肃北敦煌旱峡新发现的古玉矿:一个早期古代玉器材料潜在的重要源头

The Ancient Jade Mine Discovered in Dunhuang Hanxia of Northern Gansu Province: A Potential Important Source of Jade Material in Early Stage of China

  • 摘要: 古代开采玉矿遗址的发现对于考古遗址出土玉器来源的确认具有重要的价值。敦煌旱峡古玉矿遗址位于敦煌市东南部。2015年9月,甘肃省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民间线索的指引下合作勘查发现该遗址,并在当年确认了发现地面各类采矿有关遗迹145处;2016年,两家单位合作,获得国家自然科学基金项目的资助开展对敦煌古代玉矿及其玉料流变正式的研究工作;2019年,甘肃省文物及考古研究所对该玉矿遗址进行了正式发掘工作。根据遗址陶片文化类型及碳同位素测年,确认该遗址最早开采年代距今4 000年。根据对该玉矿附近散落玉料及发掘开采玉料的研究,敦煌旱峡玉矿的玉料主要为山料和戈壁料的透闪石,可以划分为白玉、青玉、黄白玉及青白玉等多种颜色类型,根据玉矿矿化与岩浆岩的产状关系,可以确认古玉矿属于岩浆岩与大理岩接触交代成因,玉料可初步细分为交代成玉R型和热液沉淀的P型两种类型。有限证据显示,在新石器晚期,肃北古玉矿的玉料已进入中原,说明肃北敦煌旱峡古玉矿是中国古代早期玉器玉料潜在的重要来源。

     

    Abstract: 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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