Gemmological Characteristic of Poudretteite
-
摘要: 硅硼钾钠石的宝石学特征的少有报道,为对该稀有宝石品种检测提供检测思路,对硅硼钾钠石样品进行常规宝石学测试,利用红外光谱仪、拉曼光谱仪、紫外-可见分光光度计和激光剥蚀-等离子体质谱仪进行了谱学特征和化学成分测试及数据分析。结果表明,硅硼钾钠石折射率范围在1.508~1.540,相对密度约为2.56~2.61,可见管状包裹体和气液包裹体,紫外灯下呈惰性,具紫红色、浅紫色中等至强的二色性;红外光谱指纹区显示1 198、1 054、951、908、797、597、559、506 cm-1和486 cm-1处特征峰;拉曼光谱测试特征拉曼位移有1 075、1 044、937、694、551、490、428、316、162 cm-1和146 cm-1;化学成分中主要含有SiO2、Na2O、K2O、B2O3,以及微量元素Al、P、Ca、Mn、Fe、Rb等,其中硅硼钾钠石含Mn元素显示紫外-可见吸收光谱测试在530 nm处绿区吸收,是其外观呈粉紫色、粉色的致色原因。Abstract: Poudretteite is a very rare gem variety, and its gemmological and spectral characteristics are rarely reported. In this paper, the gemmological and spectral characteristics and chemical compositions of poudretteite were studied using IR spectroscopy, Raman spectroscopy, LA-ICP-MS and UV-Vis spectrometer in order to provide gemmological data and the detection methods of the rare gem variety. The results showed that the refractive index of the sample is 1.508-1.540, and the relative density is 2.56-2.61. The samples showed inert under the ultraviolet lamp. It is dichromatism of purplish red and light pink. Using IR spectrometer, the absorption peaks of infrared fingerprint location feature are at 1 198、1 054、951、908、797、597、559、506 cm-1and 486 cm-1. Raman characteristic absorption peaks are at 1 075、1 044、937、694、551、490、428、316、162 cm-1and 146 cm-1. Poudretteite contains a certain amount of Al, P, Ca, Mn, Fe, Rb besides the main amounts of SiO2, Na2O, K2O, B2O3. And the 530 nm absorption band of UV-Vis spectrum is mainly caused by Mn.
-
-
表 1 硅硼钾钠石样品的常规宝石学特征
Table 1 Gemmological characteristics of poudretteite samples
样品号(颜色) 折射率 光性特征 二色性 相对密度 紫外荧光长波/短波 放大检查 P01(无色) 1.510~1.538 一轴晶正光性 无 2.56 惰性 惰性 无色、黄色空管状包裹体 P02(粉紫) 1.518~1.540 一轴晶正光性 强,紫红色、浅紫色 2.60 惰性 惰性 气液包体、管状包裹体 P03(粉色) 1.508~1.530 一轴晶正光性 强,浅紫色、粉色 2.61 惰性 惰性 “指纹状”愈合裂隙 表 2 硅硼钾钠石LA-ICP-MS测试结果
Table 2 Chemical compositions of poudretteite by LA-ICP-MS
/ppm 样品号 Be B2O3 Na2O Al2O3 SiO2 P2O5 K2O CaO MnO FeO Rb P01 1.54 109 700 68 700 8.5 770 000 430 50 500 240 1 450 77.4 P02 8.76 110 200 68 900 2.6 770 000 310 50 300 500 16 35 72.9 P03 5.90 111 500 68 900 21.6 769 000 350 50 400 200 18 45 72.7 -
[1] Smith C P, Bosshart G, Graeser S, et al. Poudretteite: A rare gem species from the Mogok Valley[J]. Gems & Gemology, 2003, 39(1): 24-31.
[2] Mayerson W M. Poudretteite[J]. Gems & Gemology, 2006, 42(4): 265.
[3] 杨主明, 傅小土. 加拿大原型产地矿物种名称的中文译名[J]. 岩石矿物学杂志, 2011, 30(4): 734-738. doi: 10.3969/j.issn.1000-6524.2011.04.019 Yang Z M, Fu X T. Recommended Chinese naming for minerals from type localities in Canada[J]. Acta Petrologica et Mineralogica, 2011, 30(4): 734-738. (in Chinese) doi: 10.3969/j.issn.1000-6524.2011.04.019
[4] Zong K, Klemd R, Yuan Y, et al. The assembly of Rodinia: The correlation of early Neoproterozoic (ca. 900Ma) high-grade metamorphism and continental arc formation in the southern Beishan Orogen, southern Central Asian Orogenic Belt (CAOB)[J]. Precambrian Research, 2017(290): 32-48.
[5] Hu Z C, Zhang W, Liu Y S, et al. "Wave" signal smoothing and mercury removing device for laser ablation quadrupole and multiple collector ICP-MS analysis: Application to lead isotope analysis[J]. Analytical Chemistry, 2015(87): 1 152-1 157.
[6] Liu Y, Hu Z, Gao S, et al. In situ analysis of major and trace elements of anhydrous minerals by LA-ICP-MS without applying an internal standard[J]. Chemical Geology, 2008, 257(1): 34-43.
[7] Lu C, Liu Y, Hu Z, et al. Accurate determinations of fifty-four major and trace elements in carbonate by LA-ICP-MS using normalization strategy of bulk components as 100%[J]. Chemical Geology, 2011, 284(3-4): 283-295.
[8] 李雯雯, 吴瑞华, 董颖. 电气石红外光谱和红外辐射特性的研究[J]. 高校地质学报, 2008, 14(3): 426-432. https://www.cnki.com.cn/Article/CJFDTOTAL-GXDX200803017.htm Li W W, Wu R H, Dong Y. Study on infrared spectra and infrared radiation characteristics of tourmaline[J]. GeologicalJournal of China Universities, 2008, 14(3): 426-432. (in Chinese) https://www.cnki.com.cn/Article/CJFDTOTAL-GXDX200803017.htm
[9] 孙宁岳, 李耿, 李星杞, 等. 马达加斯加硅硼镁铝石的宝石学特征[J]. 宝石和宝石学杂志(中英文), 2019, 21(3): 37-41. https://www.cnki.com.cn/Article/CJFDTOTAL-BSHB201903006.htm Sun N Y, Li G, Li X Q, et al. Gemmological characteristic of grandidierite from Madagascar[J]. Journal of Gems & Gemmology, 2019, 21(3): 37-41. (in Chinese) https://www.cnki.com.cn/Article/CJFDTOTAL-BSHB201903006.htm
[10] 何伟, 王以群, 毛荐. 紫色翡翠致色机理探讨[J]. 华东理工大学学报(自然科学版), 2011, 37(2): 182-185. https://www.cnki.com.cn/Article/CJFDTOTAL-HLDX201102010.htm He W, Wang Y Q, Mao J. Coloring mechanism of purple jadeite[J]. Journal of East China University of Science and Technology (Natural Science Edition), 2011, 37(2): 182-185. (in Chinese) https://www.cnki.com.cn/Article/CJFDTOTAL-HLDX201102010.htm
[11] 李英. 天然紫色翡翠致色机理的研究与探讨[D]. 秦皇岛: 燕山大学, 2013. Li Y. Research of the mechanism of color causing in the purple jade[D]. Qinhuangdao: Yanshan University, 2013. (in Chinese)
[12] 周仪君, 倪梦娜, 鲍晶, 等. 绿色荧光的粉紫色系尖晶石致色成因及发光机理探讨[J]. 中国宝石, 2021(4): 102-105. Zhou Y J, Ni M N, Bao J, et al. Discussion on the color formation and luminescence mechanism of green fluorescent pink purple spine[J]. China Gems, 2021(4): 102-105. (in Chinese)