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pascoite

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Journal Article
Published: 04 March 2022
The Canadian Mineralogist (2022) 60 (2): 341–359.
...Frank C. Hawthorne; John M. Hughes; Mark A. Cooper; Anthony R. Kampf ABSTRACT The decavanadate isopolyanion, [V 10 O 28 ] 6– , is a constituent of pascoite-family vanadate minerals and synthetic materials, and both protonated, [H x V 10 O 28 ] (6– x )– , and mixed-valence, [V 4+ x V 5+ 10– x )O 28...
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Journal Article
Published: 13 September 2021
The Canadian Mineralogist (2021) 59 (4): 771–779.
...Anthony R. Kampf; John M. Hughes; Mark A. Cooper; Frank C. Hawthorne; Barbara P. Nash; Travis A. Olds; Paul M. Adams; Joe Marty ABSTRACT Mineral species that contain the decavanadate isopolyanion [V 10 O 28 ] 6– , including its protonated and mixed-valence variants, constitute the pascoite family...
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Journal Article
Published: 01 October 2011
The Canadian Mineralogist (2011) 49 (5): 1253–1265.
...John Rakovan; Gregory R. Schmidt; Mickey E. Gunter; Barbara Nash; Joe Marty; Anthony R. Kampf; William S. Wise Abstract We report on the discovery, description and solution of the structure of a new member of the pascoite family of minerals, hughesite, from the Sunday mine, Gypsum Valley, San...
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Journal Article
Published: 01 April 2011
The Canadian Mineralogist (2011) 49 (2): 595–604.
... of the Natural History Museum of Los Angeles County under catalogue numbers 63357 and 63358. Minerals of the pascoite family (pascoite: Ca 3 V 10 O 28 ·17H 2 O) conform to the bipartite nature of mineral structures elucidated by Hawthorne (1983) . Each member of the pascoite family contains the (V 10 O...
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Journal Article
Published: 01 February 2009
The Canadian Mineralogist (2009) 47 (1): 206.
Journal Article
Published: 01 October 2008
The Canadian Mineralogist (2008) 46 (5): 1365–1372.
... , with a 23.9019(7), b 10.9993(3), c 17.0504(5) Å, β 118.284(1)°. The structure was determined using direct methods and three-dimensional X-ray-diffraction data measured with a CCD detector and refined to R = 0.0289. The mineral is a member of the pascoite group of minerals, which have a structural unit...
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Journal Article
Published: 01 June 2008
The Canadian Mineralogist (2008) 46 (3): 679–686.
...Anthony R. Kampf; Ian M. Steele Abstract Magnesiopascoite, Ca 2 Mg(V 10 O 28 )·16H 2 O, a new mineral species from the Blue Cap mine, near La Sal, San Juan County, Utah, U.S.A., is named as the Mg analogue of pascoite, Mg occupying one of the two nonequivalent Ca sites in the structure of pascoite...
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Journal Article
Published: 01 August 2005
The Canadian Mineralogist (2005) 43 (4): 1379–1386.
...John M. Hughes; Michael Schindler; Carl A. Francis Abstract The atomic arrangement of pascoite has been solved and refined to R = 0.0257 using three-dimensional data obtained with Mo K α X-radiation and a CCD detector. The mineral crystallizes in space group C 2 /m, a 19.5859(6), b 10.1405(3), c...
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Published: 13 September 2021
TABLE 1. PASCOITE FAMILY MINERALS (SPECIES LABELED PG COMPRISE THE PASCOITE GROUP AND THOSE LABELED LG COMPRISE THE LASALITE GROUP)
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Published: 18 January 2024
TABLE 8. THE PASCOITE FAMILY OF MINERALS
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Published: 04 March 2022
TABLE 1. THE MINERALS OF THE PASCOITE FAMILY
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Published: 01 August 2005
TABLE 2. ATOM POSITIONS IN PASCOITE
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Published: 01 August 2005
TABLE 1. CRYSTAL DATA AND RESULTS OF THE REFINEMENT OF THE STRUCTURE OF PASCOITE
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Published: 01 August 2005
TABLE 3. SELECTED BOND-DISTANCES AND VALENCE SUMMATIONS ( vu ) IN PASCOITE
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Hydropascoite crystals (green) with pascoite (orange); FOV 0.85 mm across.
Published: 01 March 2017
Fig. 1. Hydropascoite crystals (green) with pascoite (orange); FOV 0.85 mm across.
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Coordination around Mg in magnesiopascoite (left) and Ca1 in pascoite (right).
Published: 01 June 2008
F ig . 4. Coordination around Mg in magnesiopascoite (left) and Ca1 in pascoite (right).
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Coordination around Ca in magnesiopascoite (left) and Ca2 in pascoite (right).
Published: 01 June 2008
F ig . 5. Coordination around Ca in magnesiopascoite (left) and Ca2 in pascoite (right).
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The (V10O28)6− decavanadate unit in pascoite.
Published: 01 August 2005
F ig . 1. The (V 10 O 28 ) 6− decavanadate unit in pascoite.
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The Ca1 polyhedron in pascoite. Oxygen atom O13 is disordered into two half-occupied sites, O13A and O13B, and a hydrogen associated with O13B (H13B, Table 2) is also half-occupied. On either “side” of the equatorial plane defined by O10 and O11, either the O13A site or the pair of O13B sites is occupied. Thus, Ca1 can be 6-, 7-, or 8-coordinated with oxygen, with an average of Ca1O7. Hydrogen atom “x” = H13A, hydrogen atom “y” = H13B.
Published: 01 August 2005
F ig . 2. The Ca1 polyhedron in pascoite. Oxygen atom O13 is disordered into two half-occupied sites, O13A and O13B, and a hydrogen associated with O13B (H13B, Table 2 ) is also half-occupied. On either “side” of the equatorial plane defined by O10 and O11, either the O13A site or the pair
Journal Article
Published: 18 January 2024
The Canadian Journal of Mineralogy and Petrology (2024) 62 (1): 117–132.
...TABLE 8. THE PASCOITE FAMILY OF MINERALS ...
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