四川雅安软玉中透闪石的结构水晶粒尺度不均一性及其指示意义

Heterogeneity and Indicative Significance of Constitution Water in Nephrite from Ya'an, Sichuan Province

  • 摘要: 四川雅安软玉是一种新发现的基(超)性岩型软玉。对于其成玉机制,目前尚存在一些亟待解决的科学问题:该地区多期次成矿流体对软玉的成玉过程及其交代结构的多样性的影响;透闪石中水的赋存状态、结合方式及其演化趋势;透闪石中结构水和化学成分晶粒尺度不均一性的表现形式及其缘由。采用傅里叶变换显微红外光谱、电子探针等测试方法,从微观角度就雅安软玉中透闪石晶粒内结构水的存在形式、结合方式,特别是结构水与M1、M3位阳离子之间的耦合关系进行了测试与分析。结果表明,单个透闪石晶粒内由(Mg2+, Mg2+, Mg2+)-OH、(Mg2+, Mg2+, Fe2+)-OH、(Mg2+, Fe2+, Fe2+)-OH、(Fe2+, Fe2+, Fe2+)-OH伸缩振动致红外吸收谱带分别位于3 672、3 659、3 644、3 623 cm-1处。雅安软玉中结构水及其化学成分普遍存在晶粒尺度的不均一性。单个透闪石晶粒内结构水从中心向边缘整体呈现明显的递增趋势,与之对应的MgO质量分数整体呈现递增趋势,FeOT质量分数整体呈现递减趋势。研究成果有助于揭示该类型软玉矿床的成矿流体在其成玉过程中的演化规律,进而为解析其成玉机理提供科学依据。

     

    Abstract: Nephrite from Ya'an is a basic-ultrabasic type nephrite newly discovered in Sichuan Province. At present, there are still some scientific problems to be solved for its genetic mechanism.For example: How the multi-stage ore-forming fluids in the area affected the formation process of nephrite and the various metamorphic structure of nephrite from Ya'an; The occurrence state, bonding form and evolution trend of water in a single tremolite grain; The manifestation and cause of grain-scale in homogeneity of constitution water and chemical composition of tremolite. In the paper, Fourier transform micro-infrared spectroscopy and electron probe were used to reveal the existing form and bonding mode of constitution water in the tremolite grains of nephrite from Ya'an in a microscopic point of view. In particular, the coupling relationship between constitution water and M1 and M3 cations was analyzed.The results show that the infrared absorption bands of tremolite in nephrite from Ya'an caused by (Mg2+, Mg2+, Mg2+)-OH, (Mg2+, Mg2+, Fe2+)-OH, (Mg2+, Fe2+, Fe2+)-OH, (Fe2+, Fe2+, Fe2+)-OH stretching vibration were located at 3 672, 3 659, 3 644, 3 623 cm-1 respectively. The tremolite in nephrite from Ya'an generally shows grain scale heterogeneity of constitution water and chemical composition. The content of constitution water in a single tremolite grain shows a significant increasing trend from core to rim, while the MgO content shows an increasing trend and the FeOT content shows a decreasing trend. The results are helpful to reveal the evolution of the ore-forming fluid in the mineralization process of basic-ultrabasic type nephrite deposit, and provide a scientific basis for analyzing its genetic mechanism.

     

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