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collinsite

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Journal Article
Published: 01 October 2006
The Canadian Mineralogist (2006) 44 (5): 1181–1196.
...Sasha Herwig; Frank C. Hawthorne Abstract The crystal structures of brandtite [Ca 2 (Mn,Mg)(AsO 4 ) 2 (H 2 O) 2 , monoclinic, a 5.877(1), b 12.957(2), c 5.675(1) Å, β 108.00(3)°, V 411.0 Å 3 , space group P 2 1 / c , Z = 2], collinsite [Ca 2 (Mg,Fe)(PO 4 ) 2 (H 2 O) 2 , triclinic, a 5.729(1), b...
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Journal Article
Published: 01 August 2001
The Canadian Mineralogist (2001) 39 (4): 1081–1094.
...Ruslan P. Liferovich; Yakov A. Pakhomovsky; Alla N. Bogdanova; Elena G. Balaganskaya; Kauko V.O. Laajoki; Seppo Gehör; Nikita V. Chukanov Abstract Several generations of collinsite were formed during the hydrothermal alteration of phoscorite and dolomite carbonatite in the Kovdor alkaline...
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Morphology of <span class="search-highlight">collinsite</span> in vugs of the veins of altered dolomite carbonati...
Published: 01 August 2001
F ig . 2. Morphology of collinsite in vugs of the veins of altered dolomite carbonatite in the NE-trending fault zone. Backscattered electron images. (a) Serrate aggregate of collinsite crystals. (b) Cluster of collinsite crystals on late dolomite. (c) Aggregate of strontiowhitlockite
Image
Morphology of <span class="search-highlight">collinsite</span> in vugs of the veins of altered dolomite carbonati...
Published: 01 August 2001
F ig . 2. Morphology of collinsite in vugs of the veins of altered dolomite carbonatite in the NE-trending fault zone. Backscattered electron images. (a) Serrate aggregate of collinsite crystals. (b) Cluster of collinsite crystals on late dolomite. (c) Aggregate of strontiowhitlockite
Image
Morphology of <span class="search-highlight">collinsite</span> in vugs of the veins of altered dolomite carbonati...
Published: 01 August 2001
F ig . 2. Morphology of collinsite in vugs of the veins of altered dolomite carbonatite in the NE-trending fault zone. Backscattered electron images. (a) Serrate aggregate of collinsite crystals. (b) Cluster of collinsite crystals on late dolomite. (c) Aggregate of strontiowhitlockite
Image
Morphology of <span class="search-highlight">collinsite</span> in vugs of the veins of altered dolomite carbonati...
Published: 01 August 2001
F ig . 2. Morphology of collinsite in vugs of the veins of altered dolomite carbonatite in the NE-trending fault zone. Backscattered electron images. (a) Serrate aggregate of collinsite crystals. (b) Cluster of collinsite crystals on late dolomite. (c) Aggregate of strontiowhitlockite
Image
Spatial relationship between Sr-poor <span class="search-highlight">collinsite</span> and strontian <span class="search-highlight">collinsite</span>. (...
Published: 01 August 2001
F ig . 4. Spatial relationship between Sr-poor collinsite and strontian collinsite. (a, b, c) Peripheral concentric zone composed of strontian collinsite on an aggregate of Sr-poor collinsite. (d, e) The opposite relationship. Scanning images of polished samples in back-scattered electrons (e
Image
Spatial relationship between Sr-poor <span class="search-highlight">collinsite</span> and strontian <span class="search-highlight">collinsite</span>. (...
Published: 01 August 2001
F ig . 4. Spatial relationship between Sr-poor collinsite and strontian collinsite. (a, b, c) Peripheral concentric zone composed of strontian collinsite on an aggregate of Sr-poor collinsite. (d, e) The opposite relationship. Scanning images of polished samples in back-scattered electrons (e
Image
Spatial relationship between Sr-poor <span class="search-highlight">collinsite</span> and strontian <span class="search-highlight">collinsite</span>. (...
Published: 01 August 2001
F ig . 4. Spatial relationship between Sr-poor collinsite and strontian collinsite. (a, b, c) Peripheral concentric zone composed of strontian collinsite on an aggregate of Sr-poor collinsite. (d, e) The opposite relationship. Scanning images of polished samples in back-scattered electrons (e
Image
Spatial relationship between Sr-poor <span class="search-highlight">collinsite</span> and strontian <span class="search-highlight">collinsite</span>. (...
Published: 01 August 2001
F ig . 4. Spatial relationship between Sr-poor collinsite and strontian collinsite. (a, b, c) Peripheral concentric zone composed of strontian collinsite on an aggregate of Sr-poor collinsite. (d, e) The opposite relationship. Scanning images of polished samples in back-scattered electrons (e
Image
Spatial relationship between Sr-poor <span class="search-highlight">collinsite</span> and strontian <span class="search-highlight">collinsite</span>. (...
Published: 01 August 2001
F ig . 4. Spatial relationship between Sr-poor collinsite and strontian collinsite. (a, b, c) Peripheral concentric zone composed of strontian collinsite on an aggregate of Sr-poor collinsite. (d, e) The opposite relationship. Scanning images of polished samples in back-scattered electrons (e
Image
IR absorption powder spectra of strontian <span class="search-highlight">collinsite</span> (1) and Sr-poor collin...
Published: 01 August 2001
F ig . 5. IR absorption powder spectra of strontian collinsite (1) and Sr-poor collinsite (2), corresponding to anal. 1 and anal. 9 in Table 1 .
Journal Article
Published: 01 August 2003
The Canadian Mineralogist (2003) 41 (4): 981–988.
...Olga V. Yakubovich; Werner Massa; Ruslan P. Liferovich; Polina G. Gavrilenko; Alla N. Bogdanova; Pekka Tuisku Abstract Hillite (хиллит in Russian ), ideally Ca 2 (Zn,Mg)[PO 4 ] 2 ·2H 2 O, is a new zinc-dominant analogue of collinsite, isostructural with fairfieldite. It occurs in unmetamorphosed...
FIGURES
Journal Article
Published: 21 October 2022
The Canadian Mineralogist (2022) 60 (5): 837–847.
... can be considered a combination of the collinsite and messelite structures alternating along [001], thus representing a new structure type for minerals with kröhnkite-type chains. The discovery of dondoellite raises the question as to whether polymorphs of fairfieldite, Ca 2 Mn 2+ (PO 4 ) 2 ·2H 2 O...
FIGURES | View All (8)
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The crystal structures of bøggildite, <span class="search-highlight">collinsite</span> and fairfieldite: (a) the ...
Published: 01 January 2002
Figure 19. The crystal structures of bøggildite, collinsite and fairfieldite: (a) the [Al 2 (PO 4 )F 9 ] chain in bøggildite; (b) bøggildite projected onto (100); Ca atoms are shown as dark circles, Na atoms are shown as shaded circles; (c) collinsite projected onto (100); (d) fairfieldite
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<span class="search-highlight">Collinsite</span>–kovdorskite stockwork in the N-trending fault-zone that cross-cu...
Published: 01 August 2001
F ig . 1. Collinsite–kovdorskite stockwork in the N-trending fault-zone that cross-cuts the phoscorites and carbonatites. (a) Sketch map. (b) Geological section. (c) Druse of collinsite and kovdorskite lining a fissure. (d) Zoned crystal of kovdorskite crystal composed of zones contaminated
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Raman spectra of dondoellite, fairfieldite, and <span class="search-highlight">collinsite</span>.
Published: 21 October 2022
Fig. 3. Raman spectra of dondoellite, fairfieldite, and collinsite.
Journal Article
Published: 01 December 2000
The Canadian Mineralogist (2000) 38 (6): 1477–1485.
..., pyrochlore, several generations of magnetite, pyrite, rutile, a ternovite-like phase, catapleiite, bobierrite, rimkorolgite, juonniite, strontiowhitlockite, collinsite (including a Sr-rich variety) and chlorite. Gladiusite occurs as acicular aggregates and as free-standing radial clusters (<2 mm...
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Journal Article
Published: 01 August 2000
The Canadian Mineralogist (2000) 38 (4): 893–898.
..., and the inner region is comprised of orange-brown lithiophilite. The core of the nodule consists of an assemblage of altered lithiophilite, locally stained red (hematite?), colorless lithiophosphate and dark brown-black clots of ercitite on collinsite, fairfieldite, whitlockite and two unidentified phosphates...
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Journal Article
Published: 01 June 2000
The Canadian Mineralogist (2000) 38 (3): 617–626.
... a strong bireflectance. Reflectance values R ε and R ω are given for λ over the interval 420–720 nm. Henrymeyerite is associated with dolomite, fluorapatite, tetra-ferriphlogopite, rimkorolgite, catapleiite, collinsite, and pyrite. The composition of henrymeyerite, as determined by electron microprobe...
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