王朝文, 周武邦, 李可心, 徐畅, 严俊, 严雪俊, 陈涛, 洪汉烈. 表生作用下“老挝田黄”石皮形成的矿物学证据[J]. 宝石和宝石学杂志(中英文), 2022, 24(5): 31-43. DOI: 10.15964/j.cnki.027jgg.2022.05.003
引用本文: 王朝文, 周武邦, 李可心, 徐畅, 严俊, 严雪俊, 陈涛, 洪汉烈. 表生作用下“老挝田黄”石皮形成的矿物学证据[J]. 宝石和宝石学杂志(中英文), 2022, 24(5): 31-43. DOI: 10.15964/j.cnki.027jgg.2022.05.003
WANG Chaowen, ZHOU Wubang, LI Kexin, XU Chang, YAN Jun, YAN Xuejun, CHEN Tao, HONG Hanlie. Formation of Weathering Rim of "Laos Tianhuang" under Supergenic Process: Mineralogical Evidence[J]. Journal of Gems & Gemmology, 2022, 24(5): 31-43. DOI: 10.15964/j.cnki.027jgg.2022.05.003
Citation: WANG Chaowen, ZHOU Wubang, LI Kexin, XU Chang, YAN Jun, YAN Xuejun, CHEN Tao, HONG Hanlie. Formation of Weathering Rim of "Laos Tianhuang" under Supergenic Process: Mineralogical Evidence[J]. Journal of Gems & Gemmology, 2022, 24(5): 31-43. DOI: 10.15964/j.cnki.027jgg.2022.05.003

表生作用下“老挝田黄”石皮形成的矿物学证据

Formation of Weathering Rim of "Laos Tianhuang" under Supergenic Process: Mineralogical Evidence

  • 摘要: 田黄的鉴定和产地鉴别是当前急需解决的热点问题。石皮作为田黄形成过程中的特殊产物,记录了丰富的地质成因信息。利用常规宝石学测试、X射线粉末衍射仪、傅里叶变换红外光谱仪、拉曼光谱仪和扫描电子显微镜对“老挝田黄”样品的石肉和石皮开展了详细的矿物学特征对比,并对田黄石皮的形成过程做了深入的分析。结果表明,“老挝田黄”石皮颜色多样,有黄皮、白皮和黑皮,或多层混合。针铁矿和赤铁矿为黄皮的主要致色矿物;黄铁矿和无定型碳致其石皮呈现黑色;白色石皮主要由铁氧化物溶解流失所致。“老挝田黄”石皮较厚且磨圆较好,石皮相比石肉结构较为疏松、孔隙度大,这与田黄在沉积过程中经历了搬运作用和水岩反应有关。老挝温度高、降水量大的气候条件和富含腐殖酸的水文条件可能促进了“老挝田黄”石皮的蚀变。不同皮色的“老挝田黄”与其埋藏的位置和微环境有关。黄皮可能形成于排水受阻的环境导致Fe离子更易在石肉表面微孔隙中聚集;白皮形成于排水通畅的环境,导致Fe离子更容易流失;黑色石皮则可能与浅埋藏过程中的还原环境和微生物的作用相关。从表生成因角度去研究田黄,可为我们认识不同产地田黄之间的相似性和差别提供思路,同时对解决和田玉籽料及翡翠石皮的形成、鉴定和产地鉴别等问题具有借鉴意义。

     

    Abstract: The identification of Tianhuang and its origin identification are hot topics that needs to be solved urgently at present. The weathering rim of Tianhuang, as a special product during the formation of the stone, recorded rich geological information. In this paper, a detailed comparison of the mineralogical characteristics between the interior and weathering rim of "Laos Tianhuang" was carried out by conventional gemmological testing, X-ray powder diffractometer, Fourier transform infrared spectrosmeter, Raman spectrometer and scanning electron microscope, and the formation process of the weathering rim has been discussed in depth. The results showed that the weathering rim of "Laos Tianhuang" had various colours, including yellow, white and black, or mixed with the colours above as multiple layers. Goethite and hematite are the main colour-causing minerals of the yellow weathering rim; pyrite and amorphous carbon make the stone weathering rim black; the white stone weathering rim is mainly caused by the dissolution and loss of iron oxides. The "Laos Tianhuang" are generally well-polished and rounded with thick weathering rims. Compared with the interior, the weathering rim of "Laos Tianhuang" has a looser structure and larger porosity, which are related to the transportation and water-rock reaction of Tianhuang during the deposition process. The climatic conditions of high temperature, high precipitation, and humic acid-rich hydrological conditions in Laos may have promoted the alteration of "Laos Tianhuang". The different weathering rim colours "Laos Tianhuang" are possibly related to their burial localities and microenvironment. The yellow weathering rim may be formed in an environment with blocked drainage, which makes Fe ions more likely to accumulate in the micropores on the surface of the stone; the white weathering rim is formed in an environment with well drainage condition, which leads to the loss of Fe ions more easily; the black weathering rim may be related to the reducing environment and the role of microorganisms in the shallow burial process. Studying Tianhuang from the perspective of supergenic or surficial genesis can provide ideas for us to understand the similarities and differences between Tianhuang in different origins, and meanwhile to beneficially solve problems such as the formation, identification and origin identification of the stone crust of Hetian Yu pebble and jadeite.

     

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