摘要
采用XRF、XRD、岩相显微观察等现代检测分析技术对湖北大冶铜绿山岩阴山脚遗址东周时期地层中"风化壳"进行了化学成分及岩相组织检测分析,结合铜绿山氧化铜矿石矿物组成及地球化学特征、周围遗迹关系,初步认定"风化壳"可能是冲洗矿石后的泥流沉积(尾沙沉积)。
Phase and composition of the ＂weathering crust＂ excavated from the Yanyingshanjiao site were analyzed by microscopic observation, X-ray diffraction, and X-ray fluorescence spectrum. The resuits suggest that these crusts were sediments of waste water after washed copper ore in the ancient time.
出处
《江汉考古》
CSSCI
北大核心
2013年第4期116-119,F0003,共5页
Jianghan Archaeology
关键词
大冶铜绿山
岩阴山脚遗址
洗矿
泥流沉积
Tonglvshan of Daye City, the Yanyingshanjiao Site, ＂weathering crust＂, sediments of waste water after washed copper ore
作者简介
秦颍（1961-），男，安徽人，中国科学技术大学副教授。
