1-20 OF 103 RESULTS FOR

krupkaite

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 April 2008
The Canadian Mineralogist (2008) 46 (2): 525–539.
...Dan Topa; Václav Petřiček; Michal Dušek; Emil Makovicky; Tonči Balić-Žunić Abstract Crystal structures of intergrown lindströmite and krupkaite were determined in two distinct samples by a simultaneous crystal-structure refinement using a modified jana program package. The exsolution...
FIGURES
First thumbnail for: SIMULTANEOUS REFINEMENT OF TWO COMPONENTS OF AN EX...
Second thumbnail for: SIMULTANEOUS REFINEMENT OF TWO COMPONENTS OF AN EX...
Third thumbnail for: SIMULTANEOUS REFINEMENT OF TWO COMPONENTS OF AN EX...
Journal Article
Published: 01 August 2002
The Canadian Mineralogist (2002) 40 (4): 1147–1159.
...Dan Topa; Emil Makovicky; Tonči Balić-Žunić Abstract Crystal structures of stoichiometric gladite (empirical formula Cu 1.32 Pb 1.37 Bi 6.65 S 12.03 ) and krupkaite (empirical formula Cu 2.00 Pb 2.03 Bi 5.99 S 12.04 ) from Felbertal, Austria, were refined to R 1 = 0.045 and 0.037, respectively...
FIGURES
First thumbnail for: THE STRUCTURAL ROLE OF EXCESS Cu AND Pb IN GLADITE...
Second thumbnail for: THE STRUCTURAL ROLE OF EXCESS Cu AND Pb IN GLADITE...
Third thumbnail for: THE STRUCTURAL ROLE OF EXCESS Cu AND Pb IN GLADITE...
Journal Article
Published: 01 February 1989
American Mineralogist (1989) 74 (1-2): 250–255.
...Allan Pring Abstract The nature of compositional fields in aikinite and krupkaite has been investigated by electron diffraction and high‐resolution transmission electron microscopy. Variation from ideal composition in these minerals results from the disordered intergrowth of krupkaite units...
Journal Article
Published: 01 April 1975
American Mineralogist (1975) 60 (3-4): 300–308.
...W. G. Mumme Abstract Krupkaite, CuPbBi 3 S 6 , from the Juno Mine at Tennant Creek, Northern Territory, Australia, is orthorhombic, space group Pmc 2 1 with a = 4.003(3), b = 11.200(9), c = 11.560(9) Å. Diffraction data were recorded with an equi-inclination diffractometer equipped...
Image
Published: 01 April 2008
TABLE 8. CATION-ANION DISTANCES IN THE KRUPKAITE COMPONENT: COMPARISON WITH THE VALUES FOR PURE KRUPKAITE
Image
A. Kupčíkite (kup) in association with krupkaite (krp) replaced by emplectite (emp). B. Aggregates of paděraite laths (pad) replaced by hodrušite (hod) and emplectite (emp); the bright grain is gold (Au). C. Aggregates of laths of paděraite (pad), hodrušite (hod), emplectite (emp), kupčíkite (kup) and hammarite (ham). D. Kupčíkite (kup) in association with krupkaite (krp), replaced by emplectite (emp). E. Aikinite grains (aik) replaced by matildite (mat) and wittichenite (wit). F. Krupkaite grains (krp) replaced by aikinite (aik). G. Exsolution phenomena in dantopaite (6P). H. Krupkaite (krp) replaced by benjaminite (7P). Back-scattered electron images, Rozália vein, Rozália mine, Hodruša–Hámre.
Published: 01 April 2012
Fig. 2 A. Kupčíkite (kup) in association with krupkaite (krp) replaced by emplectite (emp). B. Aggregates of paděraite laths (pad) replaced by hodrušite (hod) and emplectite (emp); the bright grain is gold (Au). C. Aggregates of laths of paděraite (pad), hodrušite (hod), emplectite (emp
Image
Back scattered electron images showing skeletal intergrowths of krupkaite with gladite and makovickyite-bearing assemblages. (a) Area of nebulous ‘cloud’-like intergrowths (lighter grey) in krupkaite. Homogeneous gladite on left of picture hosts tetradymite. (b) Close-up of ‘cloud’-like intergrowths in b. (c) Skeletal intergrowths in krupkaite, next to makovickyite (dark grey). (d) Back-scattered image of a parquet-like intergrowth of a Cu-rich and Cu-poor makovickyite, associated with lindströmite (light grey) and chalcopyrite (black), with minor tetradymite (bright white).
Published: 01 July 2000
Fig. 2. Back scattered electron images showing skeletal intergrowths of krupkaite with gladite and makovickyite-bearing assemblages. (a) Area of nebulous ‘cloud’-like intergrowths (lighter grey) in krupkaite. Homogeneous gladite on left of picture hosts tetradymite. (b) Close-up of ‘cloud’-like
Image
(a) The crystal structure of oversubstituted gladite (naik = 39). (b) The crystal structure of oversubstituted krupkaite (naik = 59). The fully occupied Cu positions are indicated in red, the partly occupied ones (22% in gladite, 12% in krupkaite) in blue.
Published: 01 August 2002
F ig . 4. (a) The crystal structure of oversubstituted gladite ( n aik = 39). (b) The crystal structure of oversubstituted krupkaite ( n aik = 59). The fully occupied Cu positions are indicated in red, the partly occupied ones (22% in gladite, 12% in krupkaite) in blue.
Image
(a) The crystal structure of oversubstituted gladite (naik = 39). (b) The crystal structure of oversubstituted krupkaite (naik = 59). The fully occupied Cu positions are indicated in red, the partly occupied ones (22% in gladite, 12% in krupkaite) in blue.
Published: 01 August 2002
F ig . 4. (a) The crystal structure of oversubstituted gladite ( n aik = 39). (b) The crystal structure of oversubstituted krupkaite ( n aik = 59). The fully occupied Cu positions are indicated in red, the partly occupied ones (22% in gladite, 12% in krupkaite) in blue.
Journal Article
Published: 01 February 2002
The Canadian Mineralogist (2002) 40 (1): 239–245.
... of the bismuthinite – krupkaite – aikinite solid-solution series. A refinement of the crystal structure was made with single-crystal measurements, which included 2943 observed unique reflections (I > 2σ I ) and resulted in R 1 = 6.6% ( R W = 22.4%). The crystal structure is composed of a fairly complex sequence...
FIGURES
First thumbnail for: THE CRYSTAL STRUCTURE OF EMILITE, Cu 10.7 Pb 10.7 ...
Second thumbnail for: THE CRYSTAL STRUCTURE OF EMILITE, Cu 10.7 Pb 10.7 ...
Third thumbnail for: THE CRYSTAL STRUCTURE OF EMILITE, Cu 10.7 Pb 10.7 ...
Image
a. A lamella of copper-oversubstituted gladite (bd39) (the subscript indicates the naik value, explained in the caption to Table 2) with incipient exsolution; above it is a large crystal of salzburgite (bd40) with lamellae of krupkaite (bd48). Grains of native bismuth, Bi telluride and gustavite are indicated. b. Above: a crystal of salzburgite (bd41) with several exsolution-induced lamellae; below: exsolution intergrowth of oversubstituted gladite (bd37) with salzburgite (bd40). A replacement intergrowth of Ag-poor cannizzarite (ca0.6) and cupro-plumbian bismuthinite (bd9) developed at the grain junction. c. A mosaic of large grains of a low-Cu bismuthinite derivative, decomposed into an intergrowth of paarite (bd42) and krupkaite (bd49). Replacement aggregates composed of cupro-plumbian bismuthinite (light grey) and cannizzarite (white) are developed along grain boundaries. d. Graphic intergrowth of cannizzarite (ca2.6) and bismuthinite developed between grains of a bismuthinite derivative, exsolved into paarite (bd42) – krupkaite (bd49) intergrowths. Note the substantial lamellae of krupkaite close to the boundary of the light-colored, low-Cu intergrowth, indicating a Bi-rich zone predating the exsolution. a–d: Back-scattered electron images, material from Felbertal, Austria.
Published: 01 June 2005
F ig . 4. a. A lamella of copper-oversubstituted gladite (bd 39 ) (the subscript indicates the n aik value, explained in the caption to Table 2 ) with incipient exsolution; above it is a large crystal of salzburgite (bd 40 ) with lamellae of krupkaite (bd 48 ). Grains of native bismuth, Bi
Journal Article
Published: 01 October 2001
The Canadian Mineralogist (2001) 39 (5): 1377–1382.
... cell of this “fivefold derivative” contains two “bismuthinite-like” Bi 4 S 6 ribbons and eight “krupkaite-like” CuPbBi 3 S 6 ribbons. The fully occupied Cu sites occur in zigzag [001] rows at y = 0.15, 0.30, 0.70 and 0.85, comprising gladite-like and krupkaite-like intervals in the structure in regular...
FIGURES
First thumbnail for: THE CRYSTAL STRUCTURE OF PAARITE, THE NEWLY DISCOV...
Second thumbnail for: THE CRYSTAL STRUCTURE OF PAARITE, THE NEWLY DISCOV...
Third thumbnail for: THE CRYSTAL STRUCTURE OF PAARITE, THE NEWLY DISCOV...
Journal Article
Published: 01 December 1995
American Mineralogist (1995) 80 (11-12): 1166–1173.
... variation within the annealed products. HRTEM was used to monitor Cu ordering and revealed that the distribution of Cu and Pb in the cell is not that of hammarite but of a lower symmetry supercell consisting of the intergrowth of one aikinite cell (two aikinite units) with two krupkaite cells (four...
Journal Article
Published: 01 February 1976
American Mineralogist (1976) 61 (1-2): 15–20.
..., 1974) has established CuPbBi 3 S 6 as a distinct species, to which the name krupkaite has been given. The Z n principle (Moore, 1967) proposed for classification of bismuthinite derivatives has not been followed by the crystal structures found for krupkaite, CuPbBi 3 S 6 , and pekoite, CuPbBi 11 S 18...
Image
Photomicrographs demonstrating sulfosalt-telluride-native element relationships in Stanos mineralization (a) Pyrite (Py) surrounded by an intergrowth of gladite, krupkaite, bismuthinite (Bmt) and unnamed CuPbBi7S12. Native bismuth and quartz are also present (sample B, reflected light); (b) Intergrowth of gladite, krupkaite and salzburgite-gladite surrounding pyrite (sample B, reflected light); (c) unnamed CuPbBi7S12, krupkaite, lillianite-gustavite and chalcopyrite, postdating pyrite (sample G, reflected light); (d) Paarite (Prt), gladite-salzburgite (Gld-Sal), krupkaite, gladite-pekoite (Gld-Pek) and chalcopyrite replacing cosalite. Quartz is the gangue mineral (sample G, reflected light); (e) Complex intergrowth between salzburgite-gladite, krupkaite, gladite-salzburgite, matildite, native bismuth, cosalite and lillianite-gustavite within chalcopyrite (sample D, reflected light); (f) Intergrowth of phases along the matildite-galena joint (Mtd-Gn) with matildite, native bismuth and late chalcopyrite postdating pyrite. Quartz is the gangue mineral (sample H, reflected light); (g) Lillianite-gustavite associated with joséite-A and chalcopyrite postdates pyrite (sample E, reflected light); (h) Pb-rich ikunolite (Pb-Ik) isolated in quartz. Chalcopyrite rims arsenopyrite (sample I, reflected light); (i) Unnamed (Bi,Pb)4TeS 3, lillianite-gustavite, bismuthinite and chalcopyrite isolated in quartz. Native bismuth is also present (sample I, reflected light); (j) Lillianite-gustavite, intergrown with native gold (Au), Pb-rich joséite-A and chalcopyrite postdating pyrite (sample E, reflected light); (k) Native gold in contact with native bismuth. Lillianite-gustavite, galena, chalcopyrite, pyrite and quartz are also present (sample G, SEM-BSE image); (l) Native bismuth and galena replace lillianite-gustavite and native gold. Chalcopyrite and pyrite are present (sample G, SEM-BSE image).
Published: 01 February 2013
Fig. 4 Photomicrographs demonstrating sulfosalt-telluride-native element relationships in Stanos mineralization (a) Pyrite (Py) surrounded by an intergrowth of gladite, krupkaite, bismuthinite (Bmt) and unnamed CuPbBi 7 S 12 . Native bismuth and quartz are also present (sample B, reflected light
Image
Published: 01 August 2002
TABLE 6. POLYHEDRON CHARACTERISTICS FOR THE KRUPKAITE STRUCTURES REFINED
Journal Article
Published: 01 December 2001
The Canadian Mineralogist (2001) 39 (6): 1641–1652.
.... , bismuthinite ribbons, krupkaite ribbons and aikinite ribbons, could occur in the progressive exsolution or precipitation of a single phase in the bismuthinite–aikinite series. The exceptionally high contents of Ag (0.76–1.27 wt%) in the phase Cu 0.83 Ag 0.10 Pb 0.90 Bi 3.13 S 6 , presumably corresponding...
FIGURES
First thumbnail for: FELBERTALITE AND RELATED BISMUTH SULFOSALTS FROM T...
Second thumbnail for: FELBERTALITE AND RELATED BISMUTH SULFOSALTS FROM T...
Third thumbnail for: FELBERTALITE AND RELATED BISMUTH SULFOSALTS FROM T...
Journal Article
Published: 01 July 2000
European Journal of Mineralogy (2000) 12 (4): 899–917.
...Fig. 2. Back scattered electron images showing skeletal intergrowths of krupkaite with gladite and makovickyite-bearing assemblages. (a) Area of nebulous ‘cloud’-like intergrowths (lighter grey) in krupkaite. Homogeneous gladite on left of picture hosts tetradymite. (b) Close-up of ‘cloud’-like...
FIGURES
First thumbnail for: Intergrowths of bismuth sulphosalts from the Ocna ...
Second thumbnail for: Intergrowths of bismuth sulphosalts from the Ocna ...
Third thumbnail for: Intergrowths of bismuth sulphosalts from the Ocna ...
Image
Published: 01 April 2008
TABLE 2. LINDSTRÖMITE-KRUPKAITE INTERGROWTHS: EXPERIMENTAL AND REFINEMENT DATA
Image
Published: 01 April 2008
TABLE 6. ANISOTROPIC DISPLACEMENT PARAMETERS OF ATOMS IN THE KRUPKAITE COMPONENT OF: