文物保护与考古科学
文物保護與攷古科學
문물보호여고고과학
Sciences of Conservation and Archaeology
2013年
3期
55~63
,共null页
杨小刚 邹后曦 金普军 赵丛苍 凌雪 南普恒
楊小剛 鄒後晞 金普軍 趙叢蒼 凌雪 南普恆
양소강 추후희 금보군 조총창 릉설 남보항
青铜器 铅同位素 巴文化 科技考古
青銅器 鉛同位素 巴文化 科技攷古
청동기 연동위소 파문화 과기고고
Bronze ; Pb isotope ; Ba Culture ; Archaeometry
青铜器矿料来源和产地研究,是青铜时代至关重要的考古问题,也是考古的重点和难点之一。通过比较青铜器样品和矿床的Ph同位素分析数据,可以进行青铜金属原料来源的产地研究。为此,本工作利用MAT262固态离子源型质谱仪对重庆地区云阳李家坝遗址,涪陵小田溪墓群,万州大坪墓群,开县余家坝遗址东周时期巴地青铜器的铅同位素进行了测定和比值研究。结果显示其中合金中铅都为普通铅,而非放射性成因铅。实验数据反映出“Pb/。“Pb比值分布在17.4630—18.6960207Pb/。“Pb比值分布在15.5573~15.8490,208PbPb比值分布在36.7828~39.3869,除了两个数据外,大部分器物铅同位素比值分布范围几乎重叠,显示了稳定铅源的存在。此外,这批数据与滇川黔铅锌多金属成矿区的底苏和大梁子矿床数据分布范围相近,局部重合,表明其铅料来源与这一地区有着一定的关系。实验结果反映了重庆地区东周青铜器群在铅料来源上具有同一性和连续性,说明了巴人在春秋时期就已经建立了独立的青铜冶铸业,一直延续到战国时期。
青銅器礦料來源和產地研究,是青銅時代至關重要的攷古問題,也是攷古的重點和難點之一。通過比較青銅器樣品和礦床的Ph同位素分析數據,可以進行青銅金屬原料來源的產地研究。為此,本工作利用MAT262固態離子源型質譜儀對重慶地區雲暘李傢壩遺阯,涪陵小田溪墓群,萬州大坪墓群,開縣餘傢壩遺阯東週時期巴地青銅器的鉛同位素進行瞭測定和比值研究。結果顯示其中閤金中鉛都為普通鉛,而非放射性成因鉛。實驗數據反映齣“Pb/。“Pb比值分佈在17.4630—18.6960207Pb/。“Pb比值分佈在15.5573~15.8490,208PbPb比值分佈在36.7828~39.3869,除瞭兩箇數據外,大部分器物鉛同位素比值分佈範圍幾乎重疊,顯示瞭穩定鉛源的存在。此外,這批數據與滇川黔鉛鋅多金屬成礦區的底囌和大樑子礦床數據分佈範圍相近,跼部重閤,錶明其鉛料來源與這一地區有著一定的關繫。實驗結果反映瞭重慶地區東週青銅器群在鉛料來源上具有同一性和連續性,說明瞭巴人在春鞦時期就已經建立瞭獨立的青銅冶鑄業,一直延續到戰國時期。
청동기광료래원화산지연구,시청동시대지관중요적고고문제,야시고고적중점화난점지일。통과비교청동기양품화광상적Ph동위소분석수거,가이진행청동금속원료래원적산지연구。위차,본공작이용MAT262고태리자원형질보의대중경지구운양리가패유지,부릉소전계묘군,만주대평묘군,개현여가패유지동주시기파지청동기적연동위소진행료측정화비치연구。결과현시기중합금중연도위보통연,이비방사성성인연。실험수거반영출“Pb/。“Pb비치분포재17.4630—18.6960207Pb/。“Pb비치분포재15.5573~15.8490,208PbPb비치분포재36.7828~39.3869,제료량개수거외,대부분기물연동위소비치분포범위궤호중첩,현시료은정연원적존재。차외,저비수거여전천검연자다금속성광구적저소화대량자광상수거분포범위상근,국부중합,표명기연료래원여저일지구유착일정적관계。실험결과반영료중경지구동주청동기군재연료래원상구유동일성화련속성,설명료파인재춘추시기취이경건립료독립적청동야주업,일직연속도전국시기。
The origin of ore is a key issue in bronze age archaeology. It has also been one of the most difficult stud- ies. By comparing isotope ratios of lead found in ore beds and those from bronze, the researcher can sometimes i- dentify the source and origin the bronzes. This study used the MAT - 262 thermal ionization mass spectrometry (TIMS) to detect the isotope ratios of lead contained in bronzes from the Lijiaba, Xiaotianxi, Daping and Yujiaba sites in the Chongqing area. The results indicate that Pb in the bronze alloys is common lead, and that the ratios of 2~6pb/2~4pb, 2~Tpb/2~4pb and 2~spb/Z~4Pb are 17.46 - 18.67, 15.56 - 15.85 and 36.78 ~ 39.39, respectively. Except for two data sets, all results have good overlap and fall within a narrow range, indicating the same origin of the lead material. Furthermore, the isotope ratios of lead contained in bronzes from the Chongqing area match those of Pb - Zn deposits in the Sichuan - Yunnan - Guizhou Pb - Zn mineralization district, with the results being espe- cially close to those isotope ratios of Disu and Daliangzi Pb - Zn deposits. The results suggest that lead ore used for bronze in Chongqing during the East Zhou period came continuously from the same location. The results also sug- gest that the bronze smelting site of the Ba people is independent from that used from the early Spring and Autumn Period to the Warring Period.