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Llallagua

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Journal Article
Published: 01 April 2016
Mineralogical Magazine (2016) 80 (2): 311–324.
...G. Raade; J. D. Grice; R. Rowe Abstract Ferrivauxite, ideally Fe 3+ Al 2 (PO 4 ) 2 (OH) 3 ·5H 2 O, is an oxidized equivalent of vauxite, Fe 2+ Al 2 (PO 4 ) 2 (OH) 2 ·6H 2 O, and forms oxidation pseudomorphs after that mineral. It occurs in association with sigloite and crandallite at the Llallagua...
FIGURES
Journal Article
Published: 01 January 2016
The Canadian Mineralogist (2016) 54 (1): 163–176.
...Gennaro Ventruti; Emanuela Schingaro; Alessandro Monno; Maria Lacalamita; Giancarlo Della Ventura; Fabio Bellatreccia; Corrado Cuocci; Manuela Rossi; Francesco Capitelli Abstract A crystal-chemical investigation of vauxite, ideally FeAl 2 (PO 4 ) 2 (OH) 2 ·6H 2 O, from Llallagua (Bolivia) has been...
FIGURES | View All (8)
Journal Article
Published: 01 May 2001
American Mineralogist (2001) 86 (5-6): 697–700.
...John Rakovan; Matthew Newville; Steve Sutton Abstract Eu L 3 X-ray absorption near edge structure (XANES) spectroscopy was conducted with a wavelength dispersive (WDS) spectrometer to determine the valence state of europium in a natural, Mn-and REE-rich apatite from Llallagua, Bolivia. Europium...
FIGURES
Journal Article
Published: 01 February 1962
American Mineralogist (1962) 47 (1-2): 1–8.
...Cornelius S. Hurlbut, Jr.; Russell Honea Abstract Sigloite, (Fe 3+ , Fe 2+ )A1 2 (P0 4 ) 2 (0,0H)-8H 2 O, is a new mineral formed as an oxidation pseudomorph after paravauxite at Llallagua, Bolivia. Triclinic; a =5.26, b =10.52, c =7.06 Å, α=106°58’, β= 111°30’, ϒ=69°30’; a:b:c =0.4990:l:0.6711...
Journal Article
Published: 01 December 1957
The Canadian Mineralogist (1957) 6 (1): 128–135.
...F. G. Smith; S. K. DasGupta; V. G. Hill "'Wurtzite' from Llallagua, Bolivia, is a mixture of polytypes but a 2H structure is present which is shown by syntheses and x-ray diffraction to have the composition (Zn (sub 0.43) Mn (sub 0.31) Fe (sub 0.26) )S within about 5 percent uncertainty...
Journal Article
Published: 01 December 1957
The Canadian Mineralogist (1957) 6 (1): 136–139.
...M. J. Mloszewski; A. K. Saha; E. W. Nuffield The x-ray powder data for wurtzite from Llallagua, Bolivia, reported by Smith and others are here supplemented by single crystal data. Both the cell dimensions obtained, a = 3.881 and c = 6.315 A, which are larger than for ordinary wurtzite...
Journal Article
Journal: Economic Geology
Published: 01 March 1936
Economic Geology (1936) 31 (2): 219–221.
Journal Article
Journal: Economic Geology
Published: 01 March 1935
Economic Geology (1935) 30 (2): 170–190.
Journal Article
Journal: Economic Geology
Published: 01 January 1935
Economic Geology (1935) 30 (1): 14–60.
Journal Article
Journal: Economic Geology
Published: 01 August 1934
Economic Geology (1934) 29 (5): 481–499.
Journal Article
Journal: Economic Geology
Published: 01 May 1931
Economic Geology (1931) 26 (3): 241–257.
Journal Article
Published: 01 May 1938
American Mineralogist (1938) 23 (5): 314–328.
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SEM-BSE images of unreacted grains used in experiments. ( a ) Synthetic flu...
Published: 01 December 2016
Figure 1 SEM-BSE images of unreacted grains used in experiments. ( a ) Synthetic fluorapatite (FAp). ( b ) Llallagua fluorapatite with weakly visible zoning pattern. ( c ) Llallagua monazite (Mnz). ( d ) Synthetic monazite.
Journal Article
Journal: Economic Geology
Published: 01 August 1975
Economic Geology (1975) 70 (5): 913–927.
..., including those at the major Llallagua, Potosi, Oruro, and Chorolque mineralized centers, geological characteristics of which are summarized, contain stockwork, disseminated, and breccia-filling cassiterite mineralization. The deposits are designated as porphyry tin deposits, a name considered to possess...
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Solubility of <span class="search-highlight">Llallagua</span> monazite in 2 N NaOH solution represented as wt% mo...
Published: 01 March 2018
Figure 2. Solubility of Llallagua monazite in 2 N NaOH solution represented as wt% monazite dissolved in the fluid (wt. loss of crystal/wt. of fluid ×100). Solubilites increase at oxygen fugacities above the FMQ buffer. The x-axis represents the difference in log units from the FMQ equilibrium
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CRYSTAL DATA AND STRUCTURE REFINEMENT FOR VAUXITE FROM <span class="search-highlight">LLALLAGUA</span>, BOLIVIA
Published: 01 January 2016
TABLE 1. CRYSTAL DATA AND STRUCTURE REFINEMENT FOR VAUXITE FROM LLALLAGUA, BOLIVIA
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BOND LENGTHS (Å) AND SELECTED ANGLES (°) FOR VAUXITE FROM <span class="search-highlight">LLALLAGUA</span>, BOLIVI...
Published: 01 January 2016
TABLE 3. BOND LENGTHS (Å) AND SELECTED ANGLES (°) FOR VAUXITE FROM LLALLAGUA, BOLIVIA
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HYDROGEN BONDS (Å,°) FOR VAUXITE FROM <span class="search-highlight">LLALLAGUA</span>, BOLIVIA
Published: 01 January 2016
TABLE 4. HYDROGEN BONDS (Å,°) FOR VAUXITE FROM LLALLAGUA, BOLIVIA
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Powder FTIR (a) and Raman (b) spectra of the studied vauxite from <span class="search-highlight">Llallagua</span>...
Published: 01 January 2016
Fig. 6. Powder FTIR (a) and Raman (b) spectra of the studied vauxite from Llallagua in the (3800–2400 cm −1 ) H 2 O stretching region; inset: Raman broad absorption, with maxima at 3405 and 3160 cm −1 .
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Single-crystal FTIR spectrum of the studied vauxite from <span class="search-highlight">Llallagua</span> in the N...
Published: 01 January 2016
Fig. 7. Single-crystal FTIR spectrum of the studied vauxite from Llallagua in the NIR (6000–4000 cm −1 ) region.