带有黑色海藻状矿物包裹体的南红玛瑙矿物学特征

X. Su, S. Xiaoping
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摘要

来自中国四川省凉山彝族自治州的南红玛瑙因其鲜艳的颜色在中国宝石市场上广受欢迎。其迷人的橙红色是由细赤铁矿浓度产生的。近日,凉山州当地市场上出现了一种名为“黑藻纹玛瑙”的新型玛瑙,属于南红玛瑙科。显微检查表明,样品中细小的红色和黑色颗粒矿物以丝状和浸染状等多种形式分散。利用红外光谱仪、拉曼光谱仪和x射线粉末衍射对玛瑙的宝石学和矿物学特征进行了研究。结果表明,该玛瑙矿物成分以石英为主,莫干石相对含量低,有序度高。玛瑙的结晶度约为6.76。FTIR光谱显示在3 674 cm-1处有一个与OH-有关的弱峰。结合XRD测试结果(d=8.418 A),证实玛瑙中存在层状硅酸盐。红色颗粒矿物的拉曼光谱在226、245、292 cm-1处出现峰值,与赤铁矿吻合较好。黑色颗粒的光谱与硫化物矿物一致(峰位于342、377 cm-1)。进一步的扫描电镜和背散射衍射测试结果证实,黑色颗粒矿物大部分为黄铁矿(FeAs(0.015-0.018 5)S(1.826-1.886)),属于等距体系。根据拉曼数据库,289 cm-1处的最后一个峰与黄铜矿相同。这些证据表明,在“黑藻纹玛瑙”的某些区域,黄铁矿与黄铜矿存在共生关系。另一个重要特征是,这些黑色颗粒的矿物成分和形态分布与其他地方常见的海藻纹玛瑙中出现的铁锰氧化物和有机颗粒等特征明显不同,这可能表明“黑色海藻纹玛瑙”的产地来自凉山。
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Mineralogical Characteristic of Nanhong Agate with Black Seaweed Pattern Mineral Inclusion
Nanhong agate from Liangshan Yi Autonomous Prefecture of Sichuan Province, China has gained great popularity in the gem market in China for its vibrant colour. Its attractive orange-red colour is generated by fine hematite concentrations. Recently, a new kind of agate named "black seaweed pattern agate", belonging to the family of the Nanhong agates appeared in the local market of Liangshan Prefecture. Microscopic examination showed that the fine red and black grain minerals scattered in various forms such as silkiness and disseminated forms in the sample. Infrared spectrometer, Raman spectrometer and X-ray powder diffraction were used to study the gemmological and mineralogical characteristics of the agate. The results proved that the main mineral component of the agate was quartz with a low relative content of moganite and high degree of order. The crystallinity of the agate is about 6.76. FTIR spectra showed a weak peak at 3 674 cm-1 related to OH-. Combined with the XRD testing result (d=8.418 A), it supported the existence of phyllosilicates in the agate. Raman spectrum of red grain mineal showed peaks at 226, 245, 292 cm-1, which matched well with hematite. Meanwhile the spectrum of black grain was consistent with sulfide minerals (peaks at 342, 377 cm-1). Further testing results of scanning electron microscopy and back scattering diffraction confirmed that most of the black grain mineral is pyrite(FeAs(0.015-0.018 5)S(1.826-1.886)), which belongs to isometric system. According to Raman database, the last peak at 289 cm-1 was identical with chalcopyrite. All these evidence showed pyrite had a paragenetic relationship with chalcopyrite in some area of "black seaweed pattern agate". Another important features were that mineral components and morphological distribution of these black grains were obviously different from features such as Fe and Mn oxides and organic grains that appear in common seaweed pattern agate from other places, which may indicate that the origin of "black seaweed pattern agate" is from Liangshan.
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