Ore lead isotope variations in the Proterozoic massive pyrite deposit at Näsliden, Skellefte district, Sweden
Abstract The ore lead isotope ratios from the Näsliden deposit are mantle-like in terms of the idealized plumbotectonics model. They suggest that the Näsliden deposit was formed in the Proterozoic equivalent of a Phanerozoic primitive island arc. The mantle-like nature of the lead and its homogeneit...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Rickard, D. [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
1984 |
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| Schlagwörter: |
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| Systematik: |
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| Anmerkung: |
© Springer-Verlag 1984 |
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| Übergeordnetes Werk: |
Enthalten in: Mineralium deposita - Springer-Verlag, 1966, 19(1984), 2 vom: Apr., Seite 145-151 |
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| Übergeordnetes Werk: |
volume:19 ; year:1984 ; number:2 ; month:04 ; pages:145-151 |
| Links: |
|---|
| DOI / URN: |
10.1007/BF00204677 |
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| Katalog-ID: |
OLC2058240308 |
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| 520 | |a Abstract The ore lead isotope ratios from the Näsliden deposit are mantle-like in terms of the idealized plumbotectonics model. They suggest that the Näsliden deposit was formed in the Proterozoic equivalent of a Phanerozoic primitive island arc. The mantle-like nature of the lead and its homogeneity indicate that crustal lead does not constitute the major component of the ore lead. Crustal lead contamination is suggested to be the cause of divergences in ore lead isotopic compositions associated with later veins in the deposit. | ||
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10.1007/BF00204677 doi (DE-627)OLC2058240308 (DE-He213)BF00204677-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn TE 1000 VZ rvk Rickard, D. verfasserin aut Ore lead isotope variations in the Proterozoic massive pyrite deposit at Näsliden, Skellefte district, Sweden 1984 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1984 Abstract The ore lead isotope ratios from the Näsliden deposit are mantle-like in terms of the idealized plumbotectonics model. They suggest that the Näsliden deposit was formed in the Proterozoic equivalent of a Phanerozoic primitive island arc. The mantle-like nature of the lead and its homogeneity indicate that crustal lead does not constitute the major component of the ore lead. Crustal lead contamination is suggested to be the cause of divergences in ore lead isotopic compositions associated with later veins in the deposit. Pyrite Isotopic Composition Mineral Resource Isotope Ratio Lead Isotope Svensson, Sven-Åke aut Enthalten in Mineralium deposita Springer-Verlag, 1966 19(1984), 2 vom: Apr., Seite 145-151 (DE-627)12906906X (DE-600)1679-2 (DE-576)01440074X 0026-4598 nnns volume:19 year:1984 number:2 month:04 pages:145-151 https://doi.org/10.1007/BF00204677 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 19 1984 2 04 145-151 |
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10.1007/BF00204677 doi (DE-627)OLC2058240308 (DE-He213)BF00204677-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn TE 1000 VZ rvk Rickard, D. verfasserin aut Ore lead isotope variations in the Proterozoic massive pyrite deposit at Näsliden, Skellefte district, Sweden 1984 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1984 Abstract The ore lead isotope ratios from the Näsliden deposit are mantle-like in terms of the idealized plumbotectonics model. They suggest that the Näsliden deposit was formed in the Proterozoic equivalent of a Phanerozoic primitive island arc. The mantle-like nature of the lead and its homogeneity indicate that crustal lead does not constitute the major component of the ore lead. Crustal lead contamination is suggested to be the cause of divergences in ore lead isotopic compositions associated with later veins in the deposit. Pyrite Isotopic Composition Mineral Resource Isotope Ratio Lead Isotope Svensson, Sven-Åke aut Enthalten in Mineralium deposita Springer-Verlag, 1966 19(1984), 2 vom: Apr., Seite 145-151 (DE-627)12906906X (DE-600)1679-2 (DE-576)01440074X 0026-4598 nnns volume:19 year:1984 number:2 month:04 pages:145-151 https://doi.org/10.1007/BF00204677 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 19 1984 2 04 145-151 |
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10.1007/BF00204677 doi (DE-627)OLC2058240308 (DE-He213)BF00204677-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn TE 1000 VZ rvk Rickard, D. verfasserin aut Ore lead isotope variations in the Proterozoic massive pyrite deposit at Näsliden, Skellefte district, Sweden 1984 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1984 Abstract The ore lead isotope ratios from the Näsliden deposit are mantle-like in terms of the idealized plumbotectonics model. They suggest that the Näsliden deposit was formed in the Proterozoic equivalent of a Phanerozoic primitive island arc. The mantle-like nature of the lead and its homogeneity indicate that crustal lead does not constitute the major component of the ore lead. Crustal lead contamination is suggested to be the cause of divergences in ore lead isotopic compositions associated with later veins in the deposit. Pyrite Isotopic Composition Mineral Resource Isotope Ratio Lead Isotope Svensson, Sven-Åke aut Enthalten in Mineralium deposita Springer-Verlag, 1966 19(1984), 2 vom: Apr., Seite 145-151 (DE-627)12906906X (DE-600)1679-2 (DE-576)01440074X 0026-4598 nnns volume:19 year:1984 number:2 month:04 pages:145-151 https://doi.org/10.1007/BF00204677 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 19 1984 2 04 145-151 |
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10.1007/BF00204677 doi (DE-627)OLC2058240308 (DE-He213)BF00204677-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn TE 1000 VZ rvk Rickard, D. verfasserin aut Ore lead isotope variations in the Proterozoic massive pyrite deposit at Näsliden, Skellefte district, Sweden 1984 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1984 Abstract The ore lead isotope ratios from the Näsliden deposit are mantle-like in terms of the idealized plumbotectonics model. They suggest that the Näsliden deposit was formed in the Proterozoic equivalent of a Phanerozoic primitive island arc. The mantle-like nature of the lead and its homogeneity indicate that crustal lead does not constitute the major component of the ore lead. Crustal lead contamination is suggested to be the cause of divergences in ore lead isotopic compositions associated with later veins in the deposit. Pyrite Isotopic Composition Mineral Resource Isotope Ratio Lead Isotope Svensson, Sven-Åke aut Enthalten in Mineralium deposita Springer-Verlag, 1966 19(1984), 2 vom: Apr., Seite 145-151 (DE-627)12906906X (DE-600)1679-2 (DE-576)01440074X 0026-4598 nnns volume:19 year:1984 number:2 month:04 pages:145-151 https://doi.org/10.1007/BF00204677 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 19 1984 2 04 145-151 |
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10.1007/BF00204677 doi (DE-627)OLC2058240308 (DE-He213)BF00204677-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn TE 1000 VZ rvk Rickard, D. verfasserin aut Ore lead isotope variations in the Proterozoic massive pyrite deposit at Näsliden, Skellefte district, Sweden 1984 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1984 Abstract The ore lead isotope ratios from the Näsliden deposit are mantle-like in terms of the idealized plumbotectonics model. They suggest that the Näsliden deposit was formed in the Proterozoic equivalent of a Phanerozoic primitive island arc. The mantle-like nature of the lead and its homogeneity indicate that crustal lead does not constitute the major component of the ore lead. Crustal lead contamination is suggested to be the cause of divergences in ore lead isotopic compositions associated with later veins in the deposit. Pyrite Isotopic Composition Mineral Resource Isotope Ratio Lead Isotope Svensson, Sven-Åke aut Enthalten in Mineralium deposita Springer-Verlag, 1966 19(1984), 2 vom: Apr., Seite 145-151 (DE-627)12906906X (DE-600)1679-2 (DE-576)01440074X 0026-4598 nnns volume:19 year:1984 number:2 month:04 pages:145-151 https://doi.org/10.1007/BF00204677 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 19 1984 2 04 145-151 |
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550 VZ 13 ssgn TE 1000 VZ rvk Ore lead isotope variations in the Proterozoic massive pyrite deposit at Näsliden, Skellefte district, Sweden Pyrite Isotopic Composition Mineral Resource Isotope Ratio Lead Isotope |
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Ore lead isotope variations in the Proterozoic massive pyrite deposit at Näsliden, Skellefte district, Sweden |
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Ore lead isotope variations in the Proterozoic massive pyrite deposit at Näsliden, Skellefte district, Sweden |
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Rickard, D. |
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ore lead isotope variations in the proterozoic massive pyrite deposit at näsliden, skellefte district, sweden |
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Ore lead isotope variations in the Proterozoic massive pyrite deposit at Näsliden, Skellefte district, Sweden |
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Abstract The ore lead isotope ratios from the Näsliden deposit are mantle-like in terms of the idealized plumbotectonics model. They suggest that the Näsliden deposit was formed in the Proterozoic equivalent of a Phanerozoic primitive island arc. The mantle-like nature of the lead and its homogeneity indicate that crustal lead does not constitute the major component of the ore lead. Crustal lead contamination is suggested to be the cause of divergences in ore lead isotopic compositions associated with later veins in the deposit. © Springer-Verlag 1984 |
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Abstract The ore lead isotope ratios from the Näsliden deposit are mantle-like in terms of the idealized plumbotectonics model. They suggest that the Näsliden deposit was formed in the Proterozoic equivalent of a Phanerozoic primitive island arc. The mantle-like nature of the lead and its homogeneity indicate that crustal lead does not constitute the major component of the ore lead. Crustal lead contamination is suggested to be the cause of divergences in ore lead isotopic compositions associated with later veins in the deposit. © Springer-Verlag 1984 |
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Abstract The ore lead isotope ratios from the Näsliden deposit are mantle-like in terms of the idealized plumbotectonics model. They suggest that the Näsliden deposit was formed in the Proterozoic equivalent of a Phanerozoic primitive island arc. The mantle-like nature of the lead and its homogeneity indicate that crustal lead does not constitute the major component of the ore lead. Crustal lead contamination is suggested to be the cause of divergences in ore lead isotopic compositions associated with later veins in the deposit. © Springer-Verlag 1984 |
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Ore lead isotope variations in the Proterozoic massive pyrite deposit at Näsliden, Skellefte district, Sweden |
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