occur exceptionally in Verneuil corundum, its presence was not accepted as conclusive evidence of natural origin. Examination along the optic axis under crossed polarisers produced the characteristic Plato striation pattern, described as a lozenge-shaped arrangement formed by intersecting sets of lamellae. Curved colour bands, further supporting the Verneuil identification, were difficult to observe and became visible only during immersion with illumination diffused through tissue paper. The author distinguishes the conspicuous polysynthetic lamellae from the structures responsible for the Plato pattern because they followed different directions. The former appeared to lie in planes slightly inclined to the optic axis, but their precise crystallographic orientation could not be established from the faceted specimen. Although all Verneuil synthetics previously examined by the author had yielded a positive Plato test, this was the only sapphire encountered with such convincing natural-like polysynthetic twinning. The report therefore stresses the importance of seeking curved colour banding or Plato striations before identifying a sapphire from twinning alone. Possible surface diffusion treatment is also discussed because of the apparent surface concentration of colour and the absence of the usual chalky bluish green short-wave fluorescence. This interpretation remained tentative, since the stone could not be tested by repolishing. The case demonstrates how an unusual combination of internal structures and possible treatment effects can complicate sapphire identification.

Geology of World Gem Deposits

Edited Book
VanLandingham, S.L., editor (1985) Geology of World Gem Deposits.. New York, Van Nostrand Reinhold, 406 pp..
Record No. 2605  |  Sinkankas/Born No.: NIS/NIB  |  RWHL
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An edited compilation examining the geological origin, occurrence, exploration, and evaluation of gemstone deposits worldwide. The first two sections reproduce 21 contributions covering topics such as diamond formation in kimberlite, jadeite genesis through low-grade metamorphism, agate and thunder egg development, Brazilian topaz deposits, Sri Lankan sedimentary gem deposits, and the structure responsible for precious opal’s colour. Exploration studies consider magnetic characteristics associated with Australian opal deposits, sodium as a geochemical indicator of Colombian emerald mineralization, glacial tracing of Canadian kimberlite, and the economic evaluation of alluvial diamond deposits. Regional accounts describe nephrite, amethyst, agate, and other gem materials in North America. These papers are followed by VanLandingham’s extensive review of the literature and a substantial bibliography, supported by author, mineral and rock name, and subject indexes. The review encompasses gemological research, mineral composition and structure, inclusions, physical properties, and deposit geology. Particular attention is given to the conditions that produce gem-quality material and the difficulties of assessing deposits whose valuable crystals may occur irregularly within a larger mineralized body. Combining technical research with more accessible geological accounts, the volume serves as a reference for geologists, gemologists, prospectors, and collectors investigating gemstone formation and distribution.

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