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.
81–100 of 1,111 matching references
Gemological Characterization of Montana Sapphire from the Secondary Deposits at Rock Creek, Missouri River, and Dry Cottonwood Creek
Palke, A.C., Renfro, N., Hapeman, J.R. and Berg, R.B. (2023)
Journal Article · Source: Gems & Gemology · Volume: Vol. 59 · Issue: No. 1, Spring · Pages: pp. 2–45
Abstract
Montana has produced large volumes of sapphire from secondary deposits for more than 150 years. While early production was mostly for industrial use as watch and instrument bearings, modern heat treatment technology has enabled the deposits to be worked profitably as gemstone mines, bringing more of this material to the gem and jewelry trade than ever before. Although pale blue and pale green sapphires make up the bulk of the production, fine Montana sapphire comes in nearly every hue, including yellow, orange, purple, and pink, along with very rare finds of ruby. Secondary Montana sapphire shares some similarities with those from Umba and Songea in Tanzania, but it is generally straightforward to separate them on the basis of inclusion scenes and trace element chemistry fingerprints.
Keywords
gems, corundum, inclusions.5, USA.12, Montana.12, Rock Creek, Missouri River, Dry Cottonwood Creek
The Imperial Crown of the Holy Roman Empire, Part I: Photoluminescence and raman spectroscopic study of the gemstones
Nasdala, L., Lamers, T., Gilg, H.A., Chanmuang, C., Griesser, M., Kirchwegner, F., Erlacher, A. and Böhmler, M. (2023)
Journal Article · Source: Journal of Gemmology · Volume: Vol. 38 · Issue: No. 5 · Pages: pp. 448–473
Abstract
The Imperial Crown of the Holy Roman Empire is not only a unique and outstanding symbol of European history, it is also one of the most significant works of Western goldsmiths’ art from the High Middle Ages. However, little is known about the gem materials it contains. As part of an interdisciplinary research project led by the Kunsthistorisches Museum Vienna in Austria, the 172 gemstones in the crown were all conclusively identified for the first time using (non-destructive) photoluminescence and Raman spectroscopy. They include 71 blue sapphires, 50 garnets (22 almandines, 22 pyrope-almandines, five pyropes and one grossular), 20 emeralds, 13 amethysts, four chalcedonies and three spinels. In addition, 11 glass imitations of various colours were identified. Raman spectral details and inclusions in the garnets support their assignment to garnet types previously found to be used in antique and early medieval jewellery. The large red spinel in the centre of the crown’s front plate is presumably part of the original crown and, thus, is one of the earliest-known spinels in a historic object, yet it yielded spectroscopic evidence of having been heated.
Keywords
gems, corundum, history.1, sapphire, spinel, garnet, beryl, emerald, amethyst, chalcedony
Cobalt-bearing blue spinel from Lukande, near Mahenge, Tanzania
Krzemnicki, M.S., Leuenberger, A. and Balmer, W.A. (2023)
Journal Article · Source: Journal of Gemmology · Volume: Vol. 38 · Issue: No. 5 · Pages: pp. 474–493
Abstract
In September 2021, a new deposit of Co-bearing blue spinel was discovered in the Lukande area, south of Mahenge in central Tanzania. We analysed 44 faceted spinels from this source, ranging from Co-dominated blue to Fe-dominated (greyish) blue. Interestingly, nearly all of these spinels showed characteristic inclusion features, consisting predominantly of oriented rhombic lamellae (inferred to be högbomite), as well as oriented short needles and particles. In addition, trace-element analyses revealed two types of spinel from this new deposit: attractive blue stones that showed an average Co concentration of 32 ppm (designated type I), and darker material with distinctly higher Co (averaging 200 ppm; designated type II). The latter showed a beautiful blue colour only when cut into melee-sized stones (i.e. about 2 mm diameter). Based on their trace-element composition, stones from this new deposit near Lukande can be separated from Co-bearing spinels from Vietnam, Sri Lanka and Pakistan. U-Pb dating of surface-reaching zircon inclusions indicates the Tanzanian spinels formed during a late stage of the East African Orogeny, possibly overprinted by the Kuunga-Malagasy orogeny (about 500–570 million years ago).
Keywords
gems, spinel, cobalt-blue spinel, Tanzania, spinel inclusions
Origin of Emeralds in a Late-Eighteenth-Century Pectoral Cross and Ring from St Peter’s Archabbey, Salzburg, Austria
Schmetzer, K. and Gilg, H.A. (2022)
Journal Article · Source: Journal of Gemmology · Volume: Vol. 38 · Issue: No. 3 · Pages: pp. 272–283
Abstract
A pectoral cross with nine emeralds and a ring containing one emerald were donated in 1786 to newly elected Abbot Dominikus Hagenauer of St Peter’s Abbey, Salzburg, Austria. Both jewels were examined by microscopy and with a portable X-ray fluorescence unit. The emeralds’ inclusion patterns and chemical properties indicate they are of Colombian origin, although oral tradition has assumed they came from Austria’s Habachtal deposit. The faceting style of the accompanying diamonds indicates that the ring might be somewhat older than the pectoral cross.
Keywords
gems, beryl, emerald, Austria, Habachtal
Die Beryll-Gruppe — eine Übersicht zu den Varietäten Aquamarin, Morganit, Heliodore und Goldberyl
The beryl group: An overview of the varieties aquamarine, morganite, heliodor, and golden beryl
Henn, U. (2022)
Journal Article · Source: Gemmologie: Zeitschrift der Deutschen Gemmologischen Gesellschaft · Volume: Vol. 71 · Issue: No. 1/2 · Pages: pp. 3–26 · Language: in German
Abstract
The first part of this special issue deals with the origin of the term beryl as well as the denomination of the as gemstones significant varieties, except emerald. Following is a survey of the relevant physical properties that determine crystal structure, crystal chemistry and crystal morphology, as well as gemmological characterization. After a short description of the most important inclusion features the formation conditions and the occurrences are presented, specified for beryl in gem quality. Subsequently the application of the mineral beryl as well as exceptional and famous beryls are described.
Keywords
gems, beryl, aquamarine, morganite, heliodore, goshenite
Mineral component and genesis of high-grade green jadeite jade from Guatemala
Wang, L., Zhang, H., Liu, J., Wang, L., Ouyang, Q., Liu, D. and Liu, W. (2022)
Journal Article · Source: Journal of Gems & Gemmology · Volume: Vol. 24 · Issue: No. 5 · Pages: pp. 11–30 · Language: in Chinese with English abstract
Abstract
High-grade green jadeite jade samples from Guatemala were selected as the research objects. Gem microscope, polarizing microscope, microscopic laser Raman spectrometer, and electron probe microanalyser were used to analyze the appearance characteristics, magnification features, constituent minerals, microstructures, Raman spectra, and mineral chemical compositions of the samples. Based on constituent minerals and their evolution, three periods of mineralization were observed. The product of the early mineralization period is jadeite with coarse-grained, hypautomorphic–automorphic granular-columnar texture and very pure chemical composition. The main mineralization period is characterized by metasomatism, with earlier-stage products being fine-grained jadeite containing relatively higher FeO, Cr₂O₃, MgO, and CaO contents compared to jadeite from the early period, and later-stage products being fine-grained omphacite with high MgO and CaO contents, whose green color shades correspond to Cr₂O₃ variation. The late mineralization period products consist of jadeite (or albite) + titanite in a filling texture, with titanite mainly distributed in reticulated veins between jadeite/omphacite particles or in microfractures. The combination of jadeite (or albite) + titanite + fluid inclusions formed during this late stage appears as white cotton-like zones in jadeite jade, representing fluid-melt inclusions. The fluid phase in these inclusions contains CO₂ and CO, with a strong characteristic Raman shift peak at 2,145 cm⁻¹, indicating a highly reductive formation environment with high CO content, corroborated by the presence of amorphous carbon in the samples. Jadeite is the main or one of the main minerals in most of the high-grade Guatemalan green jadeite jade samples studied. In such samples, the late-stage assemblage of jadeite + reticulated titanite + CO-dominated fluid inclusions commonly found in white “cotton” areas serves as an important reference feature for distinguishing Guatemalan high-grade green jadeite jades from Burmese green jadeite jades.
Keywords
gems, jade, jadeite, fei cui, Guatemala jadeite, fei cui, imperial jade
Microscopic exploration of gem and mineral surfaces
Renfro, N. (2022)
Journal Article · Source: Gems&Jewellery · Volume: Vol. 31 · Issue: No. 3 · Pages: pp. 22–25
Abstract
Nathan Renfro, GIA’s manager of colored stones, explains how studying the surface of minerals and gemstones can provide a wealth of information about the material.
Keywords
gems, corundum, inclusions.5, diamond, quartz, synthetic ruby
Émeraudes, tout un monde!
Emeralds, A Whole World
Giuliani, G. (2022)
Edited Book · Publisher: Les Editions du Piat · Pages: 448 pp. · Language: in French
Abstract
Superb book on emeralds around the world, covering the history, geology and gemology of emerald in all the major localities. Beautifully illustrated and printed.
Keywords
gems, beryl, emerald, Afghanistan, Brazil, Colombia, China, Zimbabwe, Pakistan, Zambia, Madagascar, Mozambique, inclusions, history
Gem Notes: Blue sapphires reportedly from Azad Kashmir
Huang, T. and Gao, Y. (2022)
Journal Article · Source: Journal of Gemmology · Volume: Vol. 38 · Issue: No. 2 · Pages: pp. 122–124
Keywords
gems, corundum, Pakistan.12, inclusions.5
Gem Notes: Zircon inclusions in emeralds from Lake Manyara, Tanzania
Hennebois, U., Delaunay, A. and Karampelas, S. (2022)
Journal Article · Source: Journal of Gemmology · Volume: Vol. 38 · Issue: No. 2 · Pages: pp. 117–118
Keywords
gems, beryl, emerald, Egypt, inclusions
Spinel from the Pamir Mountains in Tajikistan
Schwarz, D., Liu, Y., Zhou, Z., Lomthong, P. and Rozet, T. (2022)
Journal Article · Source: Journal of Gemmology · Volume: Vol. 38 · Issue: No. 2 · Pages: pp. 138–154
Keywords
gems, spinel, Tajikistan, Afghanistan, inclusions
Inclusion and spectral characteristics of sapphire from Ilakaka, Madagascar
Liang, B. and Chen, M. (2022)
Journal Article · Source: Journal of Gems & Gemmology · Volume: Vol. 24 · Issue: No. 1 · Pages: pp. 28–38 · Language: in Chinese with English Abstract
Abstract
The inclusions and spectral characteristics of blue and orange sapphire from Ilakaka, Madagascar have been studied by Raman spectroscopy, infrared spectroscopy, LA-ICP-MS, UV-Vis-NIR absorption spectroscopy and fluorescence spectroscopy. This study aimed to enrich the information of characteristics of sapphire from Ilakaka, Madagascar. The results showed that the characteristic inclusions of sapphire from Ilakaka included a large number of liquid CO₂-filled negative crystals and healed fissures filled with pseudosecondary inclusions such as goethite and sulfur. It also contained a variety of solid inclusions, such as calcite, graphite, phlogopite, rutile, hematite and kaolinite. The content of Fe in sapphire was positively correlated with the intensity of blue tone. The absorption lines at 377, 387 nm and 451 nm associated with Fe³⁺ were found in all types of sapphire, and the increase of Fe content could promote the formation of Fe³⁺–Fe³⁺ exchange-coupled ion pairs and enhance the absorption at 377 nm and 451 nm. R1 (694 nm) and R2 (693 nm) fluorescence lines of Cr³⁺ were observed in the fluorescence spectra of almost all samples. Orange sapphires had wide fluorescence peaks at 400–480 nm. The low temperature annealing experiment showed that these fluorescence peaks had poor thermal stability and tended to disappear when heated to 250 °C, while the fluorescence peaks increased significantly when heated to 300 °C. The thermo behavior of those fluorescence peaks may be associated with hole centers [V_Al⁺ + O⁻] and [Mg²⁺ + O⁻].
Keywords
gems, corundum, Madagascar.12, Ilakaka, sapphire
Classic Collections of 2020 China Jade Carving & Stone Carving Works Awarded with Tian Gong Prize
2020中国玉雕·石雕作品天工奖"典藏集"
Yan, A. (2021)
Edited Book · Publisher: 中国地质大学出版社 [China University of Geosciences Press] · Pages: 296 pp. · Language: in Chinese
Abstract
This extensively illustrated catalogue presents the award-winning works from the 2020 Tiangong Prize, one of China’s major national competitions for contemporary jade and stone carving. The collection documents the extraordinary range of materials, techniques, and artistic approaches employed by modern Chinese carvers, encompassing jade and other ornamental stones fashioned as figures, animals, landscapes, vessels, scholar’s objects, and sculptural compositions. Works combine traditional Chinese subjects and symbolism with increasingly individual and contemporary approaches to design, while exploiting the natural color, texture, translucency, inclusions, and form of the rough material as integral elements of the finished carving. The volume provides a valuable visual record of contemporary Chinese lapidary craftsmanship and changing aesthetic preferences, demonstrating the continuing importance of jade carving as both a traditional craft and a modern sculptural art. As a dated record of prize-winning works, it is particularly useful for documenting materials, carving styles, subject matter, and technical standards current in the Chinese jade and ornamental-stone industry in 2020.
Keywords
gems, jade, nephrite, jadeite, fei cui, China, Burma, Chinese jade carving, coral, agate, quartz, rock crystal, chalcedony, onyx, amethyst, turquoise
Purple gem spinel from Vietnam and Afghanistan: Comparison of trace element chemistry, cause of color, and inclusions
Belley, P.M. and Palke, A.C. (2021)
Journal Article · Source: Gems & Gemology · Volume: Vol. 57 · Issue: No. 3, Fall · Pages: pp. 228–238
Abstract
This study compares two purple gem spinel samples with regard to trace element chemistry and visible light absorption spectra, and presents the first reported example of a spinel with a saturated purple color caused predominantly by chromium and cobalt. Sample VN, from a placer deposit in the Luc Yen district of Vietnam, exhibited strong saturation, orange-red fluorescence in UV, and magnesite and graphite inclusions. Sample AF was from Badakhshan, Afghanistan, with light to medium saturation and containing phlogopite, amphibole, and probable fluid inclusions. UV-Vis-NIR spectra are compared along with trace element chemistry. Sample VN is colored primarily by cobalt (17.9 ppma) and chromium (593 ppma), with minor color contribution from Fe (2437 ppma), and contains significantly more cobalt than typical Cr-enriched red, pink, and purple gem spinels (
Keywords
gems, spinel, Afghanistan, Vietnam
Raman spectroscopic investigation of zircon in gem-quality sapphire: Application in origin determination
Xu, W. and Krzemnicki, M.S. (2021)
Journal Article · Source: Journal of Raman Spectroscopy · Volume: Vol. 52
Abstract
In this study, zircon inclusions in selected 115 unheated sapphires originating from metamorphic deposits were studied by confocal micro‐Raman spectroscopy. By comparing Raman features of zircon inclusions in gem‐quality sapphires from Myanmar, India (Kashmir), Sri Lanka, and Madagascar, it could be established that those of younger age (sapphires from Myanmar and India [Kashmir]) contain zircon inclusion which exhibit relatively low ʋ1 and ʋ3 band positions and also smaller FWHM (ʋ3) than those in the older sapphires from Sri Lanka and Madagascar. Binary plotting of ʋ1 versus ʋ3 frequencies (Figure 3) and ʋ3 wavenumber versus FWHM of the studied zircon inclusions provide a method to distinguish young sapphires formed during Alpine‐Himalayan orogeny (Kashmir, Myanmar) from those related to the Pan‐African orogeny (Sri Lanka, Madagascar). This study shows the potential of the non‐destructive method on zircon inclusions in sapphires to be used to distinguish their origin as a service to the commercial gem trade. Zircon inclusions in selected 115 unheated sapphires originating from metamorphic deposits—Myanmar, India (Kashmir), Sri Lanka, and Madagascar—were studied by confocal micro‐Raman spectroscopy. This study shows the potential of the non‐destructive method on zircon inclusions in sapphires to be used to distinguish their origin as a service to the commercial gem trade.
Keywords
gems, corundum, inclusions.5, India.12, Kashmir sapphire, Madagascar.12, Sri Lanka.12, Burma.12, zircon
Sapphires from Anakie, Australia: A Closer Look at Blue, Yellow, Green and Bicolor Sapphires
Saeseaw, S., Vertriest, W. and Palke, A. (2021)
Report · Source: GIA News from Research · Publisher: Gemological Institute of America · Pages: 18 pp.
Abstract
Australia has a long and rich sapphire mining history, yet the blue gems from Down Under have rarely been fully appreciated. While they were most desired in the early 1900s, their position has faded to the background. That doesn’t mean that mining stopped; both large and small operations kept operating in the last decades. Recent efforts have cast a new light on the variety of sapphires in Australia, which includes classic blues and yellow, green, and bicolor stones. This suite of colors is also referred to as BGY sapphires, which are classically related to alkali-basalt eruptions. In this study, we take a deeper look at the colors of these sapphires and what caused them, as well as the inclusion scenes observed in these gems.
Keywords
gems, corundum, Australia.12, Queensland, Rubyvale, Sapphire
Cation disorder caused by olivine-ringwoodite phase transition mechanism, possible explanation for blue olivine inclusion in a diamond
Bassett, W.A. and Skalwold, E.A. (2021)
Journal Article · Source: Minerals · Volume: Vol. 11 · Issue: No. 22 · Pages: 22 pp.
Abstract
Synchrotron X-ray diffraction, as well as visual observations, in a diamond anvil cell (DAC) using soft metal gaskets or slightly reducing gas environment, have revealed that the olivine-ringwoodite transition in olivines of several compositions take place in two steps: step 1: displacive restacking of the oxygen layers, followed by step 2: diffusive reordering of the cations. The initiation of the phase transition was observed at temperatures as low as 200°C below the reported temperature for the phase transition under hydrostatic conditions. These observations, especially residual disordered cations, have important implications for deep-focus earthquakes, the ability of ringwoodite to host surprising amounts of water, and possibly the observation of a blue olivine inclusion in a natural diamond from Brazil and in a pallasitic meteorite from Russia.
Keywords
gems, diamond, mantle; olivine; ringwoodite; wadsleyite; high pressure-temperature; shear deformation; diamond anvil cell; synchrotron radiation
Low-temperature heat treatment of pink sapphires from Ilakaka, Madagascar
Saeseaw, S., Khowpong, C. and Vertriest, W. (2020)
Journal Article · Source: Gems & Gemology · Volume: Vol. 56 · Issue: No. 4, Winter · Pages: pp. 448–457
Abstract
Rutile, titanium dioxide (TiO₂), is a tetragonal mineral that generally occurs in corundum as silk (exsolution-formed needles), dust-like exsolution particles, or macroscopic crystal inclusions. Rutile crystals can have orange to deep red-brown coloration, and the crystal shapes can be rounded or euhedral. The author recently examined a 4.24 ct faceted transparent blue sapphire from Afghanistan. The stone contained dusty flake-like inclusions, naturally healed fractures, lathe-like inclusions, twinning, rounded colorless crystals identified as apatite (RRUFF R040098), and an unusual long prismatic orange crystal identified as rutile (RRUFF R040049). This rutile crystal shape (figure 12) is not typical for corundum, particularly in blue sapphire.
Keywords
gems, corundum, treatments.6, inclusions.5, Madagascar.12, pink sapphire
Inclusion and trace element characteristics of emeralds from Swat Valley, Pakistan
Guo, H., Yu, X., Zheng, Y., Sun, Z. and Ng, M.F.-Y. (2020)
Journal Article · Source: Gems & Gemology · Volume: Vol. 56 · Issue: No. 3, Fall · Pages: pp. 336–355
Abstract
Swat Valley has become an important source of emeralds, including recently discovered trapiche-type crystals. In this study, emerald samples from Swat were examined by standard gemological testing, UV-Vis-NIR, FTIR, Raman analysis, EDXRF, and LA-ICP-MS. The study found three-phase hexagonal inclusions consisting of water, gaseous carbon dioxide and nitrogen, and a magnesite crystal. The gaseous mixture in two-phase inclusions is characteristic in both trapiche-type (CO₂ + N₂) and non-trapiche samples (CO₂ + N₂ + CH₄). Mineral inclusions of hematite, magnetite, rutile, graphite, and siderite are reported for the first time. Regular non-trapiche-type Swat emeralds contain high chromium (avg. 7471 ppmw), alkali metal (avg. 21,040 ppmw), magnesium (avg. 34,263 ppmw), and iron (avg. 9265 ppmw), as well as scandium (avg. 633 ppmw). Infrared spectra show that the absorption of type II H₂O is stronger than that of type I H₂O. Logarithm plots of trace elements appear to be diagnostic. Based on Raman spectroscopy, the trapiche-type emeralds’ colorless core, light green hexagonal growth zone area, and green rim are emerald, while the six black arms are a mixture of hematite and graphite.
Keywords
gems, beryl, emerald, Pakistan, Swat
Identification of opaque sulfide inclusions in rubies from Mogok, Myanmar and Montepuez, Mozambique
Vertriest, W. and Palke, A. (2020)
Book Section · Source: Mineralogy and Geochemistry of Ruby · Publisher: MDPI · Pages: pp. 205–221
Abstract
The red variety of corundum owes its color and strong fluorescence to the presence of Cr, as well as traces of Fe. The latter can reduce the fluorescence and thus impact the appearance of the final gem. Gem quality rubies are rarely available for scientific study and even less common in their rough form. Opaque inclusions in rubies are often removed during faceting and remain unidentified. This study aims to identify opaque inclusions in rubies from the two most common origins seen in the high end market today: Mogok, Myanmar and Montepuez, Mozambique. Using electron probe microanalaysis (EPMA) the inclusions were identified as sphalerite and pyrrhotite in Mogok rubies. The paragenesis of Myanmar, marble-related rubies is fairly well understood and no Fe-rich minerals apart from sulfides have been identified. Opaque inclusions in Mozambican rubies are a complex mix of Fe-Cu-Ni sulfides with exsolution textures. These inclusions are interpreted to be small amounts of sulfide melt trapped during corundum formation. The different sulfide phases crystallized from this entrapped melt and some phases experienced later exsolution during cooling. The formation of amphibole-related, Mozambican rubies is not well understood, but it is obvious that very different processes are at work compared to the marble-related Myanmar ruby deposits.
Keywords
gems, corundum, inclusions.5, Mozambique.12, Burma.12
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.
About Four Treasures
Four Treasures is Lotus Gemology's freely accessible gemological reference database. Use the full database to search by author, title or keyword and explore literature on gemology, mineralogy, jewelry and related fields. Where available, hyperlinks on titles may lead directly to the full publication.