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.

301–320 of 1,247 matching references

An oil well in your garden

Journal Article
Hänni, H.A. (1988) An oil well in your garden. Swiss Watch and Jewellery Journal, Mar-88, pp. 461–464.
Record No. 1979  |  Sinkankas/Born No.: NIS/NIB  |  RWHL*
This paper does not wish to deal with the luck of a Texan property owner, but rather to share my experience in the gemmological laboratory. The article could just as well be titled: What many people do not yet know about oiling emeralds, and others at times tend to forget. ”Cemmosophic” literature likes to use the French term jardin” (Engl.: garden) for typical, vei|—like inclusions visible to the naked eye. These internal structures, resembling leaves and tendrils, are commonly classified as healed fissures, but often also as open cracks. The latter are usually considered to be negative properties."

A new type of twinning in natural sapphire

Journal Article
Schmetzer, K. (1988) A new type of twinning in natural sapphire. Journal of Gemmology, Vol. 21, No.̨ 4, October, pp. 218–220.
Record No. 1555  |  ISBN/ISSN: 221252  |  Sinkankas/Born No.: NIS/NIB  |  RWHL*

The precipitation of alpha TiO2 from supersaturated solutions of Ti in alumina: Crystal structure and morphology

Journal Article
Jayaram, V. (1988) The precipitation of alpha TiO2 from supersaturated solutions of Ti in alumina: Crystal structure and morphology. Philosophical Magazine, Series A, Vol. 3, No. 57, pp. 525–542.
Record No. 1051  |  Sinkankas/Born No.: NIS/NIB  |  RWHL*

Goethite inclusion alteration during the heat conversion of amethyst to citrine

Journal Article
Koivula, J.I. (1987) Goethite inclusion alteration during the heat conversion of amethyst to citrine. Australian Gemmologist, Vol. 16, No. 7, pp. 271–272.
Record No. 26917  |  Sinkankas/Born No.: NIS/NIB  |  RWHL*
Important article that details how goethite inclusions, are altered to hematite by heat treatment of amethyst to citrine. This note describes the conversion of goethite to hematite when amethyst containing goethite inclusions is heated to produce brownish yellow coloured “fired” citrine quartz. The resulting hematite pseudomorphs after goethite are always accompanied by at least some fracturing in the amethyst-citrine because of water loss during dehydration of the inclusions.

New investigations of synthetic amethysts produced in Japan

Journal Article
Lind, T. and Schmetzer, K. (1987) New investigations of synthetic amethysts produced in Japan. Journal of Gemmology, Vol. 20, No. 5, pp. 274–277.
Record No. 26738  |  ISBN/ISSN: 221252  |  Sinkankas/Born No.: NIS/NIB  |  RWHL*
Synthetic amethysts of Japanese production, which are now available in the gem trade, are characterized with respect to their diagnostic properties such as inclusions, growth structures, twinning, and infrared spectra. The gemstones frequently have feathers consisting of liquid-filled and two-phase inclusions, sharp growth zoning parallel to one rhombohedral face, as well as twin structures. This twinning, however, can be distinguished from polysynthetic lamellar twinning in natural amethysts.

The emeralds of the Belmont Mine, Minas Gerais, Brazil

Journal Article
Hänni, H.A., Schwarz, D. and Fischer, M. (1987) The emeralds of the Belmont Mine, Minas Gerais, Brazil. Journal of Gemmology, Vol. 20, No. 7/8, pp. 446–456.
Record No. 6051  |  ISBN/ISSN: 221252  |  Sinkankas/Born No.: NIS/NIB  |  RWHL*
A geological and gemmological study of emeralds from the Belmont Mine near Itabira, Minas Gerais, Brazil, combining an account of mining and regional geology with optical measurements, electron microprobe analyses, and inclusion studies. The emeralds occur chiefly in mica and chlorite schists associated with pegmatites and show relatively low iron, magnesium, and sodium contents compared with similar schist-hosted material. Characteristic inclusions include biotite–phlogopite mica, multiphase fluid cavities, fine growth tubes capable of producing chatoyancy, and disc-like stress fissures useful in distinguishing Itabira stones from other Brazilian emeralds. Fluid-inclusion measurements indicate minimum formation conditions of approximately 380°C and 1,400 bars. The authors favour formation during a later metamorphic or retrograde episode rather than directly during pegmatite intrusion, and infer a complex history involving multiple events.

Synthetische Lechleitner-rubine mit natürlichen kernen und synthetischen überzügen

Synthetic Lechleitner rubies with natural cores and synthetic coatings
Journal Article
Schmetzer, K. and Bank, H. (1987) Synthetische Lechleitner-rubine mit natürlichen kernen und synthetischen überzügen. [Synthetic Lechleitner rubies with natural cores and synthetic coatings] Zeitschrift der Deutschen Gemmologischen Gesellschaft, Vol. 36, No. 1/2, pp. 1–10.
Record No. 4973  |  Sinkankas/Born No.: NIS/NIB  |  Language: In German  |  RWHL*
Describes Lechleitner rubies consisting of natural pale ruby or colourless corundum cores from Sri Lanka covered by a thin, flux-grown synthetic ruby layer. The cores include rough, bruted and faceted material and retain natural mineral and fluid inclusions, while the synthetic overgrowth contains flux residues. Six faceted specimens show violet-tinged colours resembling Sri Lankan rubies and pink sapphires. Identification requires careful microscopic examination, particularly of the boundary between core and overgrowth, which can resemble early Knischka synthetic rubies. Trace-element analysis, including examination of flux residues, together with X-ray fluorescence, electron microprobe analysis and spectroscopy, can assist identification.

Blue and yellow sapphire from Kaduna Province, Nigeria

Journal Article
Kiefert, L. and Schmetzer, K. (1987) Blue and yellow sapphire from Kaduna Province, Nigeria. Journal of Gemmology, Vol. 20, No. 7/8, pp. 427–442.
Record No. 4849  |  ISBN/ISSN: 221252  |  Sinkankas/Born No.: NIS/NIB  |  RWHL*

Esmeraldas – Inclusões em gemas

Emeralds — Inclusions in gems
Book
Schwarz, D. (1987) Esmeraldas – Inclusões em gemas. [Emeralds — Inclusions in gems] Ouro Preto, MG, Imprensa Universitária UFOP, 450 + XI pp.
Record No. 4201  |  Sinkankas/Born No.: NIS/NIB  |  Language: in Portuguese  |  RWHL*
A comprehensive study of inclusions in emerald, with particular emphasis on their use in gemological identification and determination of geographic origin. Schwarz examines solid mineral inclusions, fluid inclusions, growth features and other internal characteristics of emeralds from the principal producing localities, comparing their characteristic inclusion assemblages. Brazilian occurrences receive extensive treatment, including Carnaíba and Socotó in Bahia, Santa Terezinha in Goiás, and deposits in Minas Gerais, alongside material from Colombia and other world sources. The work illustrates how combinations of mineral inclusions, fluid inclusions and growth structures can distinguish emeralds from different geological environments and can assist in separating natural from synthetic material. It became an important reference for subsequent studies of emerald inclusions and geographic origin. Sadly this softcover book was poorly printed on low quality paper.

Inclusions in flux-grown crystals of corundum

Journal Article
Watanabe, K. (1987) Inclusions in flux-grown crystals of corundum. Crystal Research and Technology, Vol. 22, No. 3,, 3/1/87 pp. 345–355.
Record No. 3984  |  ISBN/ISSN: 2321300  |  DOI: https://dx.doi.org/10.1002/crat.2170220310  |  Sinkankas/Born No.: NIS/NIB  |  RWHL*
Single crystals of corundum were grown by seeded techniques, such as stationary, seed-rotation, and top-seeded, from molten Na- or Li-cryolite (Na₃AlF₆ or Li₃AlF₆) flux. Inclusions—such as flux inclusions, negative crystals, and cavities—present in the crystals were examined under an optical microscope, and the formation mechanisms and shapes of these inclusions, depending on differences in growth technique and conditions, are briefly described.

On twinning in natural and synthetic flux-grown ruby

Journal Article
Schmetzer, K. (1987) On twinning in natural and synthetic flux-grown ruby. Journal of Gemmology, Vol. 20, No. 5, January, pp. 294–305.
Record No. 1550  |  ISBN/ISSN: 221252  |  Sinkankas/Born No.: NIS/NIB  |  RWHL*

Internal diffusion

Journal Article
Koivula, J.I. (1987) Internal diffusion. Journal of Gemmology, Vol. 20, No. 7/8, pp. 474–477.
Record No. 1121  |  ISBN/ISSN: 221252  |  Sinkankas/Born No.: NIS/NIB  |  RWHL*
Some minerals, such as rutile, hematite and ilmenite, found as inclusions in sapphires are capable of imparting body—colour to their host during high temperature heat treatment. The inclusions are cannibalized by the host sapphire for the chromophoric elements they contain. If the inclusions are not completely consumed by their host this ‘internal diffusion’ results in a zone of intensely coloured sapphire surrounding the remaining inclusions.

On corundums from Umba Valley, Tanzania

Journal Article
Hänni, H.A. (1987) On corundums from Umba Valley, Tanzania. Journal of Gemmology, Vol. 20, No. 5, January, pp. 278–284.
Record No. 950  |  ISBN/ISSN: 221252  |  Sinkankas/Born No.: NIS/NIB  |  RWHL*
The many colours exhibited by corundums from Umba Valley in Tanzania are related to their varying contents of Fe, Ti, Cr and V. Ni and Co could not be detected by the EDS-XRF technique used. The presence of abundant inclusions distinguishes these gemstones, and the following were found: zircon, rutile(?), apatite, hematite, mica, monazite, plagioclase, calcite, pyrrhotine and graphite. Healed fractures, negative crystals, colour zoning, twinning with traces of intersecting lamellae and boehmite(?) laths were noted. Techniques for the identification of inclusions are discussed. The densities (3.98–4.01 g/cm³) and refractive indices (nₑ 1.761–1.768, nₒ 1.769–1.778) were also determined. Spectral features are given.

Inklusen im Bernstein

Inclusions in amber
Journal Article
Gübelin, E.J. and Koivula, J.I. (1986) Inklusen im Bernstein. [Inclusions in amber] Zeitschrift der Deutschen Gemmologischen Gesellschaft, Vol. 35, No. 3/4, pp. 73–86.
Record No. 5060  |  Sinkankas/Born No.: NIS/NIB  |  Language: In German  |  RWHL*
Gübelin and Koivula examine the diverse inclusions found in amber, extending attention beyond the familiar plant and animal remains to the less frequently discussed inorganic and fluid features. The article illustrates insects and other organic inclusions together with gas bubbles, liquid-bearing cavities and other structures preserved in fossil resin. Particular attention is given to the processes by which inclusions became trapped and subsequently preserved and to microscopic features that provide information about the history of the resin. Examples include cavities interpreted as gas or air bubbles and two-phase inclusions possibly representing droplets of water with contraction bubbles. The text corresponds closely to the amber section of the authors’ 1986 Photoatlas of Inclusions in Gemstones, although some of the photographs differ.

Einschlüsse im Quarz

inclusions in Quartz
Journal Article
Gübelin, E.J. and Koivula, J.I. (1986) Einschlüsse im Quarz. [inclusions in Quartz] Lapis, Vol. 11, No. 9, Sept., pp. 19–26.
Record No. 5059  |  Sinkankas/Born No.: NIS  |  Language: in German  |  RWHL*
Gübelin and Koivula present a photographic survey of inclusions in quartz, illustrating the remarkable variety of solid, liquid and gaseous features that may occur within the mineral. The examples demonstrate mineral crystals, fluid inclusions, growth phenomena and other internal structures, emphasizing both their visual diversity and their value for interpreting the formation of their quartz hosts. The article consists principally of selected photomicrographs from the authors’ Photoatlas of Inclusions in Gemstones, accompanied by explanatory captions. A contemporary Journal of Gemmology abstract specifically describes it as a series of color photographs taken from the Photoatlas and records 42 color figures.

European Gemmologists on Gemstones of the World

Conference Proceedings
CISGEM (1986) European Gemmologists on Gemstones of the World. Gemmologia Europa, Milan: CISGEM, 174 pp..
Record No. 4247  |  Sinkankas/Born No.: NIS/NIB  |  Language: in English & Italian  |  RWHL*
The first volume in CISGEM’s Gemmologia Europa series, bringing together contributions by leading European gemologists on important gem materials and gemological problems. The papers include discussions of diamond, emerald, opal and other colored stones, combining descriptions of deposits and geographic sources with gemological properties, inclusions, identification and aspects of formation. Among the contributors are E. Alan Jobbins, Henri-Jean Schubnel, Jan Kanis, Eduard J. Gübelin and Pieter C. Zwaan. Gübelin’s contribution, for example, compares Australian and Mexican opals. The volume provides a snapshot of European gemological research and expertise in the mid-1980s, with parallel English and Italian text. This includes Pailin sapphire, Sri Lankan gems, gems from Brazil, Mozambique, Zambia, Zimbabwe, South Africa, Namibia, and opal from Mexico and Australia.

Carbon dioxide fluid inclusions as proof of natural-colored corundum

Journal Article
Koivula, J.I. (1986) Carbon dioxide fluid inclusions as proof of natural-colored corundum. Gems & Gemology, Vol. 22, No. 3, Fall, pp. 152–155.
Record No. 3756  |  ISBN/ISSN: 0016626X  |  Sinkankas/Born No.: NIS/NIB  |  RWHL*
The question of how to identify natural-colored from heat-treated corundum has long puzzled the gemological community. One important clue is now provided b y carbon dioxide fluid inclusions. Because such inclusions cannot survive heat treatment, their existence intact and unruptured in rubies and sapphires i s conclusive proof that n o heat treatment has occurred.

An improved sample holder and its use in the distinction of natural and synthetic ruby as well as natural and synthetic amethyst

Journal Article
Schmetzer, K. (1986) An improved sample holder and its use in the distinction of natural and synthetic ruby as well as natural and synthetic amethyst. Journal of Gemmology, Vol. 20, No. 1, January, pp. 20–33.
Record No. 1548  |  ISBN/ISSN: 221252  |  Sinkankas/Born No.: NIS/NIB  |  RWHL*

Natürliche und synthetische Rubine—Eigenschaften und Bestimmung

Natural and Synthetic Rubies—Properties and Identification
Book
Schmetzer, K. (1986) Natürliche und synthetische Rubine—Eigenschaften und Bestimmung. [Natural and Synthetic Rubies—Properties and Identification] Stuttgart, Germany, E. Schweizerbart’sche Verlagsbuchhandlung (Nägele u. Obermiller), vi + 131 pp., with 31 color photographs, 144 black–and–white photographs and 21 figures
Record No. 1547  |  ISBN/ISSN: 3510651251  |  Sinkankas/Born No.: 5822; NIB  |  Language: in German  |  RWHL*
Schmetzer presents a comprehensive study of the identification and separation of natural and synthetic rubies, based on examination of approximately 900 natural and 350 synthetic stones. After reviewing the mineralogy and crystallography of corundum, he describes five principal methods of synthetic ruby growth and the analytical techniques employed, including microscopy, UV-visible and infrared spectroscopy, ultraviolet fluorescence, goniometry and chemical analysis. The principal emphasis is on microscopic inclusions and internal growth structures: rutile, boehmite, twinning and characteristic growth features are discussed as evidence of natural origin, while diagnostic inclusions and structures in synthetic material are related to particular growth processes and manufacturers. Natural rubies from 15 localities are described and compared, followed by similarly organized accounts of 11 types of synthetic ruby. The work is extensively illustrated and intended as a practical reference for determining whether a ruby is natural or synthetic and, in many cases, establishing its geographic source or method of synthesis.

Saphire aus Nigeria und von Sta. Terezinha de Goias, Brazilien

Sapphires from Nigeria and from Sta. Terezinha de Goiás, Brazil
Journal Article
Henn, U. (1986) Saphire aus Nigeria und von Sta. Terezinha de Goias, Brazilien. [Sapphires from Nigeria and from Sta. Terezinha de Goiás, Brazil] Zeitschrift der Deutschen Gemmologischen Gesellschaft, Vol. 35, No. 1/2, pp. 15–19.
Record No. 962  |  Sinkankas/Born No.: NIS/NIB  |  Language: In German  |  RWHL*
Henn describes blue sapphires from two then relatively little-known localities, Nigeria and Santa Terezinha de Goiás, Brazil, comparing their appearance, physical properties and characteristic inclusions. The Nigerian material, reportedly from about 50 km north of Jos, is typically dark to inky blue with pronounced color zoning. Microscopic features include fluid and elongated two-phase inclusions, idiomorphic apatite crystals and rounded zircon crystals. The Brazilian sapphires are generally of poor transparency and bluish gray color, sometimes showing strong dark-blue zoning; characteristic inclusions include muscovite and margarite oriented along cleavage directions. The study provides preliminary diagnostic information for distinguishing sapphires from these two sources.

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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