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lautite

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Journal Article
Published: 01 November 1978
The Canadian Mineralogist (1978) 16 (4): 665–669.
Journal Article
Published: 01 August 1999
European Journal of Mineralogy (1999) 11 (4): 709–719.
...Daniel E. Harlov Abstract Experimental Ag-Cu exchange equilibria (evacuated silica tubes; variable mass ratio) involving proustite (Ag,Cu) 3 AsS 3 , smithite AgAsS 2 , pearceite (Ag,Cu) 16 As 2 S 11 , lautite CuAsS, and sinnerite Cu 6 As 4 S 9 are reported over the temperature range 150-350 degrees...
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(a) The ternary diagram for Cu-As(Sb)-S phases and the location for tennantite-tetrahedrite, zhonghongite and watanabeite. (b) The variation range of As and Sb contents for intergrown watanabeite, zhonghongite and tetrahedrite. Enr/luz-Fmt = enargite/luzonite-famatinite; Tn-Td = tennantite-tetrahedrite; Sin = sinnerite; Wa = watanabeite; Ski = skinneite; Zhh = zhonghongite; Chst = chalcostibite; Lt = lautite. (Color online.)
Published: 01 February 2025
 = tennantite-tetrahedrite; Sin = sinnerite; Wa = watanabeite; Ski = skinneite; Zhh = zhonghongite; Chst = chalcostibite; Lt = lautite. (Color online.)
Journal Article
Journal: Economic Geology
Published: 01 October 1971
Economic Geology (1971) 66 (6): 901–918.
...Siegfried Maske; Brian J. Skinner Abstract Ternary phases in the system Cu-As-S are luzonite, enargite, tennantite, lautite (CuAsS), sinnerite (Cu 6 As 4 S 9 ) and a new compound A (Cu 24 As 12 S 31 ). The only compound to have an extensive composition field is tennantite, for which the generalized...
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Photographic, SEM, and EDS data from Facies I, saturated sediment below the sediment-water interface from the lake. (a) Image of the saturated sediment displaying the dark olive color. (b) BSED-SEM image of a high-backscatter grain surrounded by diatom frustules that were the dominant phase in the sediment. (c) EDS spectra of the high-backscatter grain composed of As-Cu-S. Possible minerals include tennantite, luzonite, enargite, lautite, or sinnerite.
Published: 30 November 2017
phase in the sediment. (c) EDS spectra of the high-backscatter grain composed of As-Cu-S. Possible minerals include tennantite, luzonite, enargite, lautite, or sinnerite.
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(a) Cubanite CuFe2S3 (McCammon et al. 1992). small spheres: Cu (light) and Fe (dark), solid tetrahedra: Fe. Note the edge-sharing of Fe tetrahedra. b axis is horizontal, c axis vertical. Slabs (010) of wurtzite-like arrangement are centered on the planes of Cu tetrahedra. (b) Catamarcaite Cu6GeWS8 (Putz et al. 2005). Grey tetrahedrally coordinated cations: Cu, black ones: Ge. Solid interstitial tetrahedra: W. (c) CdGa2S4 (Gastaldi et al. 1985). Gallium – solid tetrahedra of two kinds; Cd – grey spheres. (d) Lautite CuAsS (Craig and Sephenson 1965). Coordination tetrahedra of copper; anions: S - white spheres, As – black spheres. Covalent As-As bonds (dark).
Published: 01 January 2006
) Catamarcaite Cu 6 GeWS 8 (Putz et al. 2005). Grey tetrahedrally coordinated cations: Cu, black ones: Ge. Solid interstitial tetrahedra: W. (c) CdGa 2 S 4 ( Gastaldi et al. 1985 ). Gallium – solid tetrahedra of two kinds; Cd – grey spheres. (d) Lautite CuAsS (Craig and Sephenson 1965). Coordination tetrahedra
Journal Article
Published: 04 March 2024
Mineralogical Magazine (2024) 88 (3): 218–227.
.... , Catelani T. , Chelazzi L. and Bonazzi P. ( 2008 ) Reinvestigation of the crystal structure of lautite, CuAsS . Acta Crystallographica , E64 , i22...
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Phase diagrams for the Ag2S-Cu2S-AgSbS2-CuSbS2 and Ag2S-Cu2S-AgAsS2-CuAsS2 quadrilaterals of the systems Ag2S-Cu2S-Sb2S3 and Ag2S-Cu2S-As2S3 at 150, 200, 250, 300, and 350 °C (a-e) and mineral index (f). Mineral abbreviations: stephanite (st), ~(Ag,Cu)5SbS4; lautite (lt), ~ (Cu,Ag)AsS; tennantite (tnn), ~ (Cu,Ag)12+xAs4+yS13; phase A (A), ~ (Cu,Ag)24As12S30; sinnerite (sin), ~ (Cu,Ag)6As4S9; smithite (smt) ~ (Ag,Cu)AsS2; trechmannite (tmt), ~ (Ag,Cu)AsS2; arsenostephanite (As-st), ~ (Ag,Cu)5AsS4. [Used by permission of Elsevier Ltd, from Harlov and Sack (1995b), Geochim Cosmochim Acta, Vol. 59, Fig. 2, p. 4353.]
Published: 01 January 2006
) 5 SbS 4 ; lautite ( lt ), ~ (Cu,Ag)AsS; tennantite ( tnn ), ~ (Cu,Ag) 12+x As 4+y S 13 ; phase A ( A ), ~ (Cu,Ag) 24 As 12 S 30 ; sinnerite ( sin ), ~ (Cu,Ag) 6 As 4 S 9 ; smithite ( smt ) ~ (Ag,Cu)AsS 2 ; trechmannite (tmt), ~ (Ag,Cu)AsS 2 ; arsenostephanite ( As-st ), ~ (Ag,Cu) 5 AsS 4 . [Used
Journal Article
Published: 01 February 2025
American Mineralogist (2025) 110 (2): 312–318.
... = tennantite-tetrahedrite; Sin = sinnerite; Wa = watanabeite; Ski = skinneite; Zhh = zhonghongite; Chst = chalcostibite; Lt = lautite. (Color online.) ...
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Phase relations amongst As-bearing sulfosalts. (A) The system As–S (modified from Massalski et al. 1990). (B) The system As2S3–PbS (modified from Kutolglu 1969). Here it is instructive to consider the effect of melting of a small proportion of arsenopyrite (to produce As–S melt) in the presence of galena. Symbols: Srt: sartorite, Bmh: baumhauerite, Rth: rathite, Duf: dufrenoysite, Jrd: jordanite. (C) The system As–Pb–S at 550°C [constructed from information in Roland (1968) and Massalski et al.(1990)] (D) The system As2S3–PbS–Bi2S3 (after Walia & Chang 1973). (E) The system Cu–As–S (modified from Maske & Skinner 1971), showing the distribution of mineral phases and melt at 300°C, and the distribution of melt at 500°C, 600°C and 665.5°C. Symbols: Cv: covellite, En: enargite, A: unnamed compound, S: sinnerite, Lt: lautite, Dom: domeykite, fcc: face-centered cubic, hcp: hexagonal-closest packed. (F) The system As2S3–Sb2S3–Tl2S (modified from Sobott 1984) showing phase distribution at 315°C (at 1 bar). The lightly shaded region represents the extent of the liquid field at 275°C.
Published: 01 October 2006
1973 ). (E) The system Cu–As–S (modified from Maske & Skinner 1971 ), showing the distribution of mineral phases and melt at 300°C, and the distribution of melt at 500°C, 600°C and 665.5°C. Symbols: Cv: covellite, En: enargite, A: unnamed compound, S: sinnerite, Lt: lautite, Dom: domeykite, fcc
Journal Article
Published: 01 December 2013
Mineralogical Magazine (2013) 77 (8): 3105–3112.
... a ‘pyramidal’ coordination with two S and one As. The values observed for the As–As bonds are in keeping with that observed in lautite ( Bindi et al. , 2008 ) and those typically observed in As–S molecular compounds (e.g. dimorphite, realgar, uzonite; Bonazzi and Bindi, 2008 ). Table 5 shows the X-ray...
FIGURES
Journal Article
Published: 30 November 2017
The Canadian Mineralogist (2017) 55 (6): 1009–1025.
... phase in the sediment. (c) EDS spectra of the high-backscatter grain composed of As-Cu-S. Possible minerals include tennantite, luzonite, enargite, lautite, or sinnerite. ...
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Journal Article
Published: 01 December 2014
European Journal of Mineralogy (2014) 26 (6): 703–710.
... compounds with equal proportions (such as CuAsS - lautite) have InfEnt = 1.099, and so on. Whatever the number of elements in a formula, the InfEnt is highest for elements in equal proportions, and it drops as the proportions deviate from equality. In addition to the features of the Qual functions...
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Journal Article
Published: 01 December 2013
The Canadian Mineralogist (2013) 51 (6): 851–860.
... 60 , 998 – 1012 . Marumo F. Nowacki W. ( 1964 ) The crystal structure of lautite and of sinnerite, a new mineral from the Lengenbach Quarry . Schweizer Mineralogische und Petrographische Mitteilungen 44 , 440 – 454 . Maske S. Skinner B.J. ( 1971 ) Studies...
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Journal Article
Published: 01 October 2015
Mineralogical Magazine (2015) 79 (5): 1099–1109.
... species of thallium sulfosalt from Lengenbach, Switzerland . The Canadian Mineralogist , 44 , 141 – 158 . Belendorff K. ( 1986 ) A paragenesis of rare minerals from Nieder-Beerbach, Odenwald, Germany: Lautite, kutinaite, paxite . Neues Jahrbuch für Mineralogie, Monatshefte , 11...
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Image
Published: 01 September 2004
. A = unnamed compound, Cv = covellite, Dom = domeykite, En = enargite, fcc = face centered cubic, hcp = hexagonal closet packed, Lt = lautite, S = sinnerite. J. Liquidus surface map of the system Fe-Sb-S (after Barton, 1971 ). All of the fields in the detail to the right are + L 2 . Note that there is only
Journal Article
Published: 01 October 2006
The Canadian Mineralogist (2006) 44 (5): 1045–1062.
... 1973 ). (E) The system Cu–As–S (modified from Maske & Skinner 1971 ), showing the distribution of mineral phases and melt at 300°C, and the distribution of melt at 500°C, 600°C and 665.5°C. Symbols: Cv: covellite, En: enargite, A: unnamed compound, S: sinnerite, Lt: lautite, Dom: domeykite, fcc...
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Journal Article
Published: 08 December 2023
Geochemistry: Exploration, Environment, Analysis (2023) 23 (4): geochem2023-035.
... sulfides are the gersdorffite–cobaltite solid solution series ( Piestrzyński 2007 ). Accessory Co and/or Ni minerals include Co–Ni disulfides, rammelsbergite, nickeline, linneite, siegenite, carrolite, skutterudite and lautite ( Speczik and Wojciechowski 1997 ; Speczik et al. 1997 ; Kucha 2007...
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Journal Article
Journal: Economic Geology
Published: 01 September 2004
Economic Geology (2004) 99 (6): 1063–1084.
.... A = unnamed compound, Cv = covellite, Dom = domeykite, En = enargite, fcc = face centered cubic, hcp = hexagonal closet packed, Lt = lautite, S = sinnerite. J. Liquidus surface map of the system Fe-Sb-S (after Barton, 1971 ). All of the fields in the detail to the right are + L 2 . Note that there is only...
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Journal Article
Published: 01 January 2006
Reviews in Mineralogy and Geochemistry (2006) 61 (1): 7–125.
...) Catamarcaite Cu 6 GeWS 8 (Putz et al. 2005). Grey tetrahedrally coordinated cations: Cu, black ones: Ge. Solid interstitial tetrahedra: W. (c) CdGa 2 S 4 ( Gastaldi et al. 1985 ). Gallium – solid tetrahedra of two kinds; Cd – grey spheres. (d) Lautite CuAsS (Craig and Sephenson 1965). Coordination tetrahedra...
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