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先秦遺址出土朱砂的化學(xué)鑒定和產(chǎn)地判斷方法評述

發(fā)布時間:2018-08-04 19:40
【摘要】:朱砂作為顏料或墓底鋪墊在黃河流域和長江流域的眾多先秦考古遺址中都有發(fā)現(xiàn),然而現(xiàn)代朱砂礦藏則主要集中分布在我國的西南地區(qū)。因此,先秦時代很可能存在某種形式的廣域交換網(wǎng)絡(luò),促成了朱砂和其他物品的遠距離傳播。經(jīng)過對國內(nèi)外朱砂產(chǎn)地相關(guān)研究方法的評述,可知采用硫同位素和汞同位素相結(jié)合的方法對古人可能利用的汞礦的朱砂樣本和考古遺址出土的朱砂樣本進行采樣分析,有望重建先秦朱砂交換網(wǎng)絡(luò)。
[Abstract]:Cinnabar is found in many archaeological sites of the pre-Qin period in the Yellow River basin and the Yangtze River basin as a pigment or tomb bottom. However, the modern cinnabar deposits are mainly distributed in the southwest of China. Therefore, there may be some form of wide-area exchange network in the pre-Qin period, which contributed to the long-distance transmission of cinnabar and other objects. Based on the review of the relevant research methods of cinnabar production area at home and abroad, it is known that the method of combining sulfur isotope and mercury isotope can be used to sample and analyze the cinnabar samples of the mercury ores and the cinnabar samples unearthed from archaeological sites. It is expected to rebuild the pre-Qin cinnabar exchange network.
【作者單位】: 山東大學(xué)歷史文化學(xué)院;
【基金】:山東大學(xué)“考古與歷史學(xué)學(xué)科高峰建設(shè)計劃”資助
【分類號】:K878
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本文編號:2164944

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