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salammoniac

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Salammoniac: gas vent 5. (a) Distribution of salammoniac (white mineral) on quartzofeldspathic sand suggests mineralization occurred in response to a gas moving primarily toward the right in the photo. (b) Crystal faces of euhedral salammoniac do not touch or are in contact along straight-grain boundaries, suggesting sublimation from a gas, as discussed in the text (SEM). (c) Cryptocrystalline salammoniac from the same sample as b; finer-grained texture is possibly due to a faster sublimation rate (SEM).
Published: 01 November 2005
F igure 7. Salammoniac: gas vent 5. ( a ) Distribution of salammoniac (white mineral) on quartzofeldspathic sand suggests mineralization occurred in response to a gas moving primarily toward the right in the photo. ( b ) Crystal faces of euhedral salammoniac do not touch or are in contact along
Image
Blue interrupted crusts of bojarite on an aggregate of salammoniac–halite. Dark areas are very thin films of an unidentified Mn oxide. Field of view: 7 cm wide, holotype.
Published: 30 October 2020
Fig. 1. Blue interrupted crusts of bojarite on an aggregate of salammoniac–halite. Dark areas are very thin films of an unidentified Mn oxide. Field of view: 7 cm wide, holotype.
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Aggregates of triazolite crystals on salammoniac (field of view 2.2 mm). Photograph: M. Burkhardt.
Published: 02 May 2018
Fig. 1. Aggregates of triazolite crystals on salammoniac (field of view 2.2 mm). Photograph: M. Burkhardt.
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Violet microcrystalline aggregates of joanneumite on salammoniac. Field of view: 4 mm. Photograph: H.-P. Bojar.
Published: 01 February 2017
Fig. 1. Violet microcrystalline aggregates of joanneumite on salammoniac. Field of view: 4 mm. Photograph: H.-P. Bojar.
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Euhedral cubic crystals of salammoniac (AV2344a, solid fragment, SEM–SE).
Published: 01 June 2009
F ig . 10. Euhedral cubic crystals of salammoniac (AV2344a, solid fragment, SEM–SE).
Image
Recently formed minerals near the interface between the cliff face and talus slope. The white dendritic crystals are salammoniac. (FOV = 22 cm).
Published: 01 September 2016
Figure 2 Recently formed minerals near the interface between the cliff face and talus slope. The white dendritic crystals are salammoniac. (FOV = 22 cm).
Journal Article
Published: 01 December 2010
The Canadian Mineralogist (2010) 48 (6): 1359–1371.
... occurring crystals. Ammineite occurs as hypidiomorphic mm-sized blue crystals and also as powdery masses, associated with halite, atacamite, salammoniac and darapskite. The Mohs hardness is 1, the streak is light blue, the luster is vitreous, and the calculated density is 2.38 g/cm 3 at 100 K and 2.31 g/cm...
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Journal Article
Published: 01 April 2010
The Canadian Mineralogist (2010) 48 (2): 307–313.
... on a pyroclastic breccia as colorless to white prismatic crystals up to 0.2 mm in length, in association with salammoniac and kremersite. The mineral is trigonal, space group R 3 c (no. 161) with a 15.2171(14), c 8.9323(8) Å, V 1791.3(3) Å 3 and Z = 6. The strongest six reflections in the X-ray powder...
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Journal Article
Published: 01 June 2009
The Canadian Mineralogist (2009) 47 (3): 573–591.
...F ig . 10. Euhedral cubic crystals of salammoniac (AV2344a, solid fragment, SEM–SE). ...
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Image
Recently formed minerals near the interface between the cliff face and talus slope. The white dendritic crystals are salammoniac. (FOV = 22 cm). (Color online.)
Published: 01 July 2014
Figure 2 Recently formed minerals near the interface between the cliff face and talus slope. The white dendritic crystals are salammoniac. (FOV = 22 cm). (Color online.)
Journal Article
Published: 01 November 2005
American Mineralogist (2005) 90 (11-12): 1729–1739.
...F igure 7. Salammoniac: gas vent 5. ( a ) Distribution of salammoniac (white mineral) on quartzofeldspathic sand suggests mineralization occurred in response to a gas moving primarily toward the right in the photo. ( b ) Crystal faces of euhedral salammoniac do not touch or are in contact along...
FIGURES | View All (7)
Journal Article
Published: 01 April 1994
American Mineralogist (1994) 79 (3-4): 381–384.
...Anna Garavelli; Filippo Vurro Abstract Barberiite, ammonium tetrafluoroborate, occurs as a fumarolic encrustation at Fossa crater on Vulcano, Aeolian Islands, Italy. Associated minerals are sulfur, malladrite, realgar, salammoniac, cannizzarite, galenobismutite, and bismuthinite. The mineral...
Journal Article
Published: 01 November 2004
American Mineralogist (2004) 89 (11-12): 1838–1839.
... Mineralogist 2004 Corrected average enthalpies of solution for buddingtonite (−598.1 ± 2.5 kJ/mol), tobelite (−935.0 ± 3.7 kJ/mol), and salammoniac (+11.23 ± 0.04 kJ/mol) have been determined by multiplying the original enthalpies of solution by factors equal to the correct gfw (257.2733, 377.2498...
FIGURES
Journal Article
Published: 01 January 2004
American Mineralogist (2004) 89 (1): 85–93.
... solution calorimetric data from this laboratory for sanidine, albite, muscovite, paragonite, halite, sylvite, salammoniac, gibbsite, and water, along with enthalpies of formation from Robie and Hemingway (1995) for the same phases, the heats of formation at 298.15 K of buddingtonite and tobelite have been...
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Journal Article
Published: 14 October 2022
Mineralogical Magazine (2023) 87 (1): 69–78.
..., salammoniac, alacránite, bonazziite and thermessaite-(NH 4 ). In addition, there are amorphous As 2 S 3 intergrowths associated with ermakovite. The mineral typically occurs as tabular or prismatic hexagonal crystals up to 200 μm with the following forms: c (001), m (010) and p (014). Spherulites and multi...
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Journal Article
Published: 13 December 2021
Mineralogical Magazine (2022) 86 (4): 531–538.
... of phases that include a variety of vanadates, phosphates, oxalates and chlorides, some containing NH 4 + . Other secondary minerals found in association with dendoraite-(NH 4 ) are antipinite, fluorite, mimetite, mottramite, relianceite-(K), rowleyite, salammoniac, struvite, vanadinite, willemite...
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Journal Article
Published: 13 December 2021
Mineralogical Magazine (2022) 86 (4): 539–547.
... of phases. Other secondary minerals associated with relianceite-(K) are antipinite, dendoraite-(NH 4 ), fluorite, mimetite, mottramite, rowleyite, salammoniac, struvite, vanadinite, willemite, wulfenite and at least one other new mineral. Crystals of relianceite-(K) are sky blue prisms up to ~0.1 mm...
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The powder XRD patterns (CuKα, 40 kV, 40 mA, 293 K) of joanneumite (a) with its Rietveld refinement using TOPAS 4.2 (b) and difference pattern (c) are in good agreement with those of the synthetic analogue of joanneumite (d) and its Rietveld refinement (e) with difference pattern (f). Impurities of salammoniac (Sa) and gypsum (Gy) in joanneumite (a) are visible. The eight strongest lines are indexed.
Published: 01 February 2017
pattern ( f ). Impurities of salammoniac (Sa) and gypsum (Gy) in joanneumite ( a ) are visible. The eight strongest lines are indexed.
Journal Article
Published: 30 October 2020
Mineralogical Magazine (2020) 84 (6): 921–927.
...Fig. 1. Blue interrupted crusts of bojarite on an aggregate of salammoniac–halite. Dark areas are very thin films of an unidentified Mn oxide. Field of view: 7 cm wide, holotype. ...
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Journal Article
Published: 05 June 2020
Mineralogical Magazine (2020) 84 (5): 705–711.
... Mountain, Iquique Province, Tarapacá Region, Chile. Associated minerals are halite, gypsum, salammoniac and clay minerals. Ammoniotinsleyite occurs as pink to pale violet globular aggregates up to 3 mm across with individual single crystals ~10–15 μm. The mineral is brittle. Its Mohs hardness is 4. D meas...
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