New mineral data from the kamafugitecarbonatite association: The melilitolite from Pian di Celle, Italy
Summary A detailed mineralogical investigation of a Pian di Celle sill rock (San Venanzo, Italy), classified asmelilitolite and associated withvenanzite and carbonatitic pyroclasts, revealed new and rare mineral parageneses, considered as characteristic of thekamafugite-carbonatite association. Thes...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Stoppa, F. [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
1997 |
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| Anmerkung: |
© Springer-Verlag 1997 |
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| Übergeordnetes Werk: |
Enthalten in: Mineralogy and petrology - Springer-Verlag, 1987, 61(1997), 1-4 vom: März, Seite 27-45 |
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| Übergeordnetes Werk: |
volume:61 ; year:1997 ; number:1-4 ; month:03 ; pages:27-45 |
| Links: |
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| DOI / URN: |
10.1007/BF01172476 |
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| Katalog-ID: |
OLC2062480997 |
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| 245 | 1 | 0 | |a New mineral data from the kamafugitecarbonatite association: The melilitolite from Pian di Celle, Italy |
| 264 | 1 | |c 1997 | |
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| 520 | |a Summary A detailed mineralogical investigation of a Pian di Celle sill rock (San Venanzo, Italy), classified asmelilitolite and associated withvenanzite and carbonatitic pyroclasts, revealed new and rare mineral parageneses, considered as characteristic of thekamafugite-carbonatite association. These are formed by several accessory minerals, including minerals of the cuspidine family, götzenite, khibinskite, minerals of the rhodesite- delhayelite- macdonaldite family, pyrrhotite, bartonite and (Fe, Ni, Co) monoarsenide, mostly optically and chemically identified also in fluid inclusions. The chemical composition of these minerals and their probable crystallisation succession, deduced from textural relationships, demonstrates extensive atomic substitutions, notably for Ca, Ti, Mg and alkali, essentially reflecting high concentrations of REE, Sr, Ba, Nb and Zr, which significantly varied during crystallisation. Molecular alkali excess over Al and high Ca content in ($ H_{2} $O, F, $ CO_{2} $)-rich, Siundersaturated liquid(s) are considered the dominant factors in controlling the stability of disilicate-type minerals. Separation of the carbonatite liquid from the silicate magma, constrained by textural and fluid inclusion data, was fundamental in moving the residuum onto a strongly peralkaline trend which stabilised the sulphides under changed redox conditions. | ||
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| 650 | 4 | |a Mineral Paragenesis | |
| 650 | 4 | |a Fluid Inclusion Data | |
| 650 | 4 | |a Mineralogical Investigation | |
| 700 | 1 | |a Sharygin, V. V. |4 aut | |
| 700 | 1 | |a Cundari, A. |4 aut | |
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10.1007/BF01172476 doi (DE-627)OLC2062480997 (DE-He213)BF01172476-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn TE 1000 VZ rvk Stoppa, F. verfasserin aut New mineral data from the kamafugitecarbonatite association: The melilitolite from Pian di Celle, Italy 1997 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1997 Summary A detailed mineralogical investigation of a Pian di Celle sill rock (San Venanzo, Italy), classified asmelilitolite and associated withvenanzite and carbonatitic pyroclasts, revealed new and rare mineral parageneses, considered as characteristic of thekamafugite-carbonatite association. These are formed by several accessory minerals, including minerals of the cuspidine family, götzenite, khibinskite, minerals of the rhodesite- delhayelite- macdonaldite family, pyrrhotite, bartonite and (Fe, Ni, Co) monoarsenide, mostly optically and chemically identified also in fluid inclusions. The chemical composition of these minerals and their probable crystallisation succession, deduced from textural relationships, demonstrates extensive atomic substitutions, notably for Ca, Ti, Mg and alkali, essentially reflecting high concentrations of REE, Sr, Ba, Nb and Zr, which significantly varied during crystallisation. Molecular alkali excess over Al and high Ca content in ($ H_{2} $O, F, $ CO_{2} $)-rich, Siundersaturated liquid(s) are considered the dominant factors in controlling the stability of disilicate-type minerals. Separation of the carbonatite liquid from the silicate magma, constrained by textural and fluid inclusion data, was fundamental in moving the residuum onto a strongly peralkaline trend which stabilised the sulphides under changed redox conditions. Fluid Inclusion Silicate Magma Mineral Paragenesis Fluid Inclusion Data Mineralogical Investigation Sharygin, V. V. aut Cundari, A. aut Enthalten in Mineralogy and petrology Springer-Verlag, 1987 61(1997), 1-4 vom: März, Seite 27-45 (DE-627)129383856 (DE-600)166036-6 (DE-576)014770881 0930-0708 nnns volume:61 year:1997 number:1-4 month:03 pages:27-45 https://doi.org/10.1007/BF01172476 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_22 GBV_ILN_31 GBV_ILN_40 GBV_ILN_65 GBV_ILN_70 GBV_ILN_2004 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_2027 GBV_ILN_2399 GBV_ILN_4012 GBV_ILN_4029 GBV_ILN_4103 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4306 TE 1000 AR 61 1997 1-4 03 27-45 |
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10.1007/BF01172476 doi (DE-627)OLC2062480997 (DE-He213)BF01172476-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn TE 1000 VZ rvk Stoppa, F. verfasserin aut New mineral data from the kamafugitecarbonatite association: The melilitolite from Pian di Celle, Italy 1997 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1997 Summary A detailed mineralogical investigation of a Pian di Celle sill rock (San Venanzo, Italy), classified asmelilitolite and associated withvenanzite and carbonatitic pyroclasts, revealed new and rare mineral parageneses, considered as characteristic of thekamafugite-carbonatite association. These are formed by several accessory minerals, including minerals of the cuspidine family, götzenite, khibinskite, minerals of the rhodesite- delhayelite- macdonaldite family, pyrrhotite, bartonite and (Fe, Ni, Co) monoarsenide, mostly optically and chemically identified also in fluid inclusions. The chemical composition of these minerals and their probable crystallisation succession, deduced from textural relationships, demonstrates extensive atomic substitutions, notably for Ca, Ti, Mg and alkali, essentially reflecting high concentrations of REE, Sr, Ba, Nb and Zr, which significantly varied during crystallisation. Molecular alkali excess over Al and high Ca content in ($ H_{2} $O, F, $ CO_{2} $)-rich, Siundersaturated liquid(s) are considered the dominant factors in controlling the stability of disilicate-type minerals. Separation of the carbonatite liquid from the silicate magma, constrained by textural and fluid inclusion data, was fundamental in moving the residuum onto a strongly peralkaline trend which stabilised the sulphides under changed redox conditions. Fluid Inclusion Silicate Magma Mineral Paragenesis Fluid Inclusion Data Mineralogical Investigation Sharygin, V. V. aut Cundari, A. aut Enthalten in Mineralogy and petrology Springer-Verlag, 1987 61(1997), 1-4 vom: März, Seite 27-45 (DE-627)129383856 (DE-600)166036-6 (DE-576)014770881 0930-0708 nnns volume:61 year:1997 number:1-4 month:03 pages:27-45 https://doi.org/10.1007/BF01172476 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_22 GBV_ILN_31 GBV_ILN_40 GBV_ILN_65 GBV_ILN_70 GBV_ILN_2004 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_2027 GBV_ILN_2399 GBV_ILN_4012 GBV_ILN_4029 GBV_ILN_4103 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4306 TE 1000 AR 61 1997 1-4 03 27-45 |
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10.1007/BF01172476 doi (DE-627)OLC2062480997 (DE-He213)BF01172476-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn TE 1000 VZ rvk Stoppa, F. verfasserin aut New mineral data from the kamafugitecarbonatite association: The melilitolite from Pian di Celle, Italy 1997 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1997 Summary A detailed mineralogical investigation of a Pian di Celle sill rock (San Venanzo, Italy), classified asmelilitolite and associated withvenanzite and carbonatitic pyroclasts, revealed new and rare mineral parageneses, considered as characteristic of thekamafugite-carbonatite association. These are formed by several accessory minerals, including minerals of the cuspidine family, götzenite, khibinskite, minerals of the rhodesite- delhayelite- macdonaldite family, pyrrhotite, bartonite and (Fe, Ni, Co) monoarsenide, mostly optically and chemically identified also in fluid inclusions. The chemical composition of these minerals and their probable crystallisation succession, deduced from textural relationships, demonstrates extensive atomic substitutions, notably for Ca, Ti, Mg and alkali, essentially reflecting high concentrations of REE, Sr, Ba, Nb and Zr, which significantly varied during crystallisation. Molecular alkali excess over Al and high Ca content in ($ H_{2} $O, F, $ CO_{2} $)-rich, Siundersaturated liquid(s) are considered the dominant factors in controlling the stability of disilicate-type minerals. Separation of the carbonatite liquid from the silicate magma, constrained by textural and fluid inclusion data, was fundamental in moving the residuum onto a strongly peralkaline trend which stabilised the sulphides under changed redox conditions. Fluid Inclusion Silicate Magma Mineral Paragenesis Fluid Inclusion Data Mineralogical Investigation Sharygin, V. V. aut Cundari, A. aut Enthalten in Mineralogy and petrology Springer-Verlag, 1987 61(1997), 1-4 vom: März, Seite 27-45 (DE-627)129383856 (DE-600)166036-6 (DE-576)014770881 0930-0708 nnns volume:61 year:1997 number:1-4 month:03 pages:27-45 https://doi.org/10.1007/BF01172476 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_22 GBV_ILN_31 GBV_ILN_40 GBV_ILN_65 GBV_ILN_70 GBV_ILN_2004 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_2027 GBV_ILN_2399 GBV_ILN_4012 GBV_ILN_4029 GBV_ILN_4103 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4306 TE 1000 AR 61 1997 1-4 03 27-45 |
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10.1007/BF01172476 doi (DE-627)OLC2062480997 (DE-He213)BF01172476-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn TE 1000 VZ rvk Stoppa, F. verfasserin aut New mineral data from the kamafugitecarbonatite association: The melilitolite from Pian di Celle, Italy 1997 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1997 Summary A detailed mineralogical investigation of a Pian di Celle sill rock (San Venanzo, Italy), classified asmelilitolite and associated withvenanzite and carbonatitic pyroclasts, revealed new and rare mineral parageneses, considered as characteristic of thekamafugite-carbonatite association. These are formed by several accessory minerals, including minerals of the cuspidine family, götzenite, khibinskite, minerals of the rhodesite- delhayelite- macdonaldite family, pyrrhotite, bartonite and (Fe, Ni, Co) monoarsenide, mostly optically and chemically identified also in fluid inclusions. The chemical composition of these minerals and their probable crystallisation succession, deduced from textural relationships, demonstrates extensive atomic substitutions, notably for Ca, Ti, Mg and alkali, essentially reflecting high concentrations of REE, Sr, Ba, Nb and Zr, which significantly varied during crystallisation. Molecular alkali excess over Al and high Ca content in ($ H_{2} $O, F, $ CO_{2} $)-rich, Siundersaturated liquid(s) are considered the dominant factors in controlling the stability of disilicate-type minerals. Separation of the carbonatite liquid from the silicate magma, constrained by textural and fluid inclusion data, was fundamental in moving the residuum onto a strongly peralkaline trend which stabilised the sulphides under changed redox conditions. Fluid Inclusion Silicate Magma Mineral Paragenesis Fluid Inclusion Data Mineralogical Investigation Sharygin, V. V. aut Cundari, A. aut Enthalten in Mineralogy and petrology Springer-Verlag, 1987 61(1997), 1-4 vom: März, Seite 27-45 (DE-627)129383856 (DE-600)166036-6 (DE-576)014770881 0930-0708 nnns volume:61 year:1997 number:1-4 month:03 pages:27-45 https://doi.org/10.1007/BF01172476 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_22 GBV_ILN_31 GBV_ILN_40 GBV_ILN_65 GBV_ILN_70 GBV_ILN_2004 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_2027 GBV_ILN_2399 GBV_ILN_4012 GBV_ILN_4029 GBV_ILN_4103 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4306 TE 1000 AR 61 1997 1-4 03 27-45 |
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10.1007/BF01172476 doi (DE-627)OLC2062480997 (DE-He213)BF01172476-p DE-627 ger DE-627 rakwb eng 550 VZ 13 ssgn TE 1000 VZ rvk Stoppa, F. verfasserin aut New mineral data from the kamafugitecarbonatite association: The melilitolite from Pian di Celle, Italy 1997 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1997 Summary A detailed mineralogical investigation of a Pian di Celle sill rock (San Venanzo, Italy), classified asmelilitolite and associated withvenanzite and carbonatitic pyroclasts, revealed new and rare mineral parageneses, considered as characteristic of thekamafugite-carbonatite association. These are formed by several accessory minerals, including minerals of the cuspidine family, götzenite, khibinskite, minerals of the rhodesite- delhayelite- macdonaldite family, pyrrhotite, bartonite and (Fe, Ni, Co) monoarsenide, mostly optically and chemically identified also in fluid inclusions. The chemical composition of these minerals and their probable crystallisation succession, deduced from textural relationships, demonstrates extensive atomic substitutions, notably for Ca, Ti, Mg and alkali, essentially reflecting high concentrations of REE, Sr, Ba, Nb and Zr, which significantly varied during crystallisation. Molecular alkali excess over Al and high Ca content in ($ H_{2} $O, F, $ CO_{2} $)-rich, Siundersaturated liquid(s) are considered the dominant factors in controlling the stability of disilicate-type minerals. Separation of the carbonatite liquid from the silicate magma, constrained by textural and fluid inclusion data, was fundamental in moving the residuum onto a strongly peralkaline trend which stabilised the sulphides under changed redox conditions. Fluid Inclusion Silicate Magma Mineral Paragenesis Fluid Inclusion Data Mineralogical Investigation Sharygin, V. V. aut Cundari, A. aut Enthalten in Mineralogy and petrology Springer-Verlag, 1987 61(1997), 1-4 vom: März, Seite 27-45 (DE-627)129383856 (DE-600)166036-6 (DE-576)014770881 0930-0708 nnns volume:61 year:1997 number:1-4 month:03 pages:27-45 https://doi.org/10.1007/BF01172476 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_22 GBV_ILN_31 GBV_ILN_40 GBV_ILN_65 GBV_ILN_70 GBV_ILN_2004 GBV_ILN_2010 GBV_ILN_2015 GBV_ILN_2027 GBV_ILN_2399 GBV_ILN_4012 GBV_ILN_4029 GBV_ILN_4103 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4306 TE 1000 AR 61 1997 1-4 03 27-45 |
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Enthalten in Mineralogy and petrology 61(1997), 1-4 vom: März, Seite 27-45 volume:61 year:1997 number:1-4 month:03 pages:27-45 |
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Enthalten in Mineralogy and petrology 61(1997), 1-4 vom: März, Seite 27-45 volume:61 year:1997 number:1-4 month:03 pages:27-45 |
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550 VZ 13 ssgn TE 1000 VZ rvk New mineral data from the kamafugitecarbonatite association: The melilitolite from Pian di Celle, Italy Fluid Inclusion Silicate Magma Mineral Paragenesis Fluid Inclusion Data Mineralogical Investigation |
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new mineral data from the kamafugitecarbonatite association: the melilitolite from pian di celle, italy |
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New mineral data from the kamafugitecarbonatite association: The melilitolite from Pian di Celle, Italy |
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Summary A detailed mineralogical investigation of a Pian di Celle sill rock (San Venanzo, Italy), classified asmelilitolite and associated withvenanzite and carbonatitic pyroclasts, revealed new and rare mineral parageneses, considered as characteristic of thekamafugite-carbonatite association. These are formed by several accessory minerals, including minerals of the cuspidine family, götzenite, khibinskite, minerals of the rhodesite- delhayelite- macdonaldite family, pyrrhotite, bartonite and (Fe, Ni, Co) monoarsenide, mostly optically and chemically identified also in fluid inclusions. The chemical composition of these minerals and their probable crystallisation succession, deduced from textural relationships, demonstrates extensive atomic substitutions, notably for Ca, Ti, Mg and alkali, essentially reflecting high concentrations of REE, Sr, Ba, Nb and Zr, which significantly varied during crystallisation. Molecular alkali excess over Al and high Ca content in ($ H_{2} $O, F, $ CO_{2} $)-rich, Siundersaturated liquid(s) are considered the dominant factors in controlling the stability of disilicate-type minerals. Separation of the carbonatite liquid from the silicate magma, constrained by textural and fluid inclusion data, was fundamental in moving the residuum onto a strongly peralkaline trend which stabilised the sulphides under changed redox conditions. © Springer-Verlag 1997 |
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Summary A detailed mineralogical investigation of a Pian di Celle sill rock (San Venanzo, Italy), classified asmelilitolite and associated withvenanzite and carbonatitic pyroclasts, revealed new and rare mineral parageneses, considered as characteristic of thekamafugite-carbonatite association. These are formed by several accessory minerals, including minerals of the cuspidine family, götzenite, khibinskite, minerals of the rhodesite- delhayelite- macdonaldite family, pyrrhotite, bartonite and (Fe, Ni, Co) monoarsenide, mostly optically and chemically identified also in fluid inclusions. The chemical composition of these minerals and their probable crystallisation succession, deduced from textural relationships, demonstrates extensive atomic substitutions, notably for Ca, Ti, Mg and alkali, essentially reflecting high concentrations of REE, Sr, Ba, Nb and Zr, which significantly varied during crystallisation. Molecular alkali excess over Al and high Ca content in ($ H_{2} $O, F, $ CO_{2} $)-rich, Siundersaturated liquid(s) are considered the dominant factors in controlling the stability of disilicate-type minerals. Separation of the carbonatite liquid from the silicate magma, constrained by textural and fluid inclusion data, was fundamental in moving the residuum onto a strongly peralkaline trend which stabilised the sulphides under changed redox conditions. © Springer-Verlag 1997 |
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Summary A detailed mineralogical investigation of a Pian di Celle sill rock (San Venanzo, Italy), classified asmelilitolite and associated withvenanzite and carbonatitic pyroclasts, revealed new and rare mineral parageneses, considered as characteristic of thekamafugite-carbonatite association. These are formed by several accessory minerals, including minerals of the cuspidine family, götzenite, khibinskite, minerals of the rhodesite- delhayelite- macdonaldite family, pyrrhotite, bartonite and (Fe, Ni, Co) monoarsenide, mostly optically and chemically identified also in fluid inclusions. The chemical composition of these minerals and their probable crystallisation succession, deduced from textural relationships, demonstrates extensive atomic substitutions, notably for Ca, Ti, Mg and alkali, essentially reflecting high concentrations of REE, Sr, Ba, Nb and Zr, which significantly varied during crystallisation. Molecular alkali excess over Al and high Ca content in ($ H_{2} $O, F, $ CO_{2} $)-rich, Siundersaturated liquid(s) are considered the dominant factors in controlling the stability of disilicate-type minerals. Separation of the carbonatite liquid from the silicate magma, constrained by textural and fluid inclusion data, was fundamental in moving the residuum onto a strongly peralkaline trend which stabilised the sulphides under changed redox conditions. © Springer-Verlag 1997 |
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