Gemstone Inclusions Bibliography

Gemstone Inclusions Bibliography

Explore books, articles and historical sources on inclusions in gemstones in Four Treasures, the Lotus Gemology reference database. This bibliography brings together matching records from the collection, with publication details, abstracts and cover images where available.

Gemstone Inclusion References

The list below matches the terms inclusion or inclusions in the database's searchable fields. Some references discuss inclusions as part of a broader subject.

981–1,000 of 1,165 matching references

On the cause of asterism in star corundum

Journal Article
Nassau, K. (1968) On the cause of asterism in star corundum. American Mineralogist, Vol. 53, January–February, pp. 300–305.
Record No. 1330  |  Sinkankas/Born No.: NIS/NIB  |  RWHL
It has been generally accepted that asterism in corundum (star rubies and sapphires) is caused by needles of rutile (TiO₂) aligned along crystallographic planes of the corundum (e.g. Webster, 1962). The evidence given by Tait (1955) was: (1) the presence of titanium, (2) the needle-like habit, and (3) the square cross-section of the needles. Based on the analogy with rutilated quartz, and by eliminating octahedrite and brookite by the morphology, rutile was accordingly identified. This type of evidence, however, is explained equally well by either TiO₂ or the compound aluminum titanate Al₂TiO₆.

An Olmec serpentine figure at Dumbarton Oaks

Journal Article
Coe, M.D. (1967) An Olmec serpentine figure at Dumbarton Oaks. American Antiquity, Vol. 32, No. 1, pp. 11–113.
Record No. 28556  |  DOI: https://doi.org/10.2307/278788  |  Sinkankas/Born No.: NIS/NIB  |  RWHL
An Olmec figurine said to have been found at La Venta falls stylistically within the range of variation of other figurines known to be from that site. Four designs engraved on the upper parts of the limbs represent abstract were-jaguar heads identical with those of the serpentine mosaic pavements at La Venta. Thus, the pavements should be considered examples of the Olmec style and not, as has been claimed, pre-Olmec. In 1965 an important Olmec figurine (Figs. 1 and 2) was acquired by the Robert Woods Bliss Collection of Pre-Columbian Art at Dumbarton Oaks, Washington, D.C. The provenience is not definitely known, but it is said to have been found at La Venta in the state of Tabasco, Mexico. The material from which the piece was carved is a white to greyish-buff serpentine with small, shiny black inclusions. While presently 8.1 cm in height, the figurine had been broken in ancient times, so that one foot is missing, as well as the lower part of the other leg. There has been no restoration, although a recent break across the left shoulder and the chin has been repaired. The material, workmanship, and patination all testify to its authenticity.

Studies on Jadeites and Albitites from Guatemala

Thesis
da Silva, Z.C.G. (1967) Studies on Jadeites and Albitites from Guatemala., Houston: Rice University
Record No. 28499  |  Sinkankas/Born No.: NIS/NIB  |  RWHL
In the central part of the San Augustin Acasaguastlan Quadrangle north of the Metagua River Valley, Guatemala, jadeite-rich rocks occur as inclusions in serpentine. The associated minerals are albite and in minor amounts, muscovite, actinolite and zoisite. The country rock is generally highly sheared serpentine, although massive serpentine is also present in lesser amounts. Most of the jadalte in the area is white or slightly greenish, having only small amounts of diopside, acmite and hedenbergite molecules. The green variety has a higher content of these pyroxene molecules and the variation in optical properties of the different specimens of jadeite analyzed is related to the impurities present. Jadeite seems to have formed before serpentinization of the ultrabasic body and later reacted with silica-bearing aqueous solutions forming secondary albite. Albitites are quite abundant in the area, occurring as large included bodies in the serpentine. From field relationship, chemical and mineral composition, they seem to have originated from a pegmatite which underwent desilication.

Eclogites and jadeite from the Motagua Fault Zone, Guatemala

Journal Article
McBirney, A., Aoki, K.-i. and Bass, M.N. (1967) Eclogites and jadeite from the Motagua Fault Zone, Guatemala. American Mineralogist, Vol. 52, No. 5–6, May–June, pp. 908–918.
Record No. 7824  |  ISBN/ISSN: 0003004X  |  Sinkankas/Born No.: NIS/NIB  |  RWHL
Jadeite occurs as inclusions in serpentinite in the Motagua fault zone. A boulder of remarkable size and purity was found near Manzanal, Guatemala, and chemical, optical, and X-ray studies have been made of a separated sample of the jadeite. Elsewhere in the Motagua fault zone, omphacite-garnet eclogites and glaucophane-lawsonite-omphacite-garnet rocks have been found in similar environments. Only at the Manzanal locality, however, have sodic pyroxenes been found in rocks which are nearly monomineralic.

Solid inclusions in corundum and almandine garnet from Ceylon, identified by x-ray powder photographs

Journal Article
Zwaan, P.C. (1967) Solid inclusions in corundum and almandine garnet from Ceylon, identified by x-ray powder photographs. Journal of Gemmology, Vol. 10, No. 7, July, pp. 224–234.
Record No. 1924  |  ISBN/ISSN: 221252  |  Sinkankas/Born No.: NIS/NIB  |  RWHL

Determination of solid inclusions in gemstones

Journal Article
Schubnel, H.-J. (1967) Determination of solid inclusions in gemstones. Journal of Gemmology, Vol. 10, No. 6, April, pp. 189–193.
Record No. 1563  |  ISBN/ISSN: 221252  |  Sinkankas/Born No.: NIS/NIB  |  RWHL

The diagnostic significance of inclusions in precious stones

Journal Article
Eppler, W.F. (1964) The diagnostic significance of inclusions in precious stones. Lapidary Journal, Vol. 18, No. 6, September, pp. 676–679.
Record No. 719  |  Sinkankas/Born No.: NIS/NIB  |  RWHL

Sapphire from Rio Coxim, Mato Grosso, Brazil

Journal Article
Eppler, W.F. (1964) Sapphire from Rio Coxim, Mato Grosso, Brazil. Journal of Gemmology, Vol. 9, No. 6, April, pp. 199–204.
Record No. 718  |  ISBN/ISSN: 221252  |  Sinkankas/Born No.: NIS/NIB  |  RWHL
About four years ago, Professor J. E. de Souza Campos of the University of São Paulo, Brazil, reported on a new sapphire from Brazil. He mentioned strange inclusions, unknown until now in sapphire and resembling rounded gas bubbles so typical of synthetic corundum. At the author’s request, Professor de Souza Campos very kindly made available two cut stones of this sapphire and later some raw material, which could be tested more easily. The locality of these sapphires is quoted by de Souza Campos as Jauré and Quilombo, Rio Coxim, Mato Grosso. He found the refraction for sodium light to be nₒ = 1.770, nₑ = 1.762, and the birefringence 0.008. The dichroism for blue-coloured stones is o = blue to violet blue, e = green; for greenish-coloured stones o = green, e = yellow-green. With the hydrostatic balance he determined the specific gravity at 3.952 to 4.052. The stones exhibit a dark blue colour but, regrettably, the transparency is considerably reduced by many inclusions. At a first sight through the microscope, many of them indeed resembled rounded gas bubbles. But when using a higher magnification, it is seen that two kinds of inclusions are present: liquid and gas-filled discs, and negative crystals, many of them exhibiting rounded forms.

Mineralogische Untersuchungen an Granaten aus in Schweden gefundenen Schmuckgegenständen der Merowinger- und Karolingerzeit

Mineralogical investigations of garnets from jewelry items found in Sweden dating to the Merovingian and Carolingian periods
Journal Article
Mellis, O. (1963) Mineralogische Untersuchungen an Granaten aus in Schweden gefundenen Schmuckgegenständen der Merowinger- und Karolingerzeit. [Mineralogical investigations of garnets from jewelry items found in Sweden dating to the Merovingian and Carolingian periods] Arkiv för Mineralogi och Geologi, Vol. 3, No. 4, pp. 297–362.
Record No. 26791  |  Sinkankas/Born No.: NIS/NIB  |  Language: in German  |  RWHL
Mellis presents a nondestructive mineralogical investigation of 41 red stones from Merovingian- and Carolingian-period jewelry found in Sweden, undertaken both to establish whether the stones were actually garnets and, if possible, to determine their geographical origin. Because of the cultural and historical importance of the objects, the examination was restricted chiefly to refractive index, color and absorption spectra, specific gravity, anomalous birefringence, inclusions, and, for some specimens, single-crystal X-ray study. The small polished garnet plates are described individually, with detailed observations of their optical properties and inclusions, including various types of needles, prismatic and plate-like crystals, opaque minerals, zircon, and other phases. Chemical compositions were estimated from physical and optical properties and compared with established garnet compositional groups; the examined stones include pyrope-rich and almandine-rich varieties and mixtures of the principal garnet components. Mellis explores whether inclusions and composition can identify the geological environment and source of the stones, comparing the archaeological specimens particularly with garnets from Bohemia and other known occurrences. He concludes that inclusions alone cannot, at the existing state of knowledge, provide a reliable determination of geographical provenance, although inclusions combined with chemical composition can exclude certain geological environments and help characterize possible source rocks. The study demonstrates the value of detailed mineralogical examination of archaeological garnets while emphasizing the limitations of assigning ancient worked stones to specific deposits solely from their observable mineralogical properties.

Fine zoning in Australian sapphire

Journal Article
Rutland, E.H. (1963) Fine zoning in Australian sapphire. Journal of Gemmology, Vol. 9, No. 3, July, p. 83.
Record No. 1506  |  ISBN/ISSN: 221252  |  Sinkankas/Born No.: NIS/NIB  |  RWHL

Ancient Egyptian Materials and Industries

Book
Lucas, A. and Harris, J.R. (1962) Ancient Egyptian Materials and Industries. Mineola, NY, Dover, 570 pp.
Record No. 26873  |  ISBN/ISSN: 486404463  |  Sinkankas/Born No.: 4059  |  RWHL
The majesty and splendor of ancient Egypt were largely due to the remarkably advanced technological skills developed by its artisans and craftsmen. This comprehensive and detailed study of ancient Egyptian technology meticulously documents how these workers, along with other Egyptians, exploited the land’s abundant resources. First published in 1926 and later revised and enlarged, this monumental work became a standard reference, unmatched in any other field of archaeology. The present volume reprints the fourth edition, thoroughly revised in light of more recent research and archaeological discoveries. Topics covered include a wide range of materials and techniques central to Egyptian life: the use of animal products, building materials, cosmetics, perfumes, incense, fibers, glazed ware, glass and its production, metals and alloys, painting materials, pottery, woodworking, precious and semi-precious stones, distillation of alcoholic beverages, and substances used in mummification. Profoundly erudite and rich in detail, Ancient Egyptian Materials and Industries is an indispensable reference for students of Egyptology and classical civilizations, and a vital resource for anyone interested in the long and remarkable history of technological innovation. Sinkankas: Drastically revised, rearranged: the substances now include beverages, animal products, building materials, cosmetics, perfumes & incense, ceramics & glass, fibers, metals & alloys, mummification materials, oils, fats, waxes, painting materials, pottery & its manufacture, gemstones, other stones, woods & woodworking, and a historical analysis. Ch 12, [335–54], on gemstones, among which now additionally appear coral, amber, malachite, and jade, while horn, ivory, nacre and tortoiseshell are described in Ch 2. Ornamental stones are treated in Ch 13, [355–75]. The author notes that “diamond, opal, ruby and sapphire were not known to the ancient Egyptians.” In his preface, Harris notes the inclusion of information taken from recent studies, with references added to the list in the previous edition. Much technological information is also added, with an appendix of reliable chemical analyses. “The most consistent modification has, however, been in matters of lexicography, in order to eliminate invalid evidence derived from inaccurate or disputed translations of Egyptian texts.” In this connection, see also Harris’ Lexicographical Studies in Ancient Egyptian Materials, 1961. In this edition, the following places are of gemological interest: beads, Ch 4, [41–7] (includes gemstone materials); inlaid gemstone eyes, Ch 7, [98–127] (many types & examples); gemstones in general, Ch 16, [386–405]; other stones, Ch 17, [406–28]. Lucas should always be consulted whenever one writes or lectures about Egyptian jewelry.

Ekanite, a new metamict mineral from Ceylon

Journal Article
Anderson, B.W., Claringbull, G.F., Davis, R.J. and Hill, D.K. (1961) Ekanite, a new metamict mineral from Ceylon. Nature, Vol. 190, No. 4780, p. 997.
Record No. 29918  |  DOI: 10.1038/190997a0  |  Sinkankas/Born No.: NIS/NIB  |  RWHL
Anderson, Claringbull, Davis and Hill describe ekanite, a newly recognized metamict mineral from the gem pits of Eheliyagoda in the Ratnapura district of Ceylon. Known since 1953 as green transparent-to-translucent pebbles, some fashioned as cabochons showing a gemstone-quality smoky asterism, the material was recognized as unusual by F.L.D. Ekanayake, after whom the mineral was named. Chemical analysis indicates a thorium-rich calcium silicate containing uranium, lead and minor rare-earth elements, with the approximate formula (Th,U)(Ca,Fe,Pb)₂Si₈O₂₀. The mineral is metamict, with refractive index about 1.5969 and density 3.276. Heating between 650 and 1,000 °C causes recrystallization to an X-ray powder pattern resembling thorite or zircon; at higher temperatures it melts and, if subsequently recrystallized, produces an X-ray pattern analogous to huttonite. Microscopic examination shows occasional larger opaque inclusions but no identifiable inclusions responsible for the asterism.

Corundum from Tanganyika

Journal Article
Webster, R. (1961) Corundum from Tanganyika. Gems & Gemology, Vol. 10, No. 7, Fall, pp. 202–205.
Record No. 1828  |  ISBN/ISSN: 0016626X  |  Sinkankas/Born No.: NIS/NIB  |  RWHL

The Powder Method in X-ray Crystallography

Book
Azaroff, L.V. and Bueger, M.J. (1958) The Powder Method in X-ray Crystallography. New York, MacGraw-Hill, 342 pp.
Record No. 26929  |  Sinkankas/Born No.: NIS/NIB  |  RWHL
Instruction in the various laboratory methods for investigating crystals has long been part of the mineralogy and geology curriculum at the Massachusetts Institute of Technology, encompassing both optical and x-ray techniques. While suitable texts exist for optical methods, there has been no adequate textbook on the x-ray powder method. To support lectures and prepare students for laboratory work, the authors initially wrote a set of notes on the theory and practice of this method, which eventually evolved into this book. The expanded format allowed for more detailed discussion and the inclusion of advanced material beyond what could be covered in a short course. The powder method is inherently simple yet widely valuable across science and industry, often used by individuals with no formal training in crystallography. This book is written with such users in mind, maintaining a fundamental approach while assuming only limited prior knowledge. It omits detailed coverage of general crystallography, x-ray generation, and equipment beyond powder cameras, as these are addressed in other sources. Detection methods using photographic film are emphasized, given their simplicity and permanence, despite the growing use of ionization-type detectors. The principles outlined apply regardless of detection technique, but film is expected to remain relevant in routine applications for the foreseeable future.

Notes on asterism in corundum, rose quartz and almandine garnet and chatoyancy in beryl

Journal Article
Eppler, W.F. (1958) Notes on asterism in corundum, rose quartz and almandine garnet and chatoyancy in beryl. Journal of Gemmology, Vol. 6, No. 5, January, pp. 195–212.
Record No. 715  |  ISBN/ISSN: 221252  |  Sinkankas/Born No.: NIS/NIB  |  RWHL

Application of phase contrast microscopy in gemmology

Journal Article
Gübelin, E.J. (1957) Application of phase contrast microscopy in gemmology. Journal of Gemmology, Vol. 6, No. 4, October, pp. 151–165.
Record No. 2051  |  ISBN/ISSN: 221252  |  Sinkankas/Born No.: NIS/NIB  |  RWHL

The phase-contrast method

Journal Article
Gübelin, E.J. (1957) The phase-contrast method. Gems & Gemology, Vol. 9, No. 3, Fall, pp. 67–79.
Record No. 2050  |  ISBN/ISSN: 0016626X  |  Sinkankas/Born No.: NIS/NIB  |  RWHL

Structure & inclusions of synthetic star-stones

Journal Article
Breebaart, A.J. (1957) Structure & inclusions of synthetic star-stones. Journal of Gemmology, Vol. 6, No. 2, April, pp. 72–74.
Record No. 489  |  ISBN/ISSN: 221252  |  Sinkankas/Born No.: NIS/NIB  |  RWHL

Echt oder synthetisch?

Genuine or Synthetic?
Book
Chudoba, K. and Gübelin, E. (1956) Echt oder synthetisch? [Genuine or Synthetic?] Stuttgart, Rühle-Diebener-Verlag, 156 pp.
Record No. 4735  |  Sinkankas/Born No.: 1349; NIB  |  Language: in German  |  RWHL
Chudoba and Gübelin provide a practical guide to distinguishing natural gemstones from synthetic counterparts, combining a short history of artificial gem production with detailed discussion of the principal manufacturing methods and their diagnostic consequences. The Verneuil flame-fusion process, flux growth, and hydrothermal synthesis are described, together with the characteristic structures and inclusions they produce. Particular attention is given to synthetic ruby and sapphire, spinel, emerald, and other important gem materials, with comparisons between natural and laboratory-grown stones based on growth zoning, curved striae, gas bubbles, mineral inclusions, refractive properties, fluorescence, and other microscopic and physical features. The authors emphasize examination with the gemological microscope as one of the most powerful means of separation, supported by numerous photomicrographs illustrating inclusions and growth phenomena in both natural and synthetic gems. Conceived as a concise working manual for gemologists and jewelers, the book brought together the principal identification criteria then available at a time when synthetic gemstones were becoming increasingly sophisticated and commercially important.

Inclusions in synthetic spinels

Journal Article
Gübelin, E.J. (1956) Inclusions in synthetic spinels. The Gemmologist, Vol. 25, No. 302, September, pp. 153–157; No. 303, October, pp. 173–176,
Record No. 2047  |  Sinkankas/Born No.: NIS/NIB  |  RWHL

Exploring the Literature of Gemstone Inclusions

The literature of gemstone inclusions covers identification, origin determination, treatments, synthesis, mineral inclusions, fluid inclusions and other internal features of natural and synthetic gems.

For a curated selection of important sources, read Inclusions in Gemstones — Hyperion Literature Sources.

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