本文選題：大冶銅綠山　切入點(diǎn)：巖陰山腳遺址　出處：《江漢考古》2013年04期

【摘要】：采用XRF、XRD、巖相顯微觀察等現(xiàn)代檢測(cè)分析技術(shù)對(duì)湖北大冶銅綠山巖陰山腳遺址東周時(shí)期地層中"風(fēng)化殼"進(jìn)行了化學(xué)成分及巖相組織檢測(cè)分析,結(jié)合銅綠山氧化銅礦石礦物組成及地球化學(xué)特征、周圍遺跡關(guān)系,初步認(rèn)定"風(fēng)化殼"可能是沖洗礦石后的泥流沉積(尾沙沉積)。
[Abstract]:The chemical composition and lithofacies structure of weathered crust in the strata of Yingshanjiao site of Tonglushan, Daye, Hubei Province, were detected and analyzed by means of modern detection and analysis techniques such as XRF / XRD and microscopic observation of lithofacies. Combined with the mineral composition and geochemical characteristics of Tonglushan copper oxide ore and the relationship between the surrounding relics, it is preliminarily concluded that the "weathering crust" may be the mudflow deposit after washing the ore.
【作者單位】： 中國(guó)科學(xué)技術(shù)大學(xué);
【分類號(hào)】：K878

【參考文獻(xiàn)】

相關(guān)期刊論文 前4條

1 ;江西瑞昌銅嶺商周礦冶遺址第一期發(fā)掘簡(jiǎn)報(bào)[J];江西文物;1990年03期

2 席奇峰;王文平;王新華;周v，

本文編號(hào)：1672011