The provenance of Yin-Shang bronzes with highly radiogenic lead isotopes
Abstract Even if the lead isotope results are same, the significance of the lead isotopic signature is quite different for the provenance study of the Chinese bronzes. The published data show that the radiogenic lead signatures in the unalloyed copper and the Yin-Shang bronzes with the low lead cont...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Ying, Qin [verfasserIn] Wei, Guofeng [verfasserIn] Huang, Qiao [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2020 |
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| Schlagwörter: |
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| Übergeordnetes Werk: |
Enthalten in: Archaeological and anthropological sciences - Berlin : Springer, 2009, 12(2020), 5 vom: 11. Apr. |
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| Übergeordnetes Werk: |
volume:12 ; year:2020 ; number:5 ; day:11 ; month:04 |
| Links: |
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| DOI / URN: |
10.1007/s12520-020-01056-8 |
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| Katalog-ID: |
SPR039379698 |
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| 520 | |a Abstract Even if the lead isotope results are same, the significance of the lead isotopic signature is quite different for the provenance study of the Chinese bronzes. The published data show that the radiogenic lead signatures in the unalloyed copper and the Yin-Shang bronzes with the low lead content are contributed by the copper deposits, while those of the South Africa and Zimbabwe bronzes with highly radiogenic lead were contributed by tin deposits. Combined with the results of lead isotope analysis by LA-MC-ICP-MS and the recent archeological discoveries, it was possible that for the Yin-Shang bronzes with highly radiogenic lead contents, the copper material was derived from Zhongtiao Mountain copper deposits, while the lead material from Huojiagou and Zhenggou in the northern margin of North China Craton, but we prefer that the lead materials were from the southern margin of the North China Craton. | ||
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10.1007/s12520-020-01056-8 doi (DE-627)SPR039379698 (SPR)s12520-020-01056-8-e DE-627 ger DE-627 rakwb eng 930 ASE 15.15 bkl 73.00 bkl Ying, Qin verfasserin aut The provenance of Yin-Shang bronzes with highly radiogenic lead isotopes 2020 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Even if the lead isotope results are same, the significance of the lead isotopic signature is quite different for the provenance study of the Chinese bronzes. The published data show that the radiogenic lead signatures in the unalloyed copper and the Yin-Shang bronzes with the low lead content are contributed by the copper deposits, while those of the South Africa and Zimbabwe bronzes with highly radiogenic lead were contributed by tin deposits. Combined with the results of lead isotope analysis by LA-MC-ICP-MS and the recent archeological discoveries, it was possible that for the Yin-Shang bronzes with highly radiogenic lead contents, the copper material was derived from Zhongtiao Mountain copper deposits, while the lead material from Huojiagou and Zhenggou in the northern margin of North China Craton, but we prefer that the lead materials were from the southern margin of the North China Craton. Lead isotope (dpeaa)DE-He213 Highly radiogenic lead (dpeaa)DE-He213 Provenance (dpeaa)DE-He213 Wei, Guofeng verfasserin aut Huang, Qiao verfasserin aut Enthalten in Archaeological and anthropological sciences Berlin : Springer, 2009 12(2020), 5 vom: 11. Apr. (DE-627)595710212 (DE-600)2486791-3 1866-9565 nnns volume:12 year:2020 number:5 day:11 month:04 https://dx.doi.org/10.1007/s12520-020-01056-8 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-ANG SSG-OPC-ASE 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_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 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_2118 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_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 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_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 15.15 ASE 73.00 ASE AR 12 2020 5 11 04 |
| spelling |
10.1007/s12520-020-01056-8 doi (DE-627)SPR039379698 (SPR)s12520-020-01056-8-e DE-627 ger DE-627 rakwb eng 930 ASE 15.15 bkl 73.00 bkl Ying, Qin verfasserin aut The provenance of Yin-Shang bronzes with highly radiogenic lead isotopes 2020 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Even if the lead isotope results are same, the significance of the lead isotopic signature is quite different for the provenance study of the Chinese bronzes. The published data show that the radiogenic lead signatures in the unalloyed copper and the Yin-Shang bronzes with the low lead content are contributed by the copper deposits, while those of the South Africa and Zimbabwe bronzes with highly radiogenic lead were contributed by tin deposits. Combined with the results of lead isotope analysis by LA-MC-ICP-MS and the recent archeological discoveries, it was possible that for the Yin-Shang bronzes with highly radiogenic lead contents, the copper material was derived from Zhongtiao Mountain copper deposits, while the lead material from Huojiagou and Zhenggou in the northern margin of North China Craton, but we prefer that the lead materials were from the southern margin of the North China Craton. Lead isotope (dpeaa)DE-He213 Highly radiogenic lead (dpeaa)DE-He213 Provenance (dpeaa)DE-He213 Wei, Guofeng verfasserin aut Huang, Qiao verfasserin aut Enthalten in Archaeological and anthropological sciences Berlin : Springer, 2009 12(2020), 5 vom: 11. Apr. (DE-627)595710212 (DE-600)2486791-3 1866-9565 nnns volume:12 year:2020 number:5 day:11 month:04 https://dx.doi.org/10.1007/s12520-020-01056-8 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-ANG SSG-OPC-ASE 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_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 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_2118 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_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 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_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 15.15 ASE 73.00 ASE AR 12 2020 5 11 04 |
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10.1007/s12520-020-01056-8 doi (DE-627)SPR039379698 (SPR)s12520-020-01056-8-e DE-627 ger DE-627 rakwb eng 930 ASE 15.15 bkl 73.00 bkl Ying, Qin verfasserin aut The provenance of Yin-Shang bronzes with highly radiogenic lead isotopes 2020 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Even if the lead isotope results are same, the significance of the lead isotopic signature is quite different for the provenance study of the Chinese bronzes. The published data show that the radiogenic lead signatures in the unalloyed copper and the Yin-Shang bronzes with the low lead content are contributed by the copper deposits, while those of the South Africa and Zimbabwe bronzes with highly radiogenic lead were contributed by tin deposits. Combined with the results of lead isotope analysis by LA-MC-ICP-MS and the recent archeological discoveries, it was possible that for the Yin-Shang bronzes with highly radiogenic lead contents, the copper material was derived from Zhongtiao Mountain copper deposits, while the lead material from Huojiagou and Zhenggou in the northern margin of North China Craton, but we prefer that the lead materials were from the southern margin of the North China Craton. Lead isotope (dpeaa)DE-He213 Highly radiogenic lead (dpeaa)DE-He213 Provenance (dpeaa)DE-He213 Wei, Guofeng verfasserin aut Huang, Qiao verfasserin aut Enthalten in Archaeological and anthropological sciences Berlin : Springer, 2009 12(2020), 5 vom: 11. Apr. (DE-627)595710212 (DE-600)2486791-3 1866-9565 nnns volume:12 year:2020 number:5 day:11 month:04 https://dx.doi.org/10.1007/s12520-020-01056-8 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-ANG SSG-OPC-ASE 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_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 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_2118 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_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 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_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 15.15 ASE 73.00 ASE AR 12 2020 5 11 04 |
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10.1007/s12520-020-01056-8 doi (DE-627)SPR039379698 (SPR)s12520-020-01056-8-e DE-627 ger DE-627 rakwb eng 930 ASE 15.15 bkl 73.00 bkl Ying, Qin verfasserin aut The provenance of Yin-Shang bronzes with highly radiogenic lead isotopes 2020 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract Even if the lead isotope results are same, the significance of the lead isotopic signature is quite different for the provenance study of the Chinese bronzes. The published data show that the radiogenic lead signatures in the unalloyed copper and the Yin-Shang bronzes with the low lead content are contributed by the copper deposits, while those of the South Africa and Zimbabwe bronzes with highly radiogenic lead were contributed by tin deposits. Combined with the results of lead isotope analysis by LA-MC-ICP-MS and the recent archeological discoveries, it was possible that for the Yin-Shang bronzes with highly radiogenic lead contents, the copper material was derived from Zhongtiao Mountain copper deposits, while the lead material from Huojiagou and Zhenggou in the northern margin of North China Craton, but we prefer that the lead materials were from the southern margin of the North China Craton. Lead isotope (dpeaa)DE-He213 Highly radiogenic lead (dpeaa)DE-He213 Provenance (dpeaa)DE-He213 Wei, Guofeng verfasserin aut Huang, Qiao verfasserin aut Enthalten in Archaeological and anthropological sciences Berlin : Springer, 2009 12(2020), 5 vom: 11. Apr. (DE-627)595710212 (DE-600)2486791-3 1866-9565 nnns volume:12 year:2020 number:5 day:11 month:04 https://dx.doi.org/10.1007/s12520-020-01056-8 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-ANG SSG-OPC-ASE 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_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 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_2118 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_4012 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 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_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 15.15 ASE 73.00 ASE AR 12 2020 5 11 04 |
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Enthalten in Archaeological and anthropological sciences 12(2020), 5 vom: 11. Apr. volume:12 year:2020 number:5 day:11 month:04 |
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Archaeological and anthropological sciences |
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Ying, Qin @@aut@@ Wei, Guofeng @@aut@@ Huang, Qiao @@aut@@ |
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Ying, Qin |
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Ying, Qin ddc 930 bkl 15.15 bkl 73.00 misc Lead isotope misc Highly radiogenic lead misc Provenance The provenance of Yin-Shang bronzes with highly radiogenic lead isotopes |
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930 ASE 15.15 bkl 73.00 bkl The provenance of Yin-Shang bronzes with highly radiogenic lead isotopes Lead isotope (dpeaa)DE-He213 Highly radiogenic lead (dpeaa)DE-He213 Provenance (dpeaa)DE-He213 |
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ddc 930 bkl 15.15 bkl 73.00 misc Lead isotope misc Highly radiogenic lead misc Provenance |
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ddc 930 bkl 15.15 bkl 73.00 misc Lead isotope misc Highly radiogenic lead misc Provenance |
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The provenance of Yin-Shang bronzes with highly radiogenic lead isotopes |
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The provenance of Yin-Shang bronzes with highly radiogenic lead isotopes |
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Ying, Qin |
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provenance of yin-shang bronzes with highly radiogenic lead isotopes |
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The provenance of Yin-Shang bronzes with highly radiogenic lead isotopes |
| abstract |
Abstract Even if the lead isotope results are same, the significance of the lead isotopic signature is quite different for the provenance study of the Chinese bronzes. The published data show that the radiogenic lead signatures in the unalloyed copper and the Yin-Shang bronzes with the low lead content are contributed by the copper deposits, while those of the South Africa and Zimbabwe bronzes with highly radiogenic lead were contributed by tin deposits. Combined with the results of lead isotope analysis by LA-MC-ICP-MS and the recent archeological discoveries, it was possible that for the Yin-Shang bronzes with highly radiogenic lead contents, the copper material was derived from Zhongtiao Mountain copper deposits, while the lead material from Huojiagou and Zhenggou in the northern margin of North China Craton, but we prefer that the lead materials were from the southern margin of the North China Craton. |
| abstractGer |
Abstract Even if the lead isotope results are same, the significance of the lead isotopic signature is quite different for the provenance study of the Chinese bronzes. The published data show that the radiogenic lead signatures in the unalloyed copper and the Yin-Shang bronzes with the low lead content are contributed by the copper deposits, while those of the South Africa and Zimbabwe bronzes with highly radiogenic lead were contributed by tin deposits. Combined with the results of lead isotope analysis by LA-MC-ICP-MS and the recent archeological discoveries, it was possible that for the Yin-Shang bronzes with highly radiogenic lead contents, the copper material was derived from Zhongtiao Mountain copper deposits, while the lead material from Huojiagou and Zhenggou in the northern margin of North China Craton, but we prefer that the lead materials were from the southern margin of the North China Craton. |
| abstract_unstemmed |
Abstract Even if the lead isotope results are same, the significance of the lead isotopic signature is quite different for the provenance study of the Chinese bronzes. The published data show that the radiogenic lead signatures in the unalloyed copper and the Yin-Shang bronzes with the low lead content are contributed by the copper deposits, while those of the South Africa and Zimbabwe bronzes with highly radiogenic lead were contributed by tin deposits. Combined with the results of lead isotope analysis by LA-MC-ICP-MS and the recent archeological discoveries, it was possible that for the Yin-Shang bronzes with highly radiogenic lead contents, the copper material was derived from Zhongtiao Mountain copper deposits, while the lead material from Huojiagou and Zhenggou in the northern margin of North China Craton, but we prefer that the lead materials were from the southern margin of the North China Craton. |
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5 |
| title_short |
The provenance of Yin-Shang bronzes with highly radiogenic lead isotopes |
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https://dx.doi.org/10.1007/s12520-020-01056-8 |
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Wei, Guofeng Huang, Qiao |
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Wei, Guofeng Huang, Qiao |
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| doi_str |
10.1007/s12520-020-01056-8 |
| up_date |
2024-07-03T23:38:36.343Z |
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| score |
7.401972 |