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.

1,101–1,120 of 1,163 matching references

Mineral inclusions in gemstones recently observed, analyzed and identified

Conference Paper
Gübelin, E.J. (1993) Mineral inclusions in gemstones recently observed, analyzed and identified. XXIV International Gemmological Conference, Paris S. 85.
Record No. 3114  |  Sinkankas/Born No.: NIS/NIB  |  not seen

Origin of sapphire in eastern Australian basalts: Inferred from inclusion studies

Journal Article
Guo, J., O’Reilly, S.Y. and Griffin, W.L. (1992) Origin of sapphire in eastern Australian basalts: Inferred from inclusion studies. Geological Society of Australia Abstracts, No. 32, pp. 219–220.
Record No. 7647  |  Sinkankas/Born No.: NIS/NIB  |  not seen

Identificación de gemas sintéticas fabricadas por fusión a la llama (método Verneuil)

Identification of synthetic gemstones made by flame fusion (Verneuil method).
Journal Article
Kammerling, R.C., Koivula, J.I. and Weldon, R. (1991) Identificación de gemas sintéticas fabricadas por fusión a la llama (método Verneuil). [Identification of synthetic gemstones made by flame fusion (Verneuil method).] Boletin del Instituto Gemologico Español, Vol. 33, diciembre, pp. 32–37.
Record No. 7650  |  Sinkankas/Born No.: NIS/NIB  |  Language: in Spanish  |  seen
Describes the Verneuil flame-fusion process and the diagnostic features used to identify gemstones produced by it. Particular attention is given to microscopic inclusions and absorption spectra, with illustrations showing characteristic features of flame-fusion synthetics. The article explains how evidence resulting from the growth process can distinguish these laboratory-grown materials from their natural counterparts and provides practical criteria for routine gemological identification. A contemporary Journal of Gemmology abstract specifically confirms this emphasis on the Verneuil process, inclusions and absorption spectra.

Observation of inclusions in a Madagascar emerald and their possible implications

Journal Article
Kleyenstüber, A. (1991) Observation of inclusions in a Madagascar emerald and their possible implications. South African Gemmologist, Vol. 5, No. 2, pp. 4–9.
Record No. 4196  |  Sinkankas/Born No.: NIS/NIB  |  not seen

A report on one of a number of emeralds from Madagascar

Journal Article
Campbell, I.C.C. (1991) A report on one of a number of emeralds from Madagascar. South African Gemmologist, Vol. 5, No. 1, pp. 8–15.
Record No. 4195  |  Sinkankas/Born No.: NIS/NIB  |  not seen

Inclusion of the Month: Native element inclusions

Journal Article
Koivula, J.I. (1991) Inclusion of the Month: Native element inclusions. Lapidary Journal, Vol. 44, No. 11, February, p. 48.
Record No. 1123  |  Sinkankas/Born No.: NIS/NIB  |  seen

Lamellar iron-free högbomite-24R from Tanzania

Journal Article
Schmetzer, K. and Berger, A. (1990) Lamellar iron-free högbomite-24R from Tanzania. Neues Jahrbuch für Mineralogie Monatshefte, No. 9, pp. 401–412.
Record No. 7795  |  Sinkankas/Born No.: NIS/NIB  |  not seen

Gemstones of Pakistan: Geology and Gemmology

Book
Kazmi, A.H. and O’Donoghue, M. (1990) Gemstones of Pakistan: Geology and Gemmology. Peshawar, Gemstone Corp. of Pakistan, 146 pp.
Record No. 4841  |  Sinkankas/Born No.: NIS/NIB  |  not seen
An illustrated survey of Pakistan’s gemstones that relates their properties and occurrence to the country’s geological and tectonic setting. An introductory section explains gemstone composition, physical properties, identification instruments, cutting and polishing, and the acquisition of rough. Subsequent chapters organize the deposits by geological association, covering emeralds associated with the Indus suture, ruby and spinel in the crystalline marbles of the Hunza region, pegmatite minerals, and gemstones from hydrothermal veins. Detailed accounts include aquamarine, tourmaline, feldspar, quartz, and topaz, with particular attention to the pink topaz of Katlang. Pakistani emeralds are also compared with synthetic material. Maps, geological sections, tables, and color photographs connect descriptions of individual gems with their host rocks and regional environments. Photographs by E.J.Gübelin illustrate inclusions, while A.H.Kazmi contributes specimen and landscape images. Brief concluding sections address miscellaneous gem materials and Pakistan’s gem market. Intended partly to encourage further discoveries, the book provides an accessible geological foundation for prospectors, gemologists, jewelers, and collectors, supported by an extensive bibliography.

Alexandrit aus einem heuentdeckten Vorkommen in Brasilien

Alexandrite from a newly discovered deposit in Brazil
Journal Article
Gübelin, E.J. (1988) Alexandrit aus einem heuentdeckten Vorkommen in Brasilien. [Alexandrite from a newly discovered deposit in Brazil] Schweizerische Uhrmacher- und Goldschmiede-Zeitung (SUZ), No. 2, pp. 16–22.
Record No. 2190  |  Sinkankas/Born No.: NIS/NIB  |  Language: in German  |  not seen
Gübelin reports on the newly discovered Hematita alexandrite deposit in Minas Gerais, Brazil, discovered in 1987 and notable for producing unusually fine and relatively clean material. He describes the appearance and gemological characteristics of the alexandrite, including its pronounced color change from greenish hues in daylight to reddish or purplish red under incandescent illumination. Particular attention is given to internal features useful for identifying the Brazilian material. Among the characteristic mineral inclusions subsequently identified in Hematita alexandrite are fluorite and apatite, together with mica and fluid inclusions. The discovery was significant because Hematita rapidly became an important source of fine alexandrite at a time when supplies from the traditional Russian and Sri Lankan sources were limited.

Emeralds from Goiás State – Brazil

Conference Paper
Barros, J.C. and Kinnaird, J.A. (1987) Emeralds from Goiás State – Brazil. XXI International Gemmological Conference, Abstracts, Rio de Janeiro
Record No. 7803  |  Sinkankas/Born No.: NIS/NIB  |  RHL

Die Abkühlungsgeschwindigkeit als Ursache für die Bildung entweder von Sternkorunden oder von kornblumenblauen Saphiren

The cooling rate as the cause for the formation of either star corundums or cornflower blue sapphires
Journal Article
Harder, H. and Schneider, A. (1987) Die Abkühlungsgeschwindigkeit als Ursache für die Bildung entweder von Sternkorunden oder von kornblumenblauen Saphiren. [The cooling rate as the cause for the formation of either star corundums or cornflower blue sapphires] Neues Jahrbuch fuer Mineralogie Monatshefte, No. 8, pp. 344—346.
Record No. 7775  |  Sinkankas/Born No.: NIS/NIB  |  Language: in German  |  not seen
Harder and Schneider investigate experimentally how cooling rate controls whether Ti-bearing corundum develops asterism or a cornflower-blue color. They relate the two effects to the behavior of titanium during cooling: under conditions permitting exsolution, titanium is precipitated as oriented rutile needles, producing the silk responsible for asterism; under different cooling conditions, titanium remains incorporated in the corundum lattice, where interaction between iron and titanium produces blue coloration. Thus, corundum of essentially comparable composition can develop either the oriented rutile inclusions required for a star effect or the transparent blue appearance characteristic of sapphire, depending upon its thermal history. The paper emphasizes cooling rate as a decisive factor governing the distribution of titanium between the corundum lattice and exsolved rutile.

Tiploidite in quartz

Journal Article
Koivula, J.I., Fryer, C.W. and Gübelin, E.J. (1987) Tiploidite in quartz. Indian Gemmologist, Vol. 1, No. 2, pp. 5–7.
Record No. 7772  |  Sinkankas/Born No.: NIS/NIB  |  not seen
The genesis of mineral inclusions in gemstones

The genesis of mineral inclusions in gemstones

Journal Article
Gübelin, E.J. (1987) The genesis of mineral inclusions in gemstones. Gem: Bulletinen Stockholms Gemmologiska Förening, No. 2,
Record No. 2184  |  Sinkankas/Born No.: NIS/NIB  |  Language: in Swedish  |  not seen
Discusses the formation of mineral inclusions in gemstones and their relationship to the growth history of the host crystal. Reproduces a chapter from the author’s Photoatlas of Inclusions in Gemstones.

Une nouvelle variété noble de la famille des feldspaths

A new noble variety of the feldspar family
Journal Article
Gübelin, E.J. (1987) Une nouvelle variété noble de la famille des feldspaths. [A new noble variety of the feldspar family] Monde et Mineraux, No. 79, p. 20.
Record No. 2183  |  Sinkankas/Born No.: NIS/NIB  |  Language: in French  |  not seen
Describes light blue to light green gem-quality feldspar from pegmatite dykes near Kioo, Kenya, approximately 13 km east of Sultan Hamud. The material resembles aquamarine in colour and has a vitreous lustre. Optical measurements, X-ray diffraction and electron microprobe analyses identify a sodium-rich plagioclase with a peristerite structure. Reported inclusions comprise distinctive growth irregularities, fingerprint-like patterns containing occasional two-phase inclusions, and vermiculite crystals. The article also outlines the geological setting, associated minerals and mining methods.

Lamellare Einschaltungen von Diaspor in Korund

Journal Article
Schmetzer, K. (1987) Lamellare Einschaltungen von Diaspor in Korund. Der Aufschluss, Vol. 38, No. 3, pp. 335–337.
Record No. 1554  |  Sinkankas/Born No.: NIS/NIB  |  Language: in German  |  not seen
Describes thin diaspore lamellae in blue-grey, barrel-shaped corundum crystals up to 5 cm long from Mato Grosso, Brazil. Under slight mechanical pressure, the crystals split readily along gently curved surfaces lacking a consistent crystallographic orientation. A thin mineral layer exposed on these surfaces has a lower refractive index than corundum and was identified as diaspore. The unusual splitting is attributed to these lamellae, interpreted as products of retrograde metamorphism.

Die Feldspäte als Wirt- und Gastmineralien

The feldspars as host and guest minerals
Journal Article
Gübelin, E.J. and Koivula, J.I. (1986) Die Feldspäte als Wirt- und Gastmineralien. [The feldspars as host and guest minerals] Schweizerische Uhrmacher- und Goldschmiede-Zeitung (SUZ), No. 11, pp. 26–29, 30–31.
Record No. 7714  |  Sinkankas/Born No.: NIS/NIB  |  Language: in German  |  not seen
Gübelin and Koivula examine feldspars both as gemstones containing inclusions and as mineral inclusions occurring within other gemstones. Using photomicrographs, they illustrate characteristic internal features of gem feldspars—including members of the orthoclase and plagioclase groups—and examples in which feldspar itself occurs as an included mineral. The article emphasizes the value of identifying such inclusions for understanding the geological environment and formation history of their host gemstones, while demonstrating the considerable variety of microscopic features associated with the feldspar group.

Les inclusions dans la péridot

Inclusions in peridot
Journal Article
Gübelin, E.J. (1986) Les inclusions dans la péridot. [Inclusions in peridot] Monde et Mineraux, No. 76, November–December, pp. 28–29.
Record No. 2179  |  Sinkankas/Born No.: NIS/NIB  |  Language: in French  |  not seen
Gübelin gives a brief illustrated account of inclusions characteristic of peridot. He describes the internal features encountered in gem-quality olivine, emphasizing mineral inclusions and their diagnostic appearance under the microscope. Typical features of peridot include chromite and other spinel-group crystals, commonly surrounded by stress fractures or disc-like halos, as well as negative crystals and partially healed fractures. Such inclusions are useful both for identifying natural peridot and for interpreting aspects of its geological formation.

Les opales Mexicaines

Mexican opals
Journal Article
Gübelin, E.J. (1986) Les opales Mexicaines. [Mexican opals] Revue de Gemmologie A.F.G., No. 88, September, pp. 3–6, with 11 color figures.
Record No. 2178  |  Sinkankas/Born No.: NIS/NIB  |  Language: in French  |  not seen
Gübelin provides a historical and technical survey of Mexican opal, discussing the principal varieties and their major localities. He notes the use of opal in pre-Columbian Mexico and describes the important deposits in the volcanic regions of Querétaro and Jalisco, where opal occurs in cavities and fractures in rhyolitic rocks. Particular attention is given to Mexican fire opal, with its characteristic yellow, orange and red body colors, as well as transparent precious opal displaying play-of-color. The article discusses the appearance, occurrence and characteristic inclusions of Mexican material; later studies cite Gübelin for two- and three-phase inclusions and mineral inclusions including hornblende, goethite, hematite, fluorite, quartz, cristobalite and chalcedony in Querétaro opal.

Die diagnostischen eigenschaften der neuen synthesen

The diagnostic properties of the new syntheses
Journal Article
Gübelin, E.J. (1986) Die diagnostischen eigenschaften der neuen synthesen. [The diagnostic properties of the new syntheses] Deutsche Goldschmiede-Zeitung, Vol. 84, No. 11, pp. 69–76.
Record No. 2175  |  Sinkankas/Born No.: NIS/NIB  |  Language: in German  |  not seen
Gübelin reviews the diagnostic properties of several recently introduced synthetic gemstones and the problems they pose for separation from their natural counterparts. Emphasis is placed on the combination of conventional gemological properties with microscopic examination of inclusions and growth structures, supplemented where necessary by spectroscopic and other analytical methods. The article discusses characteristic features of newer synthetic materials, particularly synthetic corundum and emerald, and shows that physical constants alone may be insufficient for identification as manufacturing techniques increasingly reproduce the appearance and properties of natural stones. Gübelin stresses the diagnostic importance of flux residues, metallic inclusions, growth zoning and other internal features associated with particular synthesis processes. The paper summarizes practical criteria by which these newer products can be recognized in gemological testing.

Rasterelektronen-mikroskopie. Einige anwendungen in der edelsteinforschung

Scanning electron microscopy. Some applications in gemstone research
Journal Article
Hofmann, C., Schrader, H.W. and Stender, E. (1985) Rasterelektronen-mikroskopie. Einige anwendungen in der edelsteinforschung. [Scanning electron microscopy. Some applications in gemstone research] Goldschmiede Zeitung, Vol. 83, No. 6, pp. 76–77.
Record No. 2382  |  Sinkankas/Born No.: NIS/NIB  |  Language: In German  |  not seen
Hofmann, Schrader and Stender describe applications of scanning electron microscopy (SEM) to gemological research, emphasizing its usefulness for examining surface structures and extremely small features beyond the practical resolution of conventional gemological microscopy. Examples illustrate how the technique can reveal the morphology of inclusions, growth and dissolution features, fracture surfaces, and other microscopic structures relevant to gemstone investigation. When combined with electron-beam microanalysis, SEM also permits localized chemical characterization of minute inclusions or surface features. The brief article demonstrates the value of SEM as a complementary research technique where conventional optical microscopy alone provides insufficient morphological or compositional information.

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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