1-20 OF 46 RESULTS FOR

liebigite

Results shown limited to content with bounding coordinates.
Follow your search
Access your saved searches in your account

Would you like to receive an alert when new items match your search?
Close Modal
Sort by
Journal Article
Published: 01 September 1994
The Canadian Mineralogist (1994) 32 (3): 553–561.
Journal Article
Published: 01 March 1993
The Canadian Mineralogist (1993) 31 (1): 167–171.
Journal Article
Published: 01 April 1950
American Mineralogist (1950) 35 (3-4): 251–254.
...Howard T. Evans, Jr.; Clifford Frondel Abstract Liebigite, Ca 2 U(CO 3 ) 4 · 10H 2 O, from Joachimsthal, Bohemia, has a 0 16.71 Å, b 0 17.55, c 0 13.79; a 0 : b 0 : c 0 = 0.952:1:0.786 ( a:b:c = 0.9539:1:0.7826, morphology, Brezina, 1890). Space group Bbam or Bba. Cell contents 8[Ca 2 U(CO 3 ) 4...
Journal Article
Published: 01 July 1917
American Mineralogist (1917) 2 (7): 87.
...Esper S. Larsen Abstract The available descriptions of uranothallite and liebigite indicate them to be very similar, except in chemical composition. Three fairly satisfactory analyses of uranothallite are available and the composition must be near 2CaO.UO 3 .3CO 2 .10H 2 O. The only published...
Journal Article
Published: 01 December 2004
The Canadian Mineralogist (2004) 42 (6): 1683–1697.
... and schoepite. Uranyl tricarbonate minerals such as liebigite precipitate on calcite only in more highly concentrated basic solutions. The crystal morphologies of almost all of these minerals were recorded on the calcite surface with an atomic force microscope (AFM). Red crystals of becquerelite grown in acidic...
FIGURES | View All (4)
Image
Heteropolyhedral layer in the structure of liebigite viewed down [010]. The unit cell is outlined with dashed lines.
Published: 27 July 2020
Fig. 9. Heteropolyhedral layer in the structure of liebigite viewed down [010]. The unit cell is outlined with dashed lines.
Image
The structures of markeyite and liebigite viewed parallel to the heteropolyhedral layers. UO8 hexagonal bipyramids are dark blue, CO3 triangles are yellow and Ca–O polyhedra are light blue; O atoms of isolated H2O groups are white balls. Unit cell outlines are shown as dashed black lines.
Published: 01 October 2018
Fig. 7. The structures of markeyite and liebigite viewed parallel to the heteropolyhedral layers. UO 8 hexagonal bipyramids are dark blue, CO 3 triangles are yellow and Ca–O polyhedra are light blue; O atoms of isolated H 2 O groups are white balls. Unit cell outlines are shown as dashed black
Image
Published: 13 December 2021
Table 6. Information measures ( I G ) for markeyite, natromarkeyite, pseudomarkeyite, paramarkeyite and liebigite including H atoms. Mineral V v I G I G,total (Å 3 ) (Å) (bits/atom) (bits/cell) Markeyite 3356 340 5.83 1983.19 Natromarkeyite 3346
Image
The U 4f7/2 spectra of liebigite, uranophane, uranophane-β, soddyite and metatorbernite. The peak assignments are provided in Figure 16A. The Figure is modified after Schindler et al. (2009a).
Published: 01 January 2014
Figure 16 The U 4 f 7/2 spectra of liebigite, uranophane, uranophane-β, soddyite and metatorbernite. The peak assignments are provided in Figure 16A. The Figure is modified after Schindler et al. (2009a) .
Image
EXAFS (left) and FT (right) spectra for (a) liebigite, (b) čejkaite, and (c) the aqueous complex \batchmode \documentclass[fleqn,10pt,legalpaper]{article} \usepackage{amssymb} \usepackage{amsfonts} \usepackage{amsmath} \pagestyle{empty} \begin{document} \(UO_{2}(CO_{3})_{3}^{4{-}}\) \end{document}. Solid lines represent experimental data; dashed lines represent fits. The FT features due to multiple scattering from bidentate carbonate groups are bracketed by the vertical dashed lines.
Published: 01 July 2004
F igure 2. EXAFS (left) and FT (right) spectra for ( a ) liebigite, ( b ) čejkaite, and ( c ) the aqueous complex \batchmode \documentclass[fleqn,10pt,legalpaper]{article} \usepackage{amssymb} \usepackage{amsfonts} \usepackage{amsmath} \pagestyle{empty} \begin{document} \(UO_{2}(CO_{3})_{3
Image
Images taken with a reflection microscope: (a) wyartite (violet) and becquerelite (red) formed under acidic conditions. (b) Uranyl-bearing calcite (brown), becquerelite (red), schoepite (yellow) and liebigite (green) formed under basic conditions. (c) Fine-grained precipitate of wyartite formed under basic conditions, with an oxidized yellow core that subsequently forms in air. (d) Becquerelite (red) with liebigite (green) formed under basic conditions.
Published: 01 December 2004
F ig . 3. Images taken with a reflection microscope: (a) wyartite (violet) and becquerelite (red) formed under acidic conditions. (b) Uranyl-bearing calcite (brown), becquerelite (red), schoepite (yellow) and liebigite (green) formed under basic conditions. (c) Fine-grained precipitate
Journal Article
Published: 01 February 2025
American Mineralogist (2025) 110 (2): 319–327.
.... In Beshtau, it occurs as yellow tabular crystals up to 0.3 mm grouped in crusts on a matrix composed of albite, microcline, quartz, and chamosite in association with liebigite, meta-autunite, and plumbogummite. The empirical formula calculated on the basis of 6 O apfu and 3 H 2 O is [ ( NH 4 ) 0.91 K 0.08...
FIGURES | View All (7)
Image
Published: 01 August 2004
TABLE 3. COMPARISON OF THE RELEVANT BANDS IN THE INFRARED SPECTRA OF SWARTZITE AND LIEBIGITE
Journal Article
Published: 01 October 2018
Mineralogical Magazine (2018) 82 (5): 1089–1100.
...Fig. 7. The structures of markeyite and liebigite viewed parallel to the heteropolyhedral layers. UO 8 hexagonal bipyramids are dark blue, CO 3 triangles are yellow and Ca–O polyhedra are light blue; O atoms of isolated H 2 O groups are white balls. Unit cell outlines are shown as dashed black...
FIGURES | View All (7)
Journal Article
Published: 01 March 1993
Jour. Geol. Soc. India (1993) 41 (3): 243–258.
... minerals including tyuyamunite, uranophane, bayleyite, andersonite, schoepite, liebigite, swarlzite, and schroeckingerite have been identified. Azurite and malachite are also associated in some of the uranium occurrences in Lower Siwaliks. The sedimentological, geochrmical, and tectonic attributes...
Journal Article
Published: 01 February 1951
American Mineralogist (1951) 36 (1-2): 1–22.
... are briefly considered. Of them, liebigite (= uranothallite) and schroeckingerite are well established. Voglite is almost certainly valid; randite certainly, and rutherfordine probably, are to be discredited; sharpite may be valid; the status of studtite and diderichite is very doubtful. * Published...
Journal Article
Published: 13 December 2021
Mineralogical Magazine (2022) 86 (1): 27–36.
...Table 6. Information measures ( I G ) for markeyite, natromarkeyite, pseudomarkeyite, paramarkeyite and liebigite including H atoms. Mineral V v I G I G,total (Å 3 ) (Å) (bits/atom) (bits/cell) Markeyite 3356 340 5.83 1983.19 Natromarkeyite 3346...
FIGURES | View All (6)
Journal Article
Published: 01 July 2004
American Mineralogist (2004) 89 (7): 1004–1021.
...F igure 2. EXAFS (left) and FT (right) spectra for ( a ) liebigite, ( b ) čejkaite, and ( c ) the aqueous complex \batchmode \documentclass[fleqn,10pt,legalpaper]{article} \usepackage{amssymb} \usepackage{amsfonts} \usepackage{amsmath} \pagestyle{empty} \begin{document} \(UO_{2}(CO_{3})_{3...
FIGURES | View All (9)
Journal Article
Published: 27 July 2020
Mineralogical Magazine (2020) 84 (5): 753–765.
...Fig. 9. Heteropolyhedral layer in the structure of liebigite viewed down [010]. The unit cell is outlined with dashed lines. ...
FIGURES | View All (9)
Journal Article
Journal: Geology
Published: 02 October 2017
Geology (2017) 45 (11): 1007–1010.
.... Ewingite forms aggregates of golden-yellow crystals as large as 0.2 mm in diameter on altered uraninite, and is associated with other uranyl carbonate minerals, including liebigite and metazellerite ( Fig. 1 ). Uranyl minerals, including ewingite, are typically various shades of yellow, green, and orange...
FIGURES