Geochemical characteristics of the plagiogranites in the vicinity of Bingdaban, central Tianshan
Abstract The tectonic and geochemical characteristics suggest that the plagiogranites exposed in the vicinity of Bingdaban on the northern margin of the central Tianshan uplift zone show a distinct mantle-source character, and their enrichment in LREE and selected enrichment in LILE (large ion litho...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Liang, Liu [verfasserIn] |
|---|
| Format: |
Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
1995 |
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| Anmerkung: |
© Institute of Geochemistry, Chinese Academy of Sciences 1995 |
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| Übergeordnetes Werk: |
Enthalten in: Chinese journal of geochemistry - Science in China Press, 1985, 14(1995), 3 vom: Juli, Seite 243-249 |
|---|---|
| Übergeordnetes Werk: |
volume:14 ; year:1995 ; number:3 ; month:07 ; pages:243-249 |
| Links: |
|---|
| DOI / URN: |
10.1007/BF02842047 |
|---|
| Katalog-ID: |
OLC2088098682 |
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| 520 | |a Abstract The tectonic and geochemical characteristics suggest that the plagiogranites exposed in the vicinity of Bingdaban on the northern margin of the central Tianshan uplift zone show a distinct mantle-source character, and their enrichment in LREE and selected enrichment in LILE (large ion lithophile elements) reflect a setting related to an arc tectonic regime. These rocks represent the products formed at shallow levels from mantle-derived magmas modified with subduction components (or super crustal rocks). | ||
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| 700 | 1 | |a Yangjie, Liu |4 aut | |
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10.1007/BF02842047 doi (DE-627)OLC2088098682 (DE-He213)BF02842047-p DE-627 ger DE-627 rakwb eng 550 540 VZ 13 ssgn Liang, Liu verfasserin aut Geochemical characteristics of the plagiogranites in the vicinity of Bingdaban, central Tianshan 1995 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Institute of Geochemistry, Chinese Academy of Sciences 1995 Abstract The tectonic and geochemical characteristics suggest that the plagiogranites exposed in the vicinity of Bingdaban on the northern margin of the central Tianshan uplift zone show a distinct mantle-source character, and their enrichment in LREE and selected enrichment in LILE (large ion lithophile elements) reflect a setting related to an arc tectonic regime. These rocks represent the products formed at shallow levels from mantle-derived magmas modified with subduction components (or super crustal rocks). Zicheng, Che aut Yangjie, Liu aut Enthalten in Chinese journal of geochemistry Science in China Press, 1985 14(1995), 3 vom: Juli, Seite 243-249 (DE-627)130963208 (DE-600)1066729-5 (DE-576)077051459 1000-9426 nnns volume:14 year:1995 number:3 month:07 pages:243-249 https://doi.org/10.1007/BF02842047 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_40 GBV_ILN_70 GBV_ILN_4012 AR 14 1995 3 07 243-249 |
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10.1007/BF02842047 doi (DE-627)OLC2088098682 (DE-He213)BF02842047-p DE-627 ger DE-627 rakwb eng 550 540 VZ 13 ssgn Liang, Liu verfasserin aut Geochemical characteristics of the plagiogranites in the vicinity of Bingdaban, central Tianshan 1995 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Institute of Geochemistry, Chinese Academy of Sciences 1995 Abstract The tectonic and geochemical characteristics suggest that the plagiogranites exposed in the vicinity of Bingdaban on the northern margin of the central Tianshan uplift zone show a distinct mantle-source character, and their enrichment in LREE and selected enrichment in LILE (large ion lithophile elements) reflect a setting related to an arc tectonic regime. These rocks represent the products formed at shallow levels from mantle-derived magmas modified with subduction components (or super crustal rocks). Zicheng, Che aut Yangjie, Liu aut Enthalten in Chinese journal of geochemistry Science in China Press, 1985 14(1995), 3 vom: Juli, Seite 243-249 (DE-627)130963208 (DE-600)1066729-5 (DE-576)077051459 1000-9426 nnns volume:14 year:1995 number:3 month:07 pages:243-249 https://doi.org/10.1007/BF02842047 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_40 GBV_ILN_70 GBV_ILN_4012 AR 14 1995 3 07 243-249 |
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10.1007/BF02842047 doi (DE-627)OLC2088098682 (DE-He213)BF02842047-p DE-627 ger DE-627 rakwb eng 550 540 VZ 13 ssgn Liang, Liu verfasserin aut Geochemical characteristics of the plagiogranites in the vicinity of Bingdaban, central Tianshan 1995 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Institute of Geochemistry, Chinese Academy of Sciences 1995 Abstract The tectonic and geochemical characteristics suggest that the plagiogranites exposed in the vicinity of Bingdaban on the northern margin of the central Tianshan uplift zone show a distinct mantle-source character, and their enrichment in LREE and selected enrichment in LILE (large ion lithophile elements) reflect a setting related to an arc tectonic regime. These rocks represent the products formed at shallow levels from mantle-derived magmas modified with subduction components (or super crustal rocks). Zicheng, Che aut Yangjie, Liu aut Enthalten in Chinese journal of geochemistry Science in China Press, 1985 14(1995), 3 vom: Juli, Seite 243-249 (DE-627)130963208 (DE-600)1066729-5 (DE-576)077051459 1000-9426 nnns volume:14 year:1995 number:3 month:07 pages:243-249 https://doi.org/10.1007/BF02842047 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_40 GBV_ILN_70 GBV_ILN_4012 AR 14 1995 3 07 243-249 |
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10.1007/BF02842047 doi (DE-627)OLC2088098682 (DE-He213)BF02842047-p DE-627 ger DE-627 rakwb eng 550 540 VZ 13 ssgn Liang, Liu verfasserin aut Geochemical characteristics of the plagiogranites in the vicinity of Bingdaban, central Tianshan 1995 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Institute of Geochemistry, Chinese Academy of Sciences 1995 Abstract The tectonic and geochemical characteristics suggest that the plagiogranites exposed in the vicinity of Bingdaban on the northern margin of the central Tianshan uplift zone show a distinct mantle-source character, and their enrichment in LREE and selected enrichment in LILE (large ion lithophile elements) reflect a setting related to an arc tectonic regime. These rocks represent the products formed at shallow levels from mantle-derived magmas modified with subduction components (or super crustal rocks). Zicheng, Che aut Yangjie, Liu aut Enthalten in Chinese journal of geochemistry Science in China Press, 1985 14(1995), 3 vom: Juli, Seite 243-249 (DE-627)130963208 (DE-600)1066729-5 (DE-576)077051459 1000-9426 nnns volume:14 year:1995 number:3 month:07 pages:243-249 https://doi.org/10.1007/BF02842047 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_40 GBV_ILN_70 GBV_ILN_4012 AR 14 1995 3 07 243-249 |
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10.1007/BF02842047 doi (DE-627)OLC2088098682 (DE-He213)BF02842047-p DE-627 ger DE-627 rakwb eng 550 540 VZ 13 ssgn Liang, Liu verfasserin aut Geochemical characteristics of the plagiogranites in the vicinity of Bingdaban, central Tianshan 1995 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Institute of Geochemistry, Chinese Academy of Sciences 1995 Abstract The tectonic and geochemical characteristics suggest that the plagiogranites exposed in the vicinity of Bingdaban on the northern margin of the central Tianshan uplift zone show a distinct mantle-source character, and their enrichment in LREE and selected enrichment in LILE (large ion lithophile elements) reflect a setting related to an arc tectonic regime. These rocks represent the products formed at shallow levels from mantle-derived magmas modified with subduction components (or super crustal rocks). Zicheng, Che aut Yangjie, Liu aut Enthalten in Chinese journal of geochemistry Science in China Press, 1985 14(1995), 3 vom: Juli, Seite 243-249 (DE-627)130963208 (DE-600)1066729-5 (DE-576)077051459 1000-9426 nnns volume:14 year:1995 number:3 month:07 pages:243-249 https://doi.org/10.1007/BF02842047 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_40 GBV_ILN_70 GBV_ILN_4012 AR 14 1995 3 07 243-249 |
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geochemical characteristics of the plagiogranites in the vicinity of bingdaban, central tianshan |
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Geochemical characteristics of the plagiogranites in the vicinity of Bingdaban, central Tianshan |
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Abstract The tectonic and geochemical characteristics suggest that the plagiogranites exposed in the vicinity of Bingdaban on the northern margin of the central Tianshan uplift zone show a distinct mantle-source character, and their enrichment in LREE and selected enrichment in LILE (large ion lithophile elements) reflect a setting related to an arc tectonic regime. These rocks represent the products formed at shallow levels from mantle-derived magmas modified with subduction components (or super crustal rocks). © Institute of Geochemistry, Chinese Academy of Sciences 1995 |
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Abstract The tectonic and geochemical characteristics suggest that the plagiogranites exposed in the vicinity of Bingdaban on the northern margin of the central Tianshan uplift zone show a distinct mantle-source character, and their enrichment in LREE and selected enrichment in LILE (large ion lithophile elements) reflect a setting related to an arc tectonic regime. These rocks represent the products formed at shallow levels from mantle-derived magmas modified with subduction components (or super crustal rocks). © Institute of Geochemistry, Chinese Academy of Sciences 1995 |
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Abstract The tectonic and geochemical characteristics suggest that the plagiogranites exposed in the vicinity of Bingdaban on the northern margin of the central Tianshan uplift zone show a distinct mantle-source character, and their enrichment in LREE and selected enrichment in LILE (large ion lithophile elements) reflect a setting related to an arc tectonic regime. These rocks represent the products formed at shallow levels from mantle-derived magmas modified with subduction components (or super crustal rocks). © Institute of Geochemistry, Chinese Academy of Sciences 1995 |
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