1. 中山大学地球科学与工程学院
2. ,广东,广州,510275
3. 泰山学院旅游学院,山东,泰安,271021
4.
5.
纸质出版日期:2019,
网络出版日期:2019-7-25,
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杨炯, 张跃峰, 丘志力, 等. 敦煌旱峡古玉矿遗址工具石锤及其岩石材料来源分析[J]. 中山大学学报(自然科学版)(中英文), 2019,58(4):1-13.
YANG Jiong, ZHANG Yuefeng, QIU Zhili, et al. Archaeomineralogy and provenance study of the stone hammers from ancient Hanxia nephrite mining site, Dunhuang[J]. Acta Scientiarum Naturalium Universitatis SunYatseni, 2019,58(4):1-13.
杨炯, 张跃峰, 丘志力, 等. 敦煌旱峡古玉矿遗址工具石锤及其岩石材料来源分析[J]. 中山大学学报(自然科学版)(中英文), 2019,58(4):1-13. DOI: 10.13471/j.cnki.acta.snus.2019.04.001.
YANG Jiong, ZHANG Yuefeng, QIU Zhili, et al. Archaeomineralogy and provenance study of the stone hammers from ancient Hanxia nephrite mining site, Dunhuang[J]. Acta Scientiarum Naturalium Universitatis SunYatseni, 2019,58(4):1-13. DOI: 10.13471/j.cnki.acta.snus.2019.04.001.
石器工具是石器时代生产力和生产方式的重要标志。敦煌旱峡古玉矿遗址是中国目前发现最古老的玉(闪石玉)矿遗址,石器工具的矿物岩石材料学特征对于揭示当地采矿(玉)工业面貌和人群活动特点有明显的学术价值。利用偏光显微镜、XRF和ICP-MS等进行的测试显示,敦煌旱峡古玉矿遗址9件典型工具石锤的原岩分别为闪长玢岩、花岗闪长玢岩、辉绿岩、玄武岩和英安岩等岩浆岩。从宏观特征、显微结构、主微量元素特征及构造环境4个方面将石锤与附近区域出露的岩石进行了对比分析,发现它们的地质地球化学特征与以玉矿遗址为中心直径100 km范围内出露的岩浆岩一致,分别形成于火山弧及板内环境。结果表明,除部分卵石石锤外,敦煌旱峡古玉矿遗址石锤主要是就地/近取材于敦煌地块三危山玉矿及附近(以遗址为中心直径100 km范围内)的岩浆岩,特别是附近较为致密坚硬的次火山岩和火山岩。根据石锤的野外分布特点及其与其它采矿遗址石锤的比较,认为目前所研究的石锤更多为选矿(玉)工具,石锤的形制特点所反映的人类行为和社会系统力量的“技术表现”对探索采矿人群的意义有待深入探讨。
The stone tool is a key symbol of productivity and production mode in the Stone Age. Ancient Hanxia nephrite mining site in Dunhuang was archeologically recognized as the oldest jade mining site discovered in China
its mining tools
i.e. stone hammers
and their rock materials including the petrological and geochemical characteristics may provide important information for revealing their material sources and the productivity at that time. In this paper
nine typical stone hammers were selected for petrological and geochemical analysis using polarizing microscope
XRF
and ICP-MS. The results showed that the stone hammers were made of diabase
basalt
dacite
granodiorite porphyrite and diorite porphyrite rocks. These rocks were characterized by the petrogeochemistry of igneous rocks formed within intraplate or volcanic arc environment
and are consistent with local igneous rocks within tens of kilometers of the site in Dunhuang area. Further comparison of the stone hammers and relative local igneous rocks in macroscopic features
microtexture
main and trace elements
and tectonic environment can infer that
except for some pebble hammers
the stone hammers were probably processed from local igneous rocks
especially those hard & dense-textured volcanic or subvolcanic rocks at Sanwei mountain nephrite mine or neighborly close-by
maybe 100 km around. Based on the scattered position of the stone hammers in the mining site and by contrasting with those stone hammers from other sites
we think the stone hammers were used as separation tools at Hanxia nephrite mining site
but more detailed research needs to do to find out their significance and value in understanding mining personnel from the stone hammer-reflected human behaviour and technical gestures in shape & structure in social system.
石锤旱峡古玉矿遗址地球化学石料来源敦煌
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