刘子琪, 华雯娴, 周征宇. 田黄的地质成因与外观特征——中华石帝之辨:“田”与“黄”[J]. 宝石和宝石学杂志(中英文), 2022, 24(2): 23-30. DOI: 10.15964/j.cnki.027jgg.2022.02.003
引用本文: 刘子琪, 华雯娴, 周征宇. 田黄的地质成因与外观特征——中华石帝之辨:“田”与“黄”[J]. 宝石和宝石学杂志(中英文), 2022, 24(2): 23-30. DOI: 10.15964/j.cnki.027jgg.2022.02.003
LIU Ziqi, HUA Wenxian, ZHOU Zhengyu. Geological Origin and Appearance Characteristics of Tianhuang: The Formation and Interpretation of Chinese "Stone Emperor"[J]. Journal of Gems & Gemmology, 2022, 24(2): 23-30. DOI: 10.15964/j.cnki.027jgg.2022.02.003
Citation: LIU Ziqi, HUA Wenxian, ZHOU Zhengyu. Geological Origin and Appearance Characteristics of Tianhuang: The Formation and Interpretation of Chinese "Stone Emperor"[J]. Journal of Gems & Gemmology, 2022, 24(2): 23-30. DOI: 10.15964/j.cnki.027jgg.2022.02.003

田黄的地质成因与外观特征——中华石帝之辨:“田”与“黄”

Geological Origin and Appearance Characteristics of Tianhuang: The Formation and Interpretation of Chinese "Stone Emperor"

  • 摘要: 通过解析田黄的生成环境及形成过程,对被誉为“石帝”的田黄的产出地、外貌表征及主要品种等开展研究和讨论,深入辨读“田”与“黄”背后的地质涵义,指出田黄“田”与“黄”是寿山石原生矿经流水的搬运作用后埋藏在山坡及山脚土壤层及砂砾层,并在富Fe的次生环境中浸染、充填致色的过程。寿山田黄经历的搬运过程不长,外表多呈棱角状、次圆状,具典型的“皮”、“红格”和“萝卜纹”特征,内部颜色通常不均一,由皮到肉,呈现颜色逐渐变浅的规律,且在微裂隙、杂质矿物及结构松散部位有颜色的集中分布,是寿山田黄鉴别的典型特征,而“乌鸦皮”、“银裹金”等非黄色田黄石皮的形成与其埋藏环境的土壤有关。

     

    Abstract: By analyzing the formation environment and process of Tianhuang, this paper studied and discussed the origin, appearance characteristics and main varieties of Tianhuang, which is known as the "stone emperor" in China and distinguished the geological meaning behind "Tian" and "Huang" in depth. It indicated that the word "Tian" and "Huang" refers to the process that the primary Shoushan stone ore transported by flowing water and is buried in the soil layer and gravel layer at the hillside and foot of the mountain and disseminated, filled and coloured in the Fe rich secondary environment. The transportation process of Tianhuang from Shoushan area is not long, and its appearance is mostly angular and sub circular, with typical characteristics including rough stone crust, fracture and radish fiber like veins. The internal colour is usually uneven, showing the pattern of gradual lightening from external to internal, and there is a concentrated distribution of colour in micro fractures, impurity minerals and loose structure, which is a typical identification feature of Tianhuang from Shoushan area. The formation of the other yellow crusts of Tianhuang are related to the buried soil environment.

     

/

返回文章
返回