Sulfur isotope study of source and deposits of stibnite in the Turhal Area, Turkey
Abstract The Turhal antimony sulfide ore deposits are hosted by a Permian-Jurassic sequence which consists of black phyllites at the base followed by interbedded phyllites and calcareous quartzites with metabasite interlayers and then by brown-gray phyllites with marble blocks. Four different styles...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Gokçe, A. [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
1991 |
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| Schlagwörter: |
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| Systematik: |
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| Anmerkung: |
© Springer-Verlag 1991 |
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| Übergeordnetes Werk: |
Enthalten in: Mineralium deposita - Springer-Verlag, 1966, 26(1991), 1 vom: Apr., Seite 30-33 |
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| Übergeordnetes Werk: |
volume:26 ; year:1991 ; number:1 ; month:04 ; pages:30-33 |
| Links: |
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| DOI / URN: |
10.1007/BF00202361 |
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| Katalog-ID: |
OLC2058244516 |
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| 245 | 1 | 0 | |a Sulfur isotope study of source and deposits of stibnite in the Turhal Area, Turkey |
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| 520 | |a Abstract The Turhal antimony sulfide ore deposits are hosted by a Permian-Jurassic sequence which consists of black phyllites at the base followed by interbedded phyllites and calcareous quartzites with metabasite interlayers and then by brown-gray phyllites with marble blocks. Four different styles and three distinct episodes of mineralization were distinguished according to deposition features of the ores and kinkbands in the stibnite crystals. Stibnite from stratiform, disseminated and vein occurrences as well as pyrite from black phyllites showed the following sulfur isotope composition ($ δ^{34} $S): +2.8 and +3.0‰ for stratiform stibnite (n = 2), +3.6 and +5.5‰ for disseminated stibnite (n = 2), +2.5 to +7.8‰ for vein stibnite (n = 11) and -6.1 to +0.1‰ for pyrite (n = 3). The $ δ^{34} $S compositions of stibnite are interpreted as suggesting an ultimately single source for sulfur in the various styles of mineralization, i.e. synsedimentary volcanic exhalations for the stratiform and disseminated together with ores and hydrothermal mobilisation of these as well as leaching of volcanic rocks to form the vein ores. Deep basinal fluids probably under normal geothermal gradient conditions caused the leaching of the primary sulfides as suggested by the oxygen isotope composition of vein quartz associated with the ores. By contrast sulfur in pyrite is essentially a derivation of seawater sulfate through bacterial and/or chemical reduction. | ||
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10.1007/BF00202361 doi (DE-627)OLC2058244516 (DE-He213)BF00202361-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn TE 1000 VZ rvk Gokçe, A. verfasserin aut Sulfur isotope study of source and deposits of stibnite in the Turhal Area, Turkey 1991 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1991 Abstract The Turhal antimony sulfide ore deposits are hosted by a Permian-Jurassic sequence which consists of black phyllites at the base followed by interbedded phyllites and calcareous quartzites with metabasite interlayers and then by brown-gray phyllites with marble blocks. Four different styles and three distinct episodes of mineralization were distinguished according to deposition features of the ores and kinkbands in the stibnite crystals. Stibnite from stratiform, disseminated and vein occurrences as well as pyrite from black phyllites showed the following sulfur isotope composition ($ δ^{34} $S): +2.8 and +3.0‰ for stratiform stibnite (n = 2), +3.6 and +5.5‰ for disseminated stibnite (n = 2), +2.5 to +7.8‰ for vein stibnite (n = 11) and -6.1 to +0.1‰ for pyrite (n = 3). The $ δ^{34} $S compositions of stibnite are interpreted as suggesting an ultimately single source for sulfur in the various styles of mineralization, i.e. synsedimentary volcanic exhalations for the stratiform and disseminated together with ores and hydrothermal mobilisation of these as well as leaching of volcanic rocks to form the vein ores. Deep basinal fluids probably under normal geothermal gradient conditions caused the leaching of the primary sulfides as suggested by the oxygen isotope composition of vein quartz associated with the ores. By contrast sulfur in pyrite is essentially a derivation of seawater sulfate through bacterial and/or chemical reduction. Pyrite Oxygen Isotope Sulfur Isotope Oxygen Isotope Composition Kinkbands Spiro, B. aut Enthalten in Mineralium deposita Springer-Verlag, 1966 26(1991), 1 vom: Apr., Seite 30-33 (DE-627)12906906X (DE-600)1679-2 (DE-576)01440074X 0026-4598 nnns volume:26 year:1991 number:1 month:04 pages:30-33 https://doi.org/10.1007/BF00202361 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_22 GBV_ILN_30 GBV_ILN_40 GBV_ILN_65 GBV_ILN_70 GBV_ILN_2004 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_4036 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4082 GBV_ILN_4103 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4319 GBV_ILN_4323 TE 1000 AR 26 1991 1 04 30-33 |
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10.1007/BF00202361 doi (DE-627)OLC2058244516 (DE-He213)BF00202361-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn TE 1000 VZ rvk Gokçe, A. verfasserin aut Sulfur isotope study of source and deposits of stibnite in the Turhal Area, Turkey 1991 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1991 Abstract The Turhal antimony sulfide ore deposits are hosted by a Permian-Jurassic sequence which consists of black phyllites at the base followed by interbedded phyllites and calcareous quartzites with metabasite interlayers and then by brown-gray phyllites with marble blocks. Four different styles and three distinct episodes of mineralization were distinguished according to deposition features of the ores and kinkbands in the stibnite crystals. Stibnite from stratiform, disseminated and vein occurrences as well as pyrite from black phyllites showed the following sulfur isotope composition ($ δ^{34} $S): +2.8 and +3.0‰ for stratiform stibnite (n = 2), +3.6 and +5.5‰ for disseminated stibnite (n = 2), +2.5 to +7.8‰ for vein stibnite (n = 11) and -6.1 to +0.1‰ for pyrite (n = 3). The $ δ^{34} $S compositions of stibnite are interpreted as suggesting an ultimately single source for sulfur in the various styles of mineralization, i.e. synsedimentary volcanic exhalations for the stratiform and disseminated together with ores and hydrothermal mobilisation of these as well as leaching of volcanic rocks to form the vein ores. Deep basinal fluids probably under normal geothermal gradient conditions caused the leaching of the primary sulfides as suggested by the oxygen isotope composition of vein quartz associated with the ores. By contrast sulfur in pyrite is essentially a derivation of seawater sulfate through bacterial and/or chemical reduction. Pyrite Oxygen Isotope Sulfur Isotope Oxygen Isotope Composition Kinkbands Spiro, B. aut Enthalten in Mineralium deposita Springer-Verlag, 1966 26(1991), 1 vom: Apr., Seite 30-33 (DE-627)12906906X (DE-600)1679-2 (DE-576)01440074X 0026-4598 nnns volume:26 year:1991 number:1 month:04 pages:30-33 https://doi.org/10.1007/BF00202361 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_22 GBV_ILN_30 GBV_ILN_40 GBV_ILN_65 GBV_ILN_70 GBV_ILN_2004 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_4036 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4082 GBV_ILN_4103 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4319 GBV_ILN_4323 TE 1000 AR 26 1991 1 04 30-33 |
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10.1007/BF00202361 doi (DE-627)OLC2058244516 (DE-He213)BF00202361-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn TE 1000 VZ rvk Gokçe, A. verfasserin aut Sulfur isotope study of source and deposits of stibnite in the Turhal Area, Turkey 1991 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1991 Abstract The Turhal antimony sulfide ore deposits are hosted by a Permian-Jurassic sequence which consists of black phyllites at the base followed by interbedded phyllites and calcareous quartzites with metabasite interlayers and then by brown-gray phyllites with marble blocks. Four different styles and three distinct episodes of mineralization were distinguished according to deposition features of the ores and kinkbands in the stibnite crystals. Stibnite from stratiform, disseminated and vein occurrences as well as pyrite from black phyllites showed the following sulfur isotope composition ($ δ^{34} $S): +2.8 and +3.0‰ for stratiform stibnite (n = 2), +3.6 and +5.5‰ for disseminated stibnite (n = 2), +2.5 to +7.8‰ for vein stibnite (n = 11) and -6.1 to +0.1‰ for pyrite (n = 3). The $ δ^{34} $S compositions of stibnite are interpreted as suggesting an ultimately single source for sulfur in the various styles of mineralization, i.e. synsedimentary volcanic exhalations for the stratiform and disseminated together with ores and hydrothermal mobilisation of these as well as leaching of volcanic rocks to form the vein ores. Deep basinal fluids probably under normal geothermal gradient conditions caused the leaching of the primary sulfides as suggested by the oxygen isotope composition of vein quartz associated with the ores. By contrast sulfur in pyrite is essentially a derivation of seawater sulfate through bacterial and/or chemical reduction. Pyrite Oxygen Isotope Sulfur Isotope Oxygen Isotope Composition Kinkbands Spiro, B. aut Enthalten in Mineralium deposita Springer-Verlag, 1966 26(1991), 1 vom: Apr., Seite 30-33 (DE-627)12906906X (DE-600)1679-2 (DE-576)01440074X 0026-4598 nnns volume:26 year:1991 number:1 month:04 pages:30-33 https://doi.org/10.1007/BF00202361 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_22 GBV_ILN_30 GBV_ILN_40 GBV_ILN_65 GBV_ILN_70 GBV_ILN_2004 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_4036 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4082 GBV_ILN_4103 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4319 GBV_ILN_4323 TE 1000 AR 26 1991 1 04 30-33 |
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10.1007/BF00202361 doi (DE-627)OLC2058244516 (DE-He213)BF00202361-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn TE 1000 VZ rvk Gokçe, A. verfasserin aut Sulfur isotope study of source and deposits of stibnite in the Turhal Area, Turkey 1991 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1991 Abstract The Turhal antimony sulfide ore deposits are hosted by a Permian-Jurassic sequence which consists of black phyllites at the base followed by interbedded phyllites and calcareous quartzites with metabasite interlayers and then by brown-gray phyllites with marble blocks. Four different styles and three distinct episodes of mineralization were distinguished according to deposition features of the ores and kinkbands in the stibnite crystals. Stibnite from stratiform, disseminated and vein occurrences as well as pyrite from black phyllites showed the following sulfur isotope composition ($ δ^{34} $S): +2.8 and +3.0‰ for stratiform stibnite (n = 2), +3.6 and +5.5‰ for disseminated stibnite (n = 2), +2.5 to +7.8‰ for vein stibnite (n = 11) and -6.1 to +0.1‰ for pyrite (n = 3). The $ δ^{34} $S compositions of stibnite are interpreted as suggesting an ultimately single source for sulfur in the various styles of mineralization, i.e. synsedimentary volcanic exhalations for the stratiform and disseminated together with ores and hydrothermal mobilisation of these as well as leaching of volcanic rocks to form the vein ores. Deep basinal fluids probably under normal geothermal gradient conditions caused the leaching of the primary sulfides as suggested by the oxygen isotope composition of vein quartz associated with the ores. By contrast sulfur in pyrite is essentially a derivation of seawater sulfate through bacterial and/or chemical reduction. Pyrite Oxygen Isotope Sulfur Isotope Oxygen Isotope Composition Kinkbands Spiro, B. aut Enthalten in Mineralium deposita Springer-Verlag, 1966 26(1991), 1 vom: Apr., Seite 30-33 (DE-627)12906906X (DE-600)1679-2 (DE-576)01440074X 0026-4598 nnns volume:26 year:1991 number:1 month:04 pages:30-33 https://doi.org/10.1007/BF00202361 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_22 GBV_ILN_30 GBV_ILN_40 GBV_ILN_65 GBV_ILN_70 GBV_ILN_2004 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_4036 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4082 GBV_ILN_4103 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4319 GBV_ILN_4323 TE 1000 AR 26 1991 1 04 30-33 |
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10.1007/BF00202361 doi (DE-627)OLC2058244516 (DE-He213)BF00202361-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn TE 1000 VZ rvk Gokçe, A. verfasserin aut Sulfur isotope study of source and deposits of stibnite in the Turhal Area, Turkey 1991 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1991 Abstract The Turhal antimony sulfide ore deposits are hosted by a Permian-Jurassic sequence which consists of black phyllites at the base followed by interbedded phyllites and calcareous quartzites with metabasite interlayers and then by brown-gray phyllites with marble blocks. Four different styles and three distinct episodes of mineralization were distinguished according to deposition features of the ores and kinkbands in the stibnite crystals. Stibnite from stratiform, disseminated and vein occurrences as well as pyrite from black phyllites showed the following sulfur isotope composition ($ δ^{34} $S): +2.8 and +3.0‰ for stratiform stibnite (n = 2), +3.6 and +5.5‰ for disseminated stibnite (n = 2), +2.5 to +7.8‰ for vein stibnite (n = 11) and -6.1 to +0.1‰ for pyrite (n = 3). The $ δ^{34} $S compositions of stibnite are interpreted as suggesting an ultimately single source for sulfur in the various styles of mineralization, i.e. synsedimentary volcanic exhalations for the stratiform and disseminated together with ores and hydrothermal mobilisation of these as well as leaching of volcanic rocks to form the vein ores. Deep basinal fluids probably under normal geothermal gradient conditions caused the leaching of the primary sulfides as suggested by the oxygen isotope composition of vein quartz associated with the ores. By contrast sulfur in pyrite is essentially a derivation of seawater sulfate through bacterial and/or chemical reduction. Pyrite Oxygen Isotope Sulfur Isotope Oxygen Isotope Composition Kinkbands Spiro, B. aut Enthalten in Mineralium deposita Springer-Verlag, 1966 26(1991), 1 vom: Apr., Seite 30-33 (DE-627)12906906X (DE-600)1679-2 (DE-576)01440074X 0026-4598 nnns volume:26 year:1991 number:1 month:04 pages:30-33 https://doi.org/10.1007/BF00202361 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_22 GBV_ILN_30 GBV_ILN_40 GBV_ILN_65 GBV_ILN_70 GBV_ILN_2004 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_4036 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4082 GBV_ILN_4103 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4319 GBV_ILN_4323 TE 1000 AR 26 1991 1 04 30-33 |
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sulfur isotope study of source and deposits of stibnite in the turhal area, turkey |
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Sulfur isotope study of source and deposits of stibnite in the Turhal Area, Turkey |
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Abstract The Turhal antimony sulfide ore deposits are hosted by a Permian-Jurassic sequence which consists of black phyllites at the base followed by interbedded phyllites and calcareous quartzites with metabasite interlayers and then by brown-gray phyllites with marble blocks. Four different styles and three distinct episodes of mineralization were distinguished according to deposition features of the ores and kinkbands in the stibnite crystals. Stibnite from stratiform, disseminated and vein occurrences as well as pyrite from black phyllites showed the following sulfur isotope composition ($ δ^{34} $S): +2.8 and +3.0‰ for stratiform stibnite (n = 2), +3.6 and +5.5‰ for disseminated stibnite (n = 2), +2.5 to +7.8‰ for vein stibnite (n = 11) and -6.1 to +0.1‰ for pyrite (n = 3). The $ δ^{34} $S compositions of stibnite are interpreted as suggesting an ultimately single source for sulfur in the various styles of mineralization, i.e. synsedimentary volcanic exhalations for the stratiform and disseminated together with ores and hydrothermal mobilisation of these as well as leaching of volcanic rocks to form the vein ores. Deep basinal fluids probably under normal geothermal gradient conditions caused the leaching of the primary sulfides as suggested by the oxygen isotope composition of vein quartz associated with the ores. By contrast sulfur in pyrite is essentially a derivation of seawater sulfate through bacterial and/or chemical reduction. © Springer-Verlag 1991 |
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Abstract The Turhal antimony sulfide ore deposits are hosted by a Permian-Jurassic sequence which consists of black phyllites at the base followed by interbedded phyllites and calcareous quartzites with metabasite interlayers and then by brown-gray phyllites with marble blocks. Four different styles and three distinct episodes of mineralization were distinguished according to deposition features of the ores and kinkbands in the stibnite crystals. Stibnite from stratiform, disseminated and vein occurrences as well as pyrite from black phyllites showed the following sulfur isotope composition ($ δ^{34} $S): +2.8 and +3.0‰ for stratiform stibnite (n = 2), +3.6 and +5.5‰ for disseminated stibnite (n = 2), +2.5 to +7.8‰ for vein stibnite (n = 11) and -6.1 to +0.1‰ for pyrite (n = 3). The $ δ^{34} $S compositions of stibnite are interpreted as suggesting an ultimately single source for sulfur in the various styles of mineralization, i.e. synsedimentary volcanic exhalations for the stratiform and disseminated together with ores and hydrothermal mobilisation of these as well as leaching of volcanic rocks to form the vein ores. Deep basinal fluids probably under normal geothermal gradient conditions caused the leaching of the primary sulfides as suggested by the oxygen isotope composition of vein quartz associated with the ores. By contrast sulfur in pyrite is essentially a derivation of seawater sulfate through bacterial and/or chemical reduction. © Springer-Verlag 1991 |
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Abstract The Turhal antimony sulfide ore deposits are hosted by a Permian-Jurassic sequence which consists of black phyllites at the base followed by interbedded phyllites and calcareous quartzites with metabasite interlayers and then by brown-gray phyllites with marble blocks. Four different styles and three distinct episodes of mineralization were distinguished according to deposition features of the ores and kinkbands in the stibnite crystals. Stibnite from stratiform, disseminated and vein occurrences as well as pyrite from black phyllites showed the following sulfur isotope composition ($ δ^{34} $S): +2.8 and +3.0‰ for stratiform stibnite (n = 2), +3.6 and +5.5‰ for disseminated stibnite (n = 2), +2.5 to +7.8‰ for vein stibnite (n = 11) and -6.1 to +0.1‰ for pyrite (n = 3). The $ δ^{34} $S compositions of stibnite are interpreted as suggesting an ultimately single source for sulfur in the various styles of mineralization, i.e. synsedimentary volcanic exhalations for the stratiform and disseminated together with ores and hydrothermal mobilisation of these as well as leaching of volcanic rocks to form the vein ores. Deep basinal fluids probably under normal geothermal gradient conditions caused the leaching of the primary sulfides as suggested by the oxygen isotope composition of vein quartz associated with the ores. By contrast sulfur in pyrite is essentially a derivation of seawater sulfate through bacterial and/or chemical reduction. © Springer-Verlag 1991 |
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