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weeksite

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Journal Article
Published: 01 April 2012
American Mineralogist (2012) 97 (4): 750–754.
...Karla Fejfarová; Jakub Plášil; Hexiong Yang; Jiří Čejka; Michal Dušek; Robert T. Downs; Madison C. Barkley; Radek Škoda Abstract The previously published structure determination of weeksite from the Anderson mine, Arizona, U.S.A., suggested that it is orthorhombic, Cmmb , with a = 14.209(2), b...
FIGURES
Journal Article
Published: 01 February 2001
The Canadian Mineralogist (2001) 39 (1): 187–195.
...Jennifer M. Jackson; Peter C. Burns Abstract The structure of weeksite, K 1.26 Ba 0.25 Ca 0.12 [(UO 2 ) 2 (Si 5 O 13 )]H 2 O, orthorhombic, a 14.209(2), b 14.248(2), c 35.869(4) Å, V 7262(2) Å 3 , space group Cmmb , has been solved by direct methods using data collected with Mo K α X-radiation...
FIGURES | View All (4)
Journal Article
Published: 01 February 1960
American Mineralogist (1960) 45 (1-2): 39–52.
... fibrous clusters. In the Thomas Kange, where it was first found, it occurs in opal veinlets in rhyolitc and as replacements of pebbles in a tuffaceous conglomerate. Weeksite also has been identified from eight other localities in Pennsylvania, Wyoming, California, New Mexico, Mexico, Arizona, and Texas...
Journal Article
Published: 01 April 1992
American Mineralogist (1992) 77 (3-4): 431–437.
...Eric P. Plesko; Barry E. Scheetz; William B. White Abstract Synthesis studies in the system K 2 O-UO 3 -SiO 2 -H 2 O are presented as an isothermal isobaric projection through the system at 300°C and 30 MPa. In addition to the compatibility relationships for weeksite, boltwoodite, and soddyite...
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Illustration of the twinning in <span class="search-highlight">weeksite</span> (red and blue net) in reciprocal s...
Published: 01 April 2012
Figure 1 Illustration of the twinning in weeksite (red and blue net) in reciprocal space viewed along b*. Reciprocal unit-cell choice by Jackson and Burns (2001) is sketched in green. Reconstruction is based on the experimental data set. (Color online.)
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Thermal decomposition of <span class="search-highlight">weeksite</span> reflected in weight-loss loss (TG) and it...
Published: 01 April 2012
Figure 2 Thermal decomposition of weeksite reflected in weight-loss loss (TG) and it is difference curve (DTG).
Image
Polyhedral representation of <span class="search-highlight">weeksite</span> structure viewed along [001] with lab...
Published: 01 April 2012
Figure 3 Polyhedral representation of weeksite structure viewed along [001] with labeled M-sites in the interlayer. Uranyl pentagonal bipyramids are yellow, silicate tetrahedra are red; atoms related to M-sites are green and oxygen atoms are red. The unit-cell edges are outlined. (Color online.)
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MISCELLANEOUS INFORMATION CONCERNING <span class="search-highlight">WEEKSITE</span>
Published: 01 February 2001
TABLE 1. MISCELLANEOUS INFORMATION CONCERNING WEEKSITE
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FINAL ATOMIC PARAMETERS FOR <span class="search-highlight">WEEKSITE</span>
Published: 01 February 2001
TABLE 2. FINAL ATOMIC PARAMETERS FOR WEEKSITE
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ANISOTROPIC DISPLACEMENT PARAMETERS FOR <span class="search-highlight">WEEKSITE</span>
Published: 01 February 2001
TABLE 3. ANISOTROPIC DISPLACEMENT PARAMETERS FOR WEEKSITE
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SELECTED INTERATOMIC DISTANCES (Å) AND ANGLES (°) FOR <span class="search-highlight">WEEKSITE</span>
Published: 01 February 2001
TABLE 4. SELECTED INTERATOMIC DISTANCES (Å) AND ANGLES (°) FOR WEEKSITE
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Polyhedral representation of the structure of <span class="search-highlight">weeksite</span> projected along [100...
Published: 01 February 2001
F ig . 1. Polyhedral representation of the structure of weeksite projected along [100]. The silicate tetrahedra are shown in red, the uranyl polyhedra are shown in yellow, purple spheres represent M sites ( M : K, Ca and Ba), and bluish gray spheres represent the two symmetrically distinct H 2
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Polyhedral representation of the uranyl silicate layer in <span class="search-highlight">weeksite</span> (a). Cha...
Published: 01 February 2001
F ig . 3. Polyhedral representation of the uranyl silicate layer in weeksite (a). Chains of silicate tetrahedra that show split sites are indicated by arrows along [100] in (a). The chain shown in (b) contains split Si sites that arise from the occurrence of the orientations shown in (c) and (d
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COMPOSITION OF <span class="search-highlight">WEEKSITE</span>, AS DETERMINED BY ELECTION-MICROPROBE ANALYSIS
Published: 01 February 2001
TABLE 5. COMPOSITION OF WEEKSITE, AS DETERMINED BY ELECTION-MICROPROBE ANALYSIS
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PROPOSED CATION ASSIGNMENTS FOR THE  M  SITES IN <span class="search-highlight">WEEKSITE</span>
Published: 01 February 2001
TABLE 6. PROPOSED CATION ASSIGNMENTS FOR THE M SITES IN WEEKSITE
Journal Article
Published: 01 May 2004
American Mineralogist (2004) 89 (5-6): 721–724.
..., Galiléia Co., Minas Gerais, Brazil. Coutinhoite is intimately associated with weeksite, phosphuranylite, meta-uranocircite, and uranocircite on muscovite and microcline. The mineral forms irregular aggregates with very small curved scales, flaky crystals, up to 10 μm long and with a thickness up to about...
FIGURES
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Polyhedral representation of the uranyl silicate layer that occurs in weeks...
Published: 01 February 2001
F ig . 2. Polyhedral representation of the uranyl silicate layer that occurs in weeksite, projected along [010]. Legend as in Figure 1 .
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Polyhedral representation of the six-membered rings of silicate tetrahedra ...
Published: 01 February 2001
F ig . 4. Polyhedral representation of the six-membered rings of silicate tetrahedra that occur in weeksite, with the location of H 2 O(28) (gray spheres) in the plane of the rings. Legend as in Figure 1 .
Journal Article
Published: 01 February 2004
American Mineralogist (2004) 89 (2-3): 339–347.
... honors geologist and conservationist Reginald Claude Sprigg (1919–1994), founder of the Arkaroola Tourist Station. Together with beta-uranophane, soddyite, kasolite, Ce-rich francoisite-(Nd), metatorbernite, billietite, Ba-bearing boltwoodite, schoepite, metaschoepite, and weeksite, spriggite results...
FIGURES | View All (6)
Journal Article
Journal: Economic Geology
Published: 01 April 1991
Economic Geology (1991) 86 (2): 233–248.
... association are observed) and the associated kaolinization of the rock are related to the circulation of hydrothermal fluids in breccias and fault systems. The present-day mineralization consists of mainly U (super +6) minerals (uranophane, weeksite, etc.) produced during later stages under oxidized...