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danalite

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Journal Article
Published: 01 August 2022
American Mineralogist (2022) 107 (8): 1598–1610.
...) analyses indicate that these helvine-group minerals are oscillatory-zoned helvine-danalite. Both the helvine and danalite zones are mixed with varying proportion of the other helvine-group end-member, and our studies indicate that the oscillatory zoning was formed mainly by periodic fluctuations...
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Journal Article
Published: 01 March 2017
The Canadian Mineralogist (2017) 55 (2): 195–206.
...Gary Zito; Sarah L. Hanson Abstract A miarolitic cavity in a pegmatite in Cheyenne Canyon, El Paso Co., Colorado has an unusual mineral assemblage that includes epitaxial genthelvite overgrowths on danalite cores. The cavity was lined with white microcline crystals with clear epitaxial albite...
FIGURES
First thumbnail for: Genthelvite Overgrowths On <span class="search-hig...
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Journal Article
Published: 01 December 2003
The Canadian Mineralogist (2003) 41 (6): 1413–1422.
...Sytle M. Antao; Ishmael Hassan; John B. Parise Abstract The structural behavior of danalite, ideally Fe 8 [Be 6 Si 6 O 24 ]S 2 , at atmospheric pressure and from 33 to 1035°C on heating, was determined by using in situ synchrotron X-ray powder-diffraction data (λ = 0.92249 Å) and Rietveld...
FIGURES
First thumbnail for: THE STRUCTURE OF <span class="search-highlight">DA...
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Journal Article
Published: 01 February 2002
The Canadian Mineralogist (2002) 40 (1): 163–172.
...Sytle M. Antao; Ishmael Hassan Abstract Differential thermal analyses (DTA) and thermogravimetric analyses (TG) were carried out on sodalite, tugtupite, danalite, and helvite using a Netzsch STA 409 EP/3/D simultaneous TG–DTA apparatus. In the DTA and TG experimental run, a weighed amount of finely...
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First thumbnail for: THERMAL ANALYSES OF SODALITE, TUGTUPITE, <span cla...
Second thumbnail for: THERMAL ANALYSES OF SODALITE, TUGTUPITE, <span cla...
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Journal Article
Published: 01 April 1996
Mineralogical Magazine (1996) 60 (2): 375–379.
Journal Article
Published: 01 April 1980
American Mineralogist (1980) 65 (3-4): 355–360.
...D. M. Burt Abstract End-member danalite is compositionally equivalent to a mixture of pyrrhotite, phenakite, and fayalite, but danalite’s natural occurrences with pyrite, magnetite, and quartz suggest that it is stable under somewhat more sulfidizing conditions than pyrrhotite and more oxidizing...
Journal Article
Published: 01 December 1957
The Canadian Mineralogist (1957) 6 (1): 68–71.
Journal Article
Published: 01 June 1944
American Mineralogist (1944) 29 (5-6): 163–191.
...Jewell J. Glass; Richard H. Jahns; Rollin E. Stevens Abstract Helvite and danalite occur at Iron Mountain in Sierra and Socorro Counties, south-western New Mexico, in a metamorphic contact zone between Paleozoic limestone and Tertiary rhyolites and granites. The host rock is a dark, banded tactite...
Image
Backscattered electron (BSE) images of helvine-group minerals from Dulong: (a–b) an euhedral-subhedral oscillatory-zoned helvine-danalite grain, showing intergrowth of sphalerite, talc, biotite, and helvine-danalite. In general, the dark-gray and bright zones are helvine and danalite, respectively; (c) fluorite veins or grains intergrown with sphalerite and pyrrhotite in the helvine-danalite; (d–f) cassiterite, biotite, ilmenite, and apatite in the danalite zone. Abbreviations: Ilm = ilmenite; Ap = apatite, and as in Figure 3.
Published: 01 August 2022
Figure 4. Backscattered electron (BSE) images of helvine-group minerals from Dulong: ( a–b ) an euhedral-subhedral oscillatory-zoned helvine-danalite grain, showing intergrowth of sphalerite, talc, biotite, and helvine-danalite. In general, the dark-gray and bright zones are helvine and danalite
Image
Crystal drawing of a danalite crystal (a) completely enclosed by a genthelvite dodecahedron and (b) partially enclosed by a genthelvite dodecahedron. The danalite is exposed as a triangular face.
Published: 01 March 2017
Fig. 4. Crystal drawing of a danalite crystal (a) completely enclosed by a genthelvite dodecahedron and (b) partially enclosed by a genthelvite dodecahedron. The danalite is exposed as a triangular face.
Image
The crystal structures of hsinghualite, trimerite and danalite; (a) hsinghualite projected onto (001); large circles are Ca atoms, small circles are Li atoms; (b) trimerite projected onto (010); circles are Ca and Mn atoms, tetrahedra occupy the vertices of a 63 net; (c) trimerite projected onto (100); Mn atoms are shown as circles; (d) danalite projected onto (001); circles are Fe atoms; (e) danalite projected onto (001); FeO3S tetrahedra are trellis-shaded.
Published: 01 January 2002
Figure 29. The crystal structures of hsinghualite, trimerite and danalite; (a) hsinghualite projected onto (001); large circles are Ca atoms, small circles are Li atoms; (b) trimerite projected onto (010); circles are Ca and Mn atoms, tetrahedra occupy the vertices of a 6 3 net; (c) trimerite
Image
Rose genthelvite with an exposed tetrahedral face of the danalite core. The danalite face is red except where it is coated by either (a) hematite after siderite or (b) a thin layer of beige genthelvite. Field of view is 9 mm.
Published: 01 March 2017
Fig. 5. Rose genthelvite with an exposed tetrahedral face of the danalite core. The danalite face is red except where it is coated by either (a) hematite after siderite or (b) a thin layer of beige genthelvite. Field of view is 9 mm.
Image
HR-TEM image (325,000×) showing the danalite-genthelvite interface, denoted by the solid line. The inset shows the electron diffraction pattern down the [011] axis from the whole image which shows the overall coherency of the danalite and genthelvite lattices.
Published: 01 March 2017
Fig. 12. HR-TEM image (325,000×) showing the danalite-genthelvite interface, denoted by the solid line. The inset shows the electron diffraction pattern down the [011] axis from the whole image which shows the overall coherency of the danalite and genthelvite lattices.
Journal Article
Published: 17 March 2023
Mineralogical Magazine (2023) 87 (3): 415–432.
... to pseudomorphs after a primary Be mineral (beryl > phenakite, helvine–danalite); and (3) a distal type on brittle fractures and fissures of host pegmatite. The mineral assemblages are highly variable: (1) axinite-(Mn), smectite, calcite and pyrite; (2) bertrandite, milarite, secondary beryl, bazzite, K...
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Compositions of genthelvite, danalite and helvine expressed as percentages of Zn + Fe + Mn atoms.
Published: 13 February 2024
Figure 6. Compositions of genthelvite, danalite and helvine expressed as percentages of Zn + Fe + Mn atoms.
Journal Article
Published: 01 May 2020
The Canadian Mineralogist (2020) 58 (3): 367–379.
...; Precambrian with Caledonian metamorphic overprint) contains Zn-rich danalite. The Ågskardet helvine contains up to 0.46 wt.% SnO 2 , and the Heftetjern ternary helvine shows a maximum of 1.74 wt.% Sc 2 O 3 . Helvine minerals were also analyzed from three occurrences connected to peralkaline granite (ekerite...
FIGURES
First thumbnail for: Helvine-group minerals from Norwegian granitic peg...
Second thumbnail for: Helvine-group minerals from Norwegian granitic peg...
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Published: 01 March 2017
TABLE 1. GENTHELVITE AND DANALITE COMPOSITIONS
Journal Article
Published: 01 August 2004
The Canadian Mineralogist (2004) 42 (4): 1047–1056.
... and danalite). Abstract Nous avons déterminé le comportement structural d’un composé synthétique dérivé de la sodalite, et ayant la composition Ca 8 [Al 12 O 24 ](CrO 4 ) 2 , à pression ambiante et au cours d’un chauffage entre 463 à 982°C, en utilisant la diffraction X in situ sur poudre, avec...
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First thumbnail for: CHROMATE ALUMINATE SODALITE, Ca 8 [Al 12 O 24 ](Cr...
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SEM photomicrograph of a genthelvite overgrowth on a danalite core.
Published: 01 March 2017
Fig. 3. SEM photomicrograph of a genthelvite overgrowth on a danalite core.
Image
Published: 01 February 2002
TABLE 1. CHEMICAL COMPOSITION OF SODALITE, TUGTUPITE, DANALITE, AND HELVITE