甘肃敦煌汉峡古玉石矿:中国早期潜在的重要玉石原料来源

Zhili Qiu, Yue Zhang, Jiong Yang, Hui Wang, Guoke Chen, Yinde Li, Shizhen Zong, Zhiyong Guo, Yishi Yang, X. Gu, Xueying Ye
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引用次数: 1

摘要

古玉石开采遗址的发现,对考古遗址出土玉器的来源确认具有重要价值。敦煌汉夏古玉石矿区位于敦煌市东南部,由甘肃文物考古研究所和中山大学地球科学与工程学院研究团队在当地业余爱好者的指导下,于2015年9月共同发现。同年,在汉峡发现了145个与各种地面采矿有关的遗骸。国家自然科学基金资助的敦煌古玉石矿及其玉石物质传递的正式研究从2016年开始。该遗址于2019年由甘肃省文物考古研究所正式发掘。根据碳同位素的年代测定和陶器的文化类型,确认该遗址最早的采矿时代为4000年前。通过对矿山附近散落的玉石材料和发掘的玉石材料的研究,敦煌汉夏玉石矿区的主要玉石材料为软玉,按其赋存状态可分为原玉石和戈壁玉石,按颜色可进一步分为白玉、绿白/黄白玉等类型。根据矿化产状与岩浆岩的关系,确定古玉石矿床属于接触交代成因。玉料也可分为交代替代玉料(R型)和热液沉淀玉料(p型)两种类型。初步证据表明,新石器时代晚期,甘肃北部古玉石矿(址)的玉石物质进入中原地区,表明甘肃北部的马宗山和敦煌汉夏古玉石矿床是中国早期潜在的重要玉石物质来源。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
The Ancient Jade Mine Discovered in Dunhuang Hanxia of Northern Gansu Province: A Potential Important Source of Jade Material in Early Stage of China
The discovery of ancient jade mining sites is of great value for the confirmation of the origin of jade artifacts unearthed from archaeological sites. Dunhuang Hanxia ancient jade mining site is located in the southeast of Dunhuang city, and was discovered by the research team of Gansu Institute of Cultural Relics and Archaeology and the School of Earth Science and Engineering of Sun Yat-sen University jointly under the guidance of local amateur in September 2015. In the same year, 145 remains related to various types of mining on the ground were identified in Hanxia. The formal research supported by the National Natural Science Foundation of China on Dunhuang ancient jade mine and jade material transmission have been carried out since 2016. The site was officially excavated by the Gansu Institute of Cultural Relics and Archaeology in 2019. According to the dating of carbon isotope and cultural types of pottery, the earliest mining age of the site is confirmed to be 4 000 years ago. Based on the research with the scattered jade materials near the mine and the excavation jade materials, the main jade material of Hanxia jade mining sites in Dunhuang is nephrite, which can be divided into primary jade and Gobi material by their occurrence, and can be further grouped into white jade, green-white / yellow-white jade and other types by colour. According to the relationship between the occurrence of the mineralization and magmatic rocks, we confirm that the ancient jade deposits belong to the genesis of contact metasomatism. The jade materials can also be split into two types, i.e. metasomatic replacement jade material(R- type)and hydrothermal precipitation material(P-type). Initial evidence shows that in the late Neolithic period, the jade materials from the ancient jade mining (sites) in Northern Gansu Province entered the Central Plains of China and indicates that Mazongshan and Dunhuang Hanxia ancient jade deposits in Northern Gansu Province are potential important sources of jade materials in early stage of China.
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