Proportions of lithospheric and asthenospheric components in Late Cenozoic K and K-Na lavas in Heilongjiang Province, Northeastern China
Abstract Spatiotemporal compositional variations were studied in Late Cenozoic lavas in the central part of Heilongjiang Province, China. In the rocks a common isotopically enriched asthenospheric component was determined, which is contained in lavas in northeastern China, North and South Korea, and...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Rasskazov, S. V. [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2011 |
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| Schlagwörter: |
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| Anmerkung: |
© Pleiades Publishing, Ltd. 2011 |
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| Übergeordnetes Werk: |
Enthalten in: Petrology - Moscow : MAIK Nauka/Interperiodica Publ. [u.a.], 1996, 19(2011), 6 vom: Nov., Seite 568-600 |
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| Übergeordnetes Werk: |
volume:19 ; year:2011 ; number:6 ; month:11 ; pages:568-600 |
| Links: |
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| DOI / URN: |
10.1134/S0869591111050031 |
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| Katalog-ID: |
SPR020202164 |
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| 100 | 1 | |a Rasskazov, S. V. |e verfasserin |4 aut | |
| 245 | 1 | 0 | |a Proportions of lithospheric and asthenospheric components in Late Cenozoic K and K-Na lavas in Heilongjiang Province, Northeastern China |
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| 520 | |a Abstract Spatiotemporal compositional variations were studied in Late Cenozoic lavas in the central part of Heilongjiang Province, China. In the rocks a common isotopically enriched asthenospheric component was determined, which is contained in lavas in northeastern China, North and South Korea, and southeastern Japan. The potassic rock series was determined to occur in the submeridionally trending zone of the Kedong-Erkeshan-Wudalianchi-Keluo-Xaogulihe fields, whereas the potassic-sodic series is spatially constrained to the sublatitudinally trending Nuominhe-Wuyiling zone. The submeridional zone is though to be dominated by the melting of lithospheric clinopyroxenites of strongly enriched isotopic and trace-element composition. The processes of magma generation in the sublatitudinal zone were complicated by the involvement of asthenospheric peridotites of less enriched composition in the magma generating processes. Modeling according to mixing models suggest that the major source of the partial melts in the territory was lithospheric material with minor amounts (no more than 9%) of an asthenospheric component. The magma generating processes were associated with the rifting-related thermal thinning of the local lithosphere during the overall Late Cenozoic extension of the continental margin of East Asia. | ||
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| 700 | 1 | |a Fefelov, N. N. |4 aut | |
| 700 | 1 | |a Saranina, E. V. |4 aut | |
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10.1134/S0869591111050031 doi (DE-627)SPR020202164 (SPR)S0869591111050031-e DE-627 ger DE-627 rakwb eng Rasskazov, S. V. verfasserin aut Proportions of lithospheric and asthenospheric components in Late Cenozoic K and K-Na lavas in Heilongjiang Province, Northeastern China 2011 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2011 Abstract Spatiotemporal compositional variations were studied in Late Cenozoic lavas in the central part of Heilongjiang Province, China. In the rocks a common isotopically enriched asthenospheric component was determined, which is contained in lavas in northeastern China, North and South Korea, and southeastern Japan. The potassic rock series was determined to occur in the submeridionally trending zone of the Kedong-Erkeshan-Wudalianchi-Keluo-Xaogulihe fields, whereas the potassic-sodic series is spatially constrained to the sublatitudinally trending Nuominhe-Wuyiling zone. The submeridional zone is though to be dominated by the melting of lithospheric clinopyroxenites of strongly enriched isotopic and trace-element composition. The processes of magma generation in the sublatitudinal zone were complicated by the involvement of asthenospheric peridotites of less enriched composition in the magma generating processes. Modeling according to mixing models suggest that the major source of the partial melts in the territory was lithospheric material with minor amounts (no more than 9%) of an asthenospheric component. The magma generating processes were associated with the rifting-related thermal thinning of the local lithosphere during the overall Late Cenozoic extension of the continental margin of East Asia. Volcanic Rock (dpeaa)DE-He213 86Sr (dpeaa)DE-He213 Late Miocene (dpeaa)DE-He213 Asthenosphere (dpeaa)DE-He213 Heilongjiang Province (dpeaa)DE-He213 Chuvashova, I. S. aut Liu, Ya. aut Meng, F. aut Yasnygina, T. A. aut Fefelov, N. N. aut Saranina, E. V. aut Enthalten in Petrology Moscow : MAIK Nauka/Interperiodica Publ. [u.a.], 1996 19(2011), 6 vom: Nov., Seite 568-600 (DE-627)511882602 (DE-600)2235750-6 1556-2085 nnns volume:19 year:2011 number:6 month:11 pages:568-600 https://dx.doi.org/10.1134/S0869591111050031 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 19 2011 6 11 568-600 |
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10.1134/S0869591111050031 doi (DE-627)SPR020202164 (SPR)S0869591111050031-e DE-627 ger DE-627 rakwb eng Rasskazov, S. V. verfasserin aut Proportions of lithospheric and asthenospheric components in Late Cenozoic K and K-Na lavas in Heilongjiang Province, Northeastern China 2011 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2011 Abstract Spatiotemporal compositional variations were studied in Late Cenozoic lavas in the central part of Heilongjiang Province, China. In the rocks a common isotopically enriched asthenospheric component was determined, which is contained in lavas in northeastern China, North and South Korea, and southeastern Japan. The potassic rock series was determined to occur in the submeridionally trending zone of the Kedong-Erkeshan-Wudalianchi-Keluo-Xaogulihe fields, whereas the potassic-sodic series is spatially constrained to the sublatitudinally trending Nuominhe-Wuyiling zone. The submeridional zone is though to be dominated by the melting of lithospheric clinopyroxenites of strongly enriched isotopic and trace-element composition. The processes of magma generation in the sublatitudinal zone were complicated by the involvement of asthenospheric peridotites of less enriched composition in the magma generating processes. Modeling according to mixing models suggest that the major source of the partial melts in the territory was lithospheric material with minor amounts (no more than 9%) of an asthenospheric component. The magma generating processes were associated with the rifting-related thermal thinning of the local lithosphere during the overall Late Cenozoic extension of the continental margin of East Asia. Volcanic Rock (dpeaa)DE-He213 86Sr (dpeaa)DE-He213 Late Miocene (dpeaa)DE-He213 Asthenosphere (dpeaa)DE-He213 Heilongjiang Province (dpeaa)DE-He213 Chuvashova, I. S. aut Liu, Ya. aut Meng, F. aut Yasnygina, T. A. aut Fefelov, N. N. aut Saranina, E. V. aut Enthalten in Petrology Moscow : MAIK Nauka/Interperiodica Publ. [u.a.], 1996 19(2011), 6 vom: Nov., Seite 568-600 (DE-627)511882602 (DE-600)2235750-6 1556-2085 nnns volume:19 year:2011 number:6 month:11 pages:568-600 https://dx.doi.org/10.1134/S0869591111050031 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 19 2011 6 11 568-600 |
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10.1134/S0869591111050031 doi (DE-627)SPR020202164 (SPR)S0869591111050031-e DE-627 ger DE-627 rakwb eng Rasskazov, S. V. verfasserin aut Proportions of lithospheric and asthenospheric components in Late Cenozoic K and K-Na lavas in Heilongjiang Province, Northeastern China 2011 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2011 Abstract Spatiotemporal compositional variations were studied in Late Cenozoic lavas in the central part of Heilongjiang Province, China. In the rocks a common isotopically enriched asthenospheric component was determined, which is contained in lavas in northeastern China, North and South Korea, and southeastern Japan. The potassic rock series was determined to occur in the submeridionally trending zone of the Kedong-Erkeshan-Wudalianchi-Keluo-Xaogulihe fields, whereas the potassic-sodic series is spatially constrained to the sublatitudinally trending Nuominhe-Wuyiling zone. The submeridional zone is though to be dominated by the melting of lithospheric clinopyroxenites of strongly enriched isotopic and trace-element composition. The processes of magma generation in the sublatitudinal zone were complicated by the involvement of asthenospheric peridotites of less enriched composition in the magma generating processes. Modeling according to mixing models suggest that the major source of the partial melts in the territory was lithospheric material with minor amounts (no more than 9%) of an asthenospheric component. The magma generating processes were associated with the rifting-related thermal thinning of the local lithosphere during the overall Late Cenozoic extension of the continental margin of East Asia. Volcanic Rock (dpeaa)DE-He213 86Sr (dpeaa)DE-He213 Late Miocene (dpeaa)DE-He213 Asthenosphere (dpeaa)DE-He213 Heilongjiang Province (dpeaa)DE-He213 Chuvashova, I. S. aut Liu, Ya. aut Meng, F. aut Yasnygina, T. A. aut Fefelov, N. N. aut Saranina, E. V. aut Enthalten in Petrology Moscow : MAIK Nauka/Interperiodica Publ. [u.a.], 1996 19(2011), 6 vom: Nov., Seite 568-600 (DE-627)511882602 (DE-600)2235750-6 1556-2085 nnns volume:19 year:2011 number:6 month:11 pages:568-600 https://dx.doi.org/10.1134/S0869591111050031 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 19 2011 6 11 568-600 |
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10.1134/S0869591111050031 doi (DE-627)SPR020202164 (SPR)S0869591111050031-e DE-627 ger DE-627 rakwb eng Rasskazov, S. V. verfasserin aut Proportions of lithospheric and asthenospheric components in Late Cenozoic K and K-Na lavas in Heilongjiang Province, Northeastern China 2011 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2011 Abstract Spatiotemporal compositional variations were studied in Late Cenozoic lavas in the central part of Heilongjiang Province, China. In the rocks a common isotopically enriched asthenospheric component was determined, which is contained in lavas in northeastern China, North and South Korea, and southeastern Japan. The potassic rock series was determined to occur in the submeridionally trending zone of the Kedong-Erkeshan-Wudalianchi-Keluo-Xaogulihe fields, whereas the potassic-sodic series is spatially constrained to the sublatitudinally trending Nuominhe-Wuyiling zone. The submeridional zone is though to be dominated by the melting of lithospheric clinopyroxenites of strongly enriched isotopic and trace-element composition. The processes of magma generation in the sublatitudinal zone were complicated by the involvement of asthenospheric peridotites of less enriched composition in the magma generating processes. Modeling according to mixing models suggest that the major source of the partial melts in the territory was lithospheric material with minor amounts (no more than 9%) of an asthenospheric component. The magma generating processes were associated with the rifting-related thermal thinning of the local lithosphere during the overall Late Cenozoic extension of the continental margin of East Asia. Volcanic Rock (dpeaa)DE-He213 86Sr (dpeaa)DE-He213 Late Miocene (dpeaa)DE-He213 Asthenosphere (dpeaa)DE-He213 Heilongjiang Province (dpeaa)DE-He213 Chuvashova, I. S. aut Liu, Ya. aut Meng, F. aut Yasnygina, T. A. aut Fefelov, N. N. aut Saranina, E. V. aut Enthalten in Petrology Moscow : MAIK Nauka/Interperiodica Publ. [u.a.], 1996 19(2011), 6 vom: Nov., Seite 568-600 (DE-627)511882602 (DE-600)2235750-6 1556-2085 nnns volume:19 year:2011 number:6 month:11 pages:568-600 https://dx.doi.org/10.1134/S0869591111050031 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 19 2011 6 11 568-600 |
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10.1134/S0869591111050031 doi (DE-627)SPR020202164 (SPR)S0869591111050031-e DE-627 ger DE-627 rakwb eng Rasskazov, S. V. verfasserin aut Proportions of lithospheric and asthenospheric components in Late Cenozoic K and K-Na lavas in Heilongjiang Province, Northeastern China 2011 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier © Pleiades Publishing, Ltd. 2011 Abstract Spatiotemporal compositional variations were studied in Late Cenozoic lavas in the central part of Heilongjiang Province, China. In the rocks a common isotopically enriched asthenospheric component was determined, which is contained in lavas in northeastern China, North and South Korea, and southeastern Japan. The potassic rock series was determined to occur in the submeridionally trending zone of the Kedong-Erkeshan-Wudalianchi-Keluo-Xaogulihe fields, whereas the potassic-sodic series is spatially constrained to the sublatitudinally trending Nuominhe-Wuyiling zone. The submeridional zone is though to be dominated by the melting of lithospheric clinopyroxenites of strongly enriched isotopic and trace-element composition. The processes of magma generation in the sublatitudinal zone were complicated by the involvement of asthenospheric peridotites of less enriched composition in the magma generating processes. Modeling according to mixing models suggest that the major source of the partial melts in the territory was lithospheric material with minor amounts (no more than 9%) of an asthenospheric component. The magma generating processes were associated with the rifting-related thermal thinning of the local lithosphere during the overall Late Cenozoic extension of the continental margin of East Asia. Volcanic Rock (dpeaa)DE-He213 86Sr (dpeaa)DE-He213 Late Miocene (dpeaa)DE-He213 Asthenosphere (dpeaa)DE-He213 Heilongjiang Province (dpeaa)DE-He213 Chuvashova, I. S. aut Liu, Ya. aut Meng, F. aut Yasnygina, T. A. aut Fefelov, N. N. aut Saranina, E. V. aut Enthalten in Petrology Moscow : MAIK Nauka/Interperiodica Publ. [u.a.], 1996 19(2011), 6 vom: Nov., Seite 568-600 (DE-627)511882602 (DE-600)2235750-6 1556-2085 nnns volume:19 year:2011 number:6 month:11 pages:568-600 https://dx.doi.org/10.1134/S0869591111050031 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2070 GBV_ILN_2086 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2116 GBV_ILN_2118 GBV_ILN_2119 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 AR 19 2011 6 11 568-600 |
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Enthalten in Petrology 19(2011), 6 vom: Nov., Seite 568-600 volume:19 year:2011 number:6 month:11 pages:568-600 |
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In the rocks a common isotopically enriched asthenospheric component was determined, which is contained in lavas in northeastern China, North and South Korea, and southeastern Japan. The potassic rock series was determined to occur in the submeridionally trending zone of the Kedong-Erkeshan-Wudalianchi-Keluo-Xaogulihe fields, whereas the potassic-sodic series is spatially constrained to the sublatitudinally trending Nuominhe-Wuyiling zone. The submeridional zone is though to be dominated by the melting of lithospheric clinopyroxenites of strongly enriched isotopic and trace-element composition. The processes of magma generation in the sublatitudinal zone were complicated by the involvement of asthenospheric peridotites of less enriched composition in the magma generating processes. Modeling according to mixing models suggest that the major source of the partial melts in the territory was lithospheric material with minor amounts (no more than 9%) of an asthenospheric component. 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Rasskazov, S. V. |
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Rasskazov, S. V. misc Volcanic Rock misc 86Sr misc Late Miocene misc Asthenosphere misc Heilongjiang Province Proportions of lithospheric and asthenospheric components in Late Cenozoic K and K-Na lavas in Heilongjiang Province, Northeastern China |
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Proportions of lithospheric and asthenospheric components in Late Cenozoic K and K-Na lavas in Heilongjiang Province, Northeastern China Volcanic Rock (dpeaa)DE-He213 86Sr (dpeaa)DE-He213 Late Miocene (dpeaa)DE-He213 Asthenosphere (dpeaa)DE-He213 Heilongjiang Province (dpeaa)DE-He213 |
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Proportions of lithospheric and asthenospheric components in Late Cenozoic K and K-Na lavas in Heilongjiang Province, Northeastern China |
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Proportions of lithospheric and asthenospheric components in Late Cenozoic K and K-Na lavas in Heilongjiang Province, Northeastern China |
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proportions of lithospheric and asthenospheric components in late cenozoic k and k-na lavas in heilongjiang province, northeastern china |
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Proportions of lithospheric and asthenospheric components in Late Cenozoic K and K-Na lavas in Heilongjiang Province, Northeastern China |
| abstract |
Abstract Spatiotemporal compositional variations were studied in Late Cenozoic lavas in the central part of Heilongjiang Province, China. In the rocks a common isotopically enriched asthenospheric component was determined, which is contained in lavas in northeastern China, North and South Korea, and southeastern Japan. The potassic rock series was determined to occur in the submeridionally trending zone of the Kedong-Erkeshan-Wudalianchi-Keluo-Xaogulihe fields, whereas the potassic-sodic series is spatially constrained to the sublatitudinally trending Nuominhe-Wuyiling zone. The submeridional zone is though to be dominated by the melting of lithospheric clinopyroxenites of strongly enriched isotopic and trace-element composition. The processes of magma generation in the sublatitudinal zone were complicated by the involvement of asthenospheric peridotites of less enriched composition in the magma generating processes. Modeling according to mixing models suggest that the major source of the partial melts in the territory was lithospheric material with minor amounts (no more than 9%) of an asthenospheric component. The magma generating processes were associated with the rifting-related thermal thinning of the local lithosphere during the overall Late Cenozoic extension of the continental margin of East Asia. © Pleiades Publishing, Ltd. 2011 |
| abstractGer |
Abstract Spatiotemporal compositional variations were studied in Late Cenozoic lavas in the central part of Heilongjiang Province, China. In the rocks a common isotopically enriched asthenospheric component was determined, which is contained in lavas in northeastern China, North and South Korea, and southeastern Japan. The potassic rock series was determined to occur in the submeridionally trending zone of the Kedong-Erkeshan-Wudalianchi-Keluo-Xaogulihe fields, whereas the potassic-sodic series is spatially constrained to the sublatitudinally trending Nuominhe-Wuyiling zone. The submeridional zone is though to be dominated by the melting of lithospheric clinopyroxenites of strongly enriched isotopic and trace-element composition. The processes of magma generation in the sublatitudinal zone were complicated by the involvement of asthenospheric peridotites of less enriched composition in the magma generating processes. Modeling according to mixing models suggest that the major source of the partial melts in the territory was lithospheric material with minor amounts (no more than 9%) of an asthenospheric component. The magma generating processes were associated with the rifting-related thermal thinning of the local lithosphere during the overall Late Cenozoic extension of the continental margin of East Asia. © Pleiades Publishing, Ltd. 2011 |
| abstract_unstemmed |
Abstract Spatiotemporal compositional variations were studied in Late Cenozoic lavas in the central part of Heilongjiang Province, China. In the rocks a common isotopically enriched asthenospheric component was determined, which is contained in lavas in northeastern China, North and South Korea, and southeastern Japan. The potassic rock series was determined to occur in the submeridionally trending zone of the Kedong-Erkeshan-Wudalianchi-Keluo-Xaogulihe fields, whereas the potassic-sodic series is spatially constrained to the sublatitudinally trending Nuominhe-Wuyiling zone. The submeridional zone is though to be dominated by the melting of lithospheric clinopyroxenites of strongly enriched isotopic and trace-element composition. The processes of magma generation in the sublatitudinal zone were complicated by the involvement of asthenospheric peridotites of less enriched composition in the magma generating processes. Modeling according to mixing models suggest that the major source of the partial melts in the territory was lithospheric material with minor amounts (no more than 9%) of an asthenospheric component. The magma generating processes were associated with the rifting-related thermal thinning of the local lithosphere during the overall Late Cenozoic extension of the continental margin of East Asia. © Pleiades Publishing, Ltd. 2011 |
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Proportions of lithospheric and asthenospheric components in Late Cenozoic K and K-Na lavas in Heilongjiang Province, Northeastern China |
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Chuvashova, I. S. Liu, Ya Meng, F. Yasnygina, T. A. Fefelov, N. N. Saranina, E. V. |
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Chuvashova, I. S. Liu, Ya Meng, F. Yasnygina, T. A. Fefelov, N. N. Saranina, E. V. |
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| score |
7.398798 |