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schalenblende

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Journal Article
Published: 01 August 1977
The Canadian Mineralogist (1977) 15 (3): 303–308.
Image
Photomicrographs (plane-polarised light) of the sulphide mineralisation. (A...
Published: 01 September 2019
Fig. 4 Photomicrographs (plane-polarised light) of the sulphide mineralisation. (A) General view of the banded schalenblende spherulite cemented by colourless sphalerite and calcite (sample RN6483, TL). (B) Detailed view of banded sphalerite (sample RN6483, TL). (C): General view of banded
Journal Article
Journal: Economic Geology
Published: 01 February 1992
Economic Geology (1992) 87 (1): 113–124.
... in the Fe-Zn zone are characterized by an abundant complex intergrowth of sphalerite and wurtzite (schalenblende). X-ray analysis indicates that the wurtzite within the schalenblende inverted to sphalerite, thereby producing pseudomorphous sphalerite after wurtzite. Because wurtzite is the sulfur-deficient...
Journal Article
Journal: Economic Geology
Published: 01 August 2010
Economic Geology (2010) 105 (5): 1005–1023.
... morphology (−31.9‰; −31.8‰); both are associated with oxysulfides. Microglobular sphalerite with well-preserved sphalerite globules has a δ 34 S value of −28.8 to −28.2 per mil; colloform sphalerite (schalenblende) ranges from −29.0 to −25.0 per mil. Microglobular sphalerite associated with fine-grained...
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Image
Elementary composition of sphalerite. (A–C) Chemical mapping (Cd and Fe) by...
Published: 01 September 2019
Fig. 5 Elementary composition of sphalerite. (A–C) Chemical mapping (Cd and Fe) by EPMA of banded schalenblende spherulite with a pyrite inclusion in the core; note the first-order inverse correlation between Cd and Fe. (D and E) Elementary profiles, based on LA-ICPMS data, across banded
Image
F ig . 8. Photomicrographs showing textures in the sphalerite ores (transmi...
Published: 01 November 2003
F ig . 8. Photomicrographs showing textures in the sphalerite ores (transmitted light, except C in reflected light, × 100). A. Colloform sphalerite showing light and dark bands ("schalenblende"). B. Baroque dolomite crystals (do b ) and fine-grained Fe-rich dolomite (do f ) filling red-brown
Journal Article
Published: 01 September 2019
European Journal of Mineralogy (2019) 31 (5-6): 983–997.
...Fig. 4 Photomicrographs (plane-polarised light) of the sulphide mineralisation. (A) General view of the banded schalenblende spherulite cemented by colourless sphalerite and calcite (sample RN6483, TL). (B) Detailed view of banded sphalerite (sample RN6483, TL). (C): General view of banded...
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Journal Article
Journal: Economic Geology
Published: 01 January 2016
Economic Geology (2016) 111 (1): 259–269.
... and are more abundant in the lower portion of the orebody above the Cu-rich zone ( Figs. 2B , 8A ). Euhedral, brown sphalerite occurs as isolated crystals in the lower portion of the Zn-rich zone ( Fig. 8B ). Schalenblende, a finely banded ZnS (sphalerite and/or wurtzite) reported previously in the Viburnum...
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A. to E. Transmitted PPL photomicrographs of sphalerite colors and textures...
Published: 01 January 2016
by coarse, orange sphalerite, in a dolomite (Dol) and clay matrix. B. Brown sphalerite with included organic matter in sandy dolomite. C. Finely banded schalenblende (bottom) overgrown by coarser red-yellow sphalerite, crosscut by late yellow sphalerite (top left next to letter). D. Concentrically zoned
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(A) Photograph of hand specimen from the first Cardita horizon showing rhyt...
Published: 01 August 2010
per mil; (IV) thin gray layer composed either of microglobules of sphalerite or Fe oxysulfides (for details see Fig. 4B ), δ 34 S = −30.2 per mil; (V) colloform sphalerite (reddish brown to whitish schalenblende) overgrowing microglobular sphalerite, δ 34 S = −29.2 per mil; (VI) variably thick layer
Journal Article
Journal: Economic Geology
Published: 01 November 2003
Economic Geology (2003) 98 (7): 1371–1396.
...F ig . 8. Photomicrographs showing textures in the sphalerite ores (transmitted light, except C in reflected light, × 100). A. Colloform sphalerite showing light and dark bands ("schalenblende"). B. Baroque dolomite crystals (do b ) and fine-grained Fe-rich dolomite (do f ) filling red-brown...
FIGURES | View All (16)
Journal Article
Published: 01 October 2005
The Canadian Mineralogist (2005) 43 (5): 1449–1456.
... minerals . Am. Mineral . 62 , 341 – 345 . Fleet , M.E. ( 1977 b): Structural transformations in natural ZnS . Am. Mineral . 62 , 540 – 546 . Fleet , M.E. ( 1977 c): The birefringence-structural state relation in natural zinc sulfides and its application to the schalenblende from...
FIGURES
Journal Article
Journal: Economic Geology
Published: 01 August 2003
Economic Geology (2003) 98 (5): 911–932.
... 450 Replacive sphalerite and layered sphalerite ("schalenblende") overgrown by     layered marcasite HP7, 8 Mineworking 450 Concentrically layered Fe sulfides overgrowing dark brown sphalerite HP9 Mineworking 450 Limestone in contact with sphalerite ore HP10...
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Journal Article
Published: 01 April 2014
American Mineralogist (2014) 99 (4): 793–803.
... Table 2 ) found in granitic gneisses and the arsenite mineral asbecasite grown as euhedral-free crystals in fissures. The mode of occurrence of these minerals has been described by Graeser and Roggiani (1976) . Samples from Wiesloch include banded sphalerite (schalenblende) and massive galenite...
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Journal Article
Published: 21 February 2023
The Canadian Mineralogist (2022) 60 (6): 881–912.
... to 370 °C; e.g ., Behr et al . 1987 , Lögering 2008 ). In contrast, the presence of Fe-poor sphalerite, typical colloform sphalerite/wurtzite (“Schalenblende”), Ag-poor galena, and marcasite in ore structures often related to N–S or NW–SE oriented faults, and the common occurrence of elevated fluid...
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Journal Article
Published: 01 December 1984
Bulletin of Canadian Petroleum Geology (1984) 32 (4): 434–464.
... the convex-arched bands are directed toward the open voids. The botryoidal, banded sphalerite ("Schalenblende") is characteristic of high-grade ores in the upper part of the Pine Point barrier complex (Skall, 1975; Nikic, 1976; Kyle, 1977, 1981). The botryoidal sphalerites of Pine Point have been care- fully...
Journal Article
Published: 01 January 2006
Reviews in Mineralogy and Geochemistry (2006) 61 (1): 365–419.
...-structural state relation in natural zinc sulfides and its application to the schalenblende from Pribram . Can Mineral 15 : 303 – 308 Fleet ME ( 1982 ) Synthetic smythite and monoclinic Fe 3 S 4 . Phys Chem Mineral 8 : 241 – 246 Fleet ME ( 1987 ) Structure of godlevskite Ni...
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Series: Geological Society, London, Geology of Series
Published: 01 January 2011
DOI: 10.1144/GOTH.17
EISBN: 9781862393943
... and schalenblende filling voids in limestone; also mineralized breccias and varve-like ore-rich sediments in lenses composed of sphalerite > galena-pyrite with accessory boulangerite, pyrargyrite, tetrahedrite and native Ag and gangue minerals of dolomite, barite and silica. Faults and thrusts of ore bodies...
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