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机构地区:[1]中国科学院地质新技术研究所,广州510640
出 处:《矿物学报》1994年第3期292-297,共6页Acta Mineralogica Sinica
摘 要:本文采用X射线衍射、化学分析、穆斯鲍尔诺、EPR谱和红外光谱,对不同颜色的岫岩玉(岫玉)进行了测试。测试结果如下:绿色岫玉主要由叶蛇纹石组成,黄色岫玉由叶蛇纹石和利蛇纹石组成。穆斯鲍尔谱显示出Fe2+和Fe3+的两个双吸收特征。Fe2+:化学位移为1.122mm/s,四极分裂为2.701~2.721mm/s,占据八面体位置;Fe3+:化学位移为0.155~0.355mm/s,四极矩为0.337~0.470mm/s,占据四面体位置。电子顺磁共振谱显示出中心场0.336T附近,存在一个具有超精细结构的六重吸收,g≈2.0,与处于八面体上的高自旋Mn2+有关。在低场区(0.16T附近),出现两个吸收线,g分别为4.29和3.88,与处于四面体位置的Fe3+有关。红外光谱显示出与叶蛇纹石有关的OH-振动吸收带(3665~3670cm-1);在3690~3680cm-1间显示出与利蛇纹石有关的吸收肩。1070,980cm-1出现Si-O振动吸收,另尚有5个吸收带(610,560,445,400,300cm-1)。随着绿色的加重和质量的提高,岫玉中Fe2+和Mn2+的浓度也增加。证实了岫玉的绿色与Fe2+→Fe3+的荷移有关,岫玉的黄色与O2-→Fe3+荷移有关。Xiuyan jade samples of different colors were examined by X-ray diffraction, chemical analysis, Mossbauer spectrometry, EPR and IR spectroscopy.The green Xiuyan jade consists of antigorite and yellow one, lizardite.The Mossbauer spectra display two double-absorption characteristics of Fe2+and Fe3+. For Fe2+, its chemical shift is 1. 122~1.143 (mm/s), quadrupole splitting is 2. 701~2.721 (mm/s),and it occupies the octahedron position. For Fe3+ its chemical shift is 0. 155 ~ 0. 355 (mm/s),quadrupole splitting is 0. 337~0. 470 (mm/s), and it occupies the tetrahedron position.The EPR spectra show that near 3360 G there appear the sixtet absorption spectra indicating the superfine structure, g≈2. 0, which are connected with high-spin Mn2+ located in the octahedron. In the low-field range (near 0. 16 T) there are two absorption lines, g = 4. 29 and 3. 88,whidh are connected with Fe3+ located in the tetrahedron.The IR spectra display an absorption bahd of OH- (3665~ 3670cm-1 ), which is connected with the antigorite. The absorption shoulder appears at 3690~3680cm-1, which is connected with the lizardite. The vibration absorption of Si-O at 1070, 980cm-1 and five absorption bands at 610,445, 400, 300m-1 are observed.With enchancing green colour and increasing quality, the concentratons of Fe3+ and Mn2+would increase, too. This indicates that the green color of Xiuyan jade is connected with the charge transfer of Fe2+ →Fe3+. The yellow color of Xiuyan jade is connected with the charge transfer of O2-→Fe3+.
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