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Aegirine
Aegirine (dark) with minor feldspar (light) from Malawi
General
CategorySilicate mineral, pyroxene
FormulaNaFe3+[Si2O6]
IMA symbolAeg[1]
Strunz classification9.DA.25
Crystal systemMonoclinic
Crystal classPrismatic (2/m)
(same H-M symbol)
Space groupC2/c
Unit cella = 9.658, b = 8.795
c = 5.294 [Å], β = 107.42°; Z = 4
Identification
Formula mass231.00 g/mol
ColorDark Green, Greenish Black
Crystal habitPrismatic crystals may be in sprays of acicular crystals, fibrous, in radial concretions
TwinningSimple and lamellar twinning common on {100}
CleavageGood on {110}, (110) ^ (110) ≈87°; parting on {100}
FractureUneven
TenacityBrittle
Mohs scale hardness6
LusterVitreous to slightly resinous
StreakYellowish-grey
DiaphaneityTranslucent to opaque
Specific gravity3.50–3.60
Optical propertiesBiaxial (−)
Refractive indexnα = 1.720 – 1.778 nβ = 1.740 – 1.819 nγ = 1.757 – 1.839
Birefringenceδ = 0.037 – 0.061
PleochroismX = emerald green, deep green; Y = grass-green, deep green, yellow; Z = brownish green, green, yellowish brown, yellow
2V angleMeasured: 60° to 90°, Calculated: 68° to 84°
Dispersionmoderate to strong r > v
References[2][3][4][5]

Aegirine is a mineral. It is a member of the clinopyroxene group of inosilicate minerals. Acmite is a fibrous green-colored variety of aegirine, with the name also used as a synonym. It was first described in 1821, in Kongsberg, Norway.

Etymology

[edit]

The name aegirine is derived from Ægir , a Norse mythological figure (god of the sea), as the mineral was first described from Norway.[2][3]

A synonym for the mineral is acmite (from Greek ἀκμή "point, edge") in reference to the typical pointed crystals.[6]

Chemistry and description

[edit]
Syenite with aegirine and acmite from Magnet Cove, Arkansas, US

Aegirine is the sodium endmember of the aegirine–augite series.[citation needed]

It has the chemical formula NaFeSi2O6, in which the iron is present as the ion Fe3+. In the aegirine–augite series, the sodium is variably replaced by calcium with iron(II) and magnesium replacing the iron(III) to balance the charge. Aluminum also substitutes for the iron(III). Acmite is a fibrous green-colored variety.[citation needed]

Aegirine occurs as dark green monoclinic prismatic crystals.[3] It has a glassy luster and perfect cleavage, "in two directions at near 90 degree angles".[7] It is described on Mindat.org as "slightly resinous", with its colour "dark green to greenish black, reddish brown, [or] black" Its Mohs hardness is 6 and its specific gravity is between 3.5 and 3.6.[3][4]

Associated minerals include augite, nepheline, andradite, baryte, quartz, spessartine, riebeckite, biotite, sodalite, and albite.[7]

Occurrence

[edit]

The acmite variety was first described in 1821, at Kongsberg, Norway,[8] and the aegirine variety in 1835 for an occurrence in Rundemyr, Øvre Eiker, Buskerud, Norway.[3]

This mineral commonly occurs in alkalic igneous rocks, nepheline syenites, carbonatites, and pegmatites. It also appears in regionally metamorphosed schists, gneisses, and iron formations; in blueschist facies rocks, and from sodium metasomatism in granulites. It may occur as an authigenic mineral in shales and marls. It occurs in association with potassic feldspar, nepheline, riebeckite, arfvedsonite, aenigmatite, astrophyllite, catapleiite, eudialyte, serandite, and apophyllite.[2]

Major localities include Mont Saint-Hilaire, Quebec, Canada; Kongsberg, Norway; Narsarssuk, Greenland; Kola Peninsula, Russia; Magnet Cove, Arkansas, US; Kenya; Scotland, and Nigeria.[7]

Aegirine also occurs in the syenite at the Bowral quarries in New South Wales, Australia, as described in a 1906 paper by geologist and later Antarctic explorer Douglas Mawson.[9][10]

Uses

[edit]

Aegirine is sometimes used as a gemstone.[11]

See also

[edit]

References

[edit]
[edit]
Revisions and contributorsEdit on WikipediaRead on Wikipedia

Aegirine

View on Grokipedia
from Grokipedia
Aegirine is a sodium iron with the NaFe³⁺Si₂O₆, classified within the clinopyroxene subgroup of the group. It typically occurs as prismatic or acicular crystals that are dark green to greenish-black, reddish-brown, or black in color, exhibiting a vitreous luster, a hardness of 6 on the , and a specific of 3.5 to 3.6. Named after Ægir, the Norse god of the , due to its initial discovery on a Norwegian coastal island, aegirine is distinguished by its deep coloration resulting from charge-transfer transitions, often involving Fe²⁺-Ti⁴⁺ interactions. Aegirine forms primarily in alkaline igneous environments, including syenites, nepheline syenites, and carbonatites, as well as in pegmatites and metasomatic deposits. It also appears in metamorphic settings such as regionally metamorphosed schists and gneisses, iron formations, blueschist-facies rocks, and granulites affected by sodium metasomatism, and can occur authigenically in certain shales and marls. In these contexts, aegirine often associates with minerals like nepheline, feldspar, and other sodium-rich silicates, reflecting conditions of high sodium and iron activity during crystallization or alteration. Notable occurrences of aegirine include its type locality at Rundemyr in Øvre Eiker, , , as well as Låven on the Langesundsfjorden peninsula in the same region, and the Bayan Obo deposit in , . It has also been documented in iron formations of the Cuyuna range in east-central , where it appears in manganese-rich layers, suggesting a role in sedimentary or low-grade metamorphic processes. While not a major , aegirine attracts interest among collectors for its striking crystal habits and is sometimes used in work due to its durability and color.

Etymology and History

Etymology

The name aegirine derives from , the Norse god of the sea in Scandinavian mythology, reflecting the mineral's initial discovery along the Norwegian coastline. This naming was proposed in 1834 by Norwegian mineralogist and priest Hans Morten Thrane Esmark, who identified specimens from the seaside locality of Låven in the Langesundsfjord area, and it was formally described under this name by Swedish chemist in 1835. A historical synonym for aegirine is acmite, coined earlier in 1821 by Berzelius for material from Rundemyr, ; the term originates from word akmē (ἀκμή), meaning "point" or "edge," in reference to the mineral's characteristic sharp, pointed crystal terminations. In 19th-century , acmite was initially classified as an distinct from the pyroxene-group aegirine, but by , Austrian mineralogist Gustav Tschermak had recognized them as the same , leading to the eventual prioritization of aegirine as the valid name. The acmite name was formally discredited as a separate species in 1988 by the Commission on New Minerals and Mineral Names of the International Mineralogical Association.

Discovery and Naming

Aegirine was first described as a new in 1821 by Norwegian mineralogist Petter Herman Ström based on specimens from the Rundemyr near , . Ström initially proposed the name "wernerin" to honor the German geologist , but after chemical analysis by Swedish chemist Jöns Jacob Berzelius, it was renamed "acmite," derived from the Greek word akmē meaning "point" or "edge," alluding to the mineral's characteristic acicular crystal form. In 1834, Norwegian clergyman and amateur ogist Hans Morten Thrane Esmark identified a closely related mineral on Låven in the Langesundsfjorden complex, , and suggested the name "aegirine" after , the Norse god of the sea, reflecting its coastal discovery site. Berzelius adopted and formalized this name in 1835, establishing "aegirine" for the species while retaining "acmite" for a fibrous variety. Rundemyr and Låven are now recognized as co-type localities for aegirine. Early mineralogists initially regarded acmite as an and aegirine as a distinct , leading to confusion with other silicates like due to compositional similarities. This was resolved in 1871 when Austrian mineralogist Gustav Tschermak unified them as a single , confirming aegirine as a sodium-iron end-member of the clinopyroxene group. Its identification significantly advanced 19th-century understanding of sodium-rich silicates in alkaline rocks.

Chemical Composition and Crystal Structure

Chemical Formula

Aegirine is defined by its ideal chemical formula NaFe3+Si2O6\mathrm{NaFe^{3+}Si_2O_6}, which represents a sodium-iron silicate composition characteristic of sodic pyroxenes. This formula indicates the presence of sodium (Na) in the larger cation site, trivalent iron (Fe³⁺) in the octahedral site, and two silicon (Si) atoms forming the tetrahedral framework with six oxygen (O) atoms. As a member of the pyroxene group, aegirine belongs specifically to the clinopyroxene subgroup, distinguished by its monoclinic crystal symmetry and structural arrangement. Within this classification, aegirine serves as the principal endmember of the sodic series, where it anchors the compositional extreme dominated by sodium and ferric iron. The fundamental structure of aegirine, like other , is based on infinite single chains of SiO4\mathrm{SiO_4} tetrahedra linked by shared oxygen atoms, forming a repeating backbone parallel to the crystal's c-axis. These chains are cross-linked by octahedral sites occupied by Fe³⁺ and other cations, with sodium coordinating in the larger interstitial positions to stabilize the framework.

Solid Solution and Substitutions

Aegirine is a key member of the aegirine-augite solid solution series within the clinopyroxene group, characterized by coupled substitutions at the M2 and M1 sites that enable compositional variability. The primary substitution involves Na⁺ at the M2 site replacing Ca²⁺, coupled with Fe³⁺ at the M1 site replacing Fe²⁺ or Mg²⁺, expressed as Na⁺ + Fe³⁺ ↔ Ca²⁺ + (Fe²⁺, Mg²⁺). This exchange allows aegirine, with its ideal endmember formula NaFe³⁺Si₂O₆, to form continuous solid solutions toward augite, (Ca,Mg,Fe)Si₂O₆, though the series is often restricted by low Fe²⁺/Fe³⁺ ratios in alkaline environments, which limit the hedenbergite (CaFe²⁺Si₂O₆) component relative to more reducing settings. Additional substitutions further diversify aegirine's composition, particularly in evolved magmatic systems. At the M1 site, higher-valence cations such as Ti⁴⁺ and Zr⁴⁺ commonly substitute for Fe³⁺, while rare earth elements (REE) can incorporate via mechanisms like Na⁺ + REE³⁺ ↔ Ca²⁺ + (Mg²⁺, Fe²⁺) or coupled with Fe³⁺ exchange. These features are evident in aegirines from fractionated alkaline melts, such as those at Mont Saint-Hilaire, Quebec, where zoning shows Ca- and Zr-rich cores transitioning to Na- and Ti-rich rims, with REE patterns displaying enrichment relative to chondrites and negative Eu anomalies. Minor Al³⁺ may enter the tetrahedral T site, but Si remains dominant at 1.96–1.99 atoms per formula unit. These solid solutions and substitutions confer stability to aegirine in peralkaline and alkaline environments, where high Na/(Na+K) ratios and oxidizing conditions favor the Na-Fe³⁺ endmember over Ca-rich pyroxenes. The incorporation of incompatible elements like Ti⁴⁺, Zr⁴⁺, and REE during late-stage enhances this adaptability, allowing aegirine to crystallize in Na-rich, low-Ca melts typical of such settings, as seen in titanian-aegirines. This compositional flexibility underscores aegirine's role as an indicator of alkaline magmatic evolution.

Physical and Optical Properties

Crystal Habit and Appearance

Aegirine belongs to the and typically exhibits a , with crystals often appearing elongated or stubby in form. These prisms are characteristically striated lengthwise and may terminate in steep or blunt pyramidal faces, aligning with common habits observed in the pyroxene group of minerals. In some occurrences, aegirine forms acicular (needle-like) crystals, contributing to its distinctive silhouette in rock matrices. The mineral's color ranges from dark green to greenish-black, with occasional reddish-brown or brownish hues, though specimens are also prevalent. Color zoning is common, often displaying patterns where the crystal edges appear darker than the core. Aegirine possesses a vitreous luster, which can appear silky in certain fibrous aggregates, enhancing its visual appeal in polished sections or hand samples. Aegirine's cleavage is perfect along two directions, specifically on the {110} planes, occurring at angles of approximately 87° and 93°, nearly at right angles. This pronounced cleavage results in well-defined, blade-like fragments when the mineral is broken. In its acmite variety, aegirine adopts a fibrous appearance, forming radiating or felted masses that contrast with the more discrete prismatic crystals of the typical form.

Mechanical and Optical Characteristics

Aegirine possesses a Mohs of 6, consistent with other clinopyroxenes. Its specific gravity ranges from 3.50 to 3.60, reflecting its dense silicate structure. The mineral produces a pale yellowish gray streak and displays translucency to opacity depending on crystal quality and thickness. Optically, aegirine is biaxial negative, with refractive indices of nα=1.722–1.776n_\alpha = 1.722–1.776, nβ=1.780–1.820n_\beta = 1.780–1.820, and nγ=1.795–1.836n_\gamma = 1.795–1.836, yielding a of δ≈0.040–0.080\delta \approx 0.040–0.080. These values highlight its high relief in thin sections, distinguishing it from lower-index pyroxenes. It exhibits distinct , appearing emerald green to deep green along the X axis, grass green to yellow along Y, and pale green to yellowish brown along Z.
PropertyValue
Refractive indicesnα=1.722–1.776n_\alpha = 1.722–1.776
nβ=1.780–1.820n_\beta = 1.780–1.820
nγ=1.795–1.836n_\gamma = 1.795–1.836
(δ\delta)≈ 0.040–0.080
Distinct: X = emerald green to deep green, Y = grass green to yellow, Z = pale green to yellowish brown

Geological Occurrence

Formation Environments

Aegirine primarily forms in alkaline igneous rocks, including syenites, phonolites, and carbonatites, where it crystallizes from sodium- and iron-rich, silica-undersaturated magmas under high-alkalinity conditions. These environments favor the stability of sodic pyroxenes like aegirine due to elevated sodium activity and oxidizing conditions that promote Fe³⁺ incorporation. In such settings, aegirine often appears in fractionated late-stage melts, where it acts as a key in peralkaline assemblages. The mineral's paragenesis in these igneous rocks typically includes associations with , , , , and , reflecting the evolution of alkali-enriched residual liquids. Aegirine also occurs in pegmatites related to alkaline intrusions and in metasomatic deposits formed through sodium metasomatism, such as fenitization around carbonatites. Secondarily, aegirine develops in regionally metamorphosed iron formations, schists, and gneisses, where it forms via Na-rich fluids during prograde or hydrothermal alteration. These metamorphic occurrences are linked to blueschist-facies conditions or sodium in granulites, often involving hydrothermal systems that introduce sodium to iron-rich protoliths.

Notable Localities

Aegirine was first described from co-type localities at Rundemyr, Øvre Eiker, , (acmite variety, 1821), and Låven, Langesundsfjorden peninsula, (aegirine variety, 1835). These sites, associated with early alkaline intrusions, remain significant for historical specimens of prismatic crystals. Among major global occurrences, in , , is renowned for its zoned aegirine crystals, which exhibit green to greenish-black coloration and form in late-stage, volatile-rich alkaline pegmatites within a carbonatite-alkaline complex. The in hosts large deposits of aegirine in the peralkaline syenites of the Khibiny and Lovozero alkaline complexes, where it occurs as a rock-forming in agpaitic rocks. In the United States, Magnet Cove in , features aegirine in igneous intrusions, including and exposures, yielding lustrous black prismatic crystals. Other notable sites include the Lueshe carbonatite complex in , of Congo, where aegirine appears in syenite-carbonatite intrusions associated with mineralization. The Ilímaussaq intrusion in southern produces sector-zoned aegirine crystals in peralkaline nepheline syenites of this agpaitic complex. More recently, aegirine has been documented in the Boziguoer Nb-Ta-Zr-Rb-REE deposit in , , linked to alkaline granite intrusions where it coexists with in peralkaline rocks.

Varieties and Synonyms

Acmite

Acmite is defined as the fibrous, acicular (needle-like) variety of aegirine, typically exhibiting a coloration. This variety is characterized by its elongated, radiating sprays of slender crystals, distinguishing it from more prismatic forms of the . Acmite serves as both a for aegirine and a specific varietal name for its acicular , historically distinguished by color but now unified under aegirine. Acmite shares the same chemical composition as aegirine, with the formula NaFe³⁺Si₂O₆, but is primarily differentiated by its distinctive rather than compositional differences. Historically, acmite was considered a separate species, initially classified among the amphiboles due to its fibrous appearance, while aegirine was recognized as a ; modern has clarified this distinction, treating acmite as a varietal name or for the acicular form of aegirine. Acmite commonly occurs in cavities and vugs within alkaline igneous rocks, such as syenites and related volcanic formations. Notable examples include specimens from Rundemyr in Øvre Eiker, , , the type locality for acmite.

Other Varieties

Aegirine forms series with , leading to aegirine-augite, a distinct species that forms a series with aegirine and , where calcium substitution for sodium occurs at the site, resulting in up to 56% Na ↔ Ca replacement in some crystals. These intermediates exhibit between pure aegirine and , with the general formula (Na,Ca)(Fe³⁺,Fe²⁺,Mg,Al)Si₂O₆, reflecting coupled substitutions that maintain charge balance without forming distinct species beyond aegirine-augite. Such aegirine-augite occurrences are documented in alkaline igneous settings, where the degree of Ca incorporation influences crystal color and , often appearing darker green due to increased Fe²⁺ content. Rare REE-enriched varieties of aegirine arise in fractionated alkaline melts, characterized by elevated concentrations relative to chondritic values and a pronounced negative . At , , these aegirines display concave REE patterns with light REE enrichment (e.g., Ce up to several hundred ppm) and heavy REE levels around 10-50 ppm, attributed to late-stage magmatic differentiation without altering the core structure. variations, such as higher TiO₂ (up to 1-2 wt%) and MnO, contribute to subtle differences in , often resulting in more prismatic or stubby forms rather than the typical acicular growth. Zoned aegirine crystals frequently incorporate Ti and Zr as inclusions or lattice substitutions, with cores enriched in Zr (up to 10,000 ppm), Hf, Sc, and Sn, transitioning to rims depleted in these elements. Sector zoning in such crystals from alkaline intrusions like Ilimaussaq shows variable Ti (2,900-11,900 ppm) and Zr (700-10,680 ppm) distributions, influencing like pleochroism intensity without defining new varieties. These zonations reflect fluctuating melt compositions during , leading to color gradients from deep cores to brownish rims due to Fe³⁺/Fe²⁺ ratios modulated by trace elements. Beyond acmite, no other distinctly named varieties are formally recognized, though pseudomorphs of aegirine after primary clinopyroxenes occur in metasomatized rocks, preserving the original crystal outlines while replacing the precursor with Na-Fe-rich compositions. These pseudomorphs, often identified in eclogitic or fenitic assemblages, exhibit partial replacement textures where aegirine overgrows igneous porphyroclasts, altering mechanical properties like without changing the external morphology.

Uses and Applications

Gemological and Collectible Uses

Aegirine serves as a minor in jewelry, primarily due to its dark to coloration and vitreous luster, which lend it an exotic appeal for collectors and designers. It is most commonly cut into cabochons for pendants and necklaces, with faceted pieces being rare owing to its opacity and hardness of 6 on the . These gems are typically set in protective mountings to safeguard against wear, and their value ranges from $20 to $182 for pendants, influenced by factors such as color intensity—where rarer greenish hues command higher prices—and overall translucence. As a collectible mineral, aegirine is prized for its striking prismatic crystals, often forming elongated, striated sprays that contrast dramatically with lighter matrix minerals like or . Specimens are valued based on crystal size, clarity, and aesthetic formation, with larger, well-defined examples fetching premium prices in mineral markets. Notable sourcing localities include in Québec, , known for sharp black crystals up to several centimeters, and the in Russia, yielding dark green prismatic clusters embedded in alkaline rocks. In metaphysical communities, aegirine enjoys popularity for its purported protective and energizing properties, such as shielding against negative energies and promoting personal empowerment, though these claims lack scientific validation. Enthusiasts often incorporate it into practices, associating it with the root chakra to enhance grounding and resilience, but its use remains confined to spiritual rather than empirical contexts.

Scientific Research and Industrial Potential

Aegirine serves as a key in petrological studies of alkaline igneous systems, where its presence signals peralkaline conditions characterized by high sodium activity and enrichment in incompatible elements. In fractionated late-stage melts, aegirine crystallizes as a product of evolution, incorporating elevated levels of rare earth elements (REE), (Zr), (Ti), and sodium (Na), which helps trace magmatic differentiation processes. For instance, research on aegirine from the complex in demonstrates strong zoning with cores enriched in Ca and Zr, transitioning to Na- and Ti-rich rims, reflecting progressive under oxidized conditions where over 85% of iron is in the Fe³⁺ state. This composition, including REE patterns with negative Eu anomalies and chondrite-normalized enrichment, underscores aegirine's utility in reconstructing the transition from parental magmas to syenites and pegmatites. Crystal chemistry investigations further elucidate aegirine's role in igneous processes through cation substitutions that respond to changing melt compositions. Common substitutions include Na-Ca exchange in the M2 site (up to 56%) and limited Al-Si disorder in the tetrahedral site (<2%), alongside Mg/Fe²⁺/Mn for Fe³⁺ in the M1 site, which stabilize the under varying and silica activities. At the Boziguoer Nb-Ta-Zr-Rb-REE deposit in , , aegirine in alkaline granites and syenites is intimately associated with pyrochlore-group minerals hosting Nb and Ta, indicating differentiation driven by Permian plume-related around 280 Ma. These substitutions provide insights into partitioning during fractional , linking aegirine to REE mobilization in peralkaline settings. Post-2021 studies have examined aegirine's stability in high-pressure environments, particularly in low-temperature metamorphic terrains. Aegirine is commonly documented in and epidote-amphibolite facies rocks, where it persists under conditions of elevated pressure and sodium metasomatism, aiding reconstructions of subduction-related fluid interactions. Such findings highlight its resilience in Na-rich, oxidized systems, contributing to models of metamorphic evolution in alkaline protoliths. Industrial applications of aegirine remain limited due to its rarity and low abundance in most deposits, precluding widespread extraction. However, it shows potential as an indicator in REE exploration, as its high Na-index and associations with critical metal-bearing phases in alkaline rocks facilitate geochemical targeting of hidden deposits. In processing contexts, aegirine from REE-rich , such as at Bayan Obo, can be roasted and leached to recover with efficiencies exceeding 97%, supporting niche uses in alloys and ceramics, though economic viability is constrained by high recovery costs. Additionally, synthetic aegirine derived from iron-silicate glasses has been explored for glass-ceramic production, leveraging its crystallization behavior for durable materials in construction and refractories.

References

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