Study on Characteristics and Genesis of “Water Line” in Qinghai Nephrite Jade
-
摘要: 通过X射线粉晶衍射分析确定了青海软玉中的“水线”主要由透闪石组成。扫描电镜下观察发现,“水线”部分中的透闪石纤维较软玉主体部分中的细且长(可达数mm),相互平行,与软玉主体部分中的透闪石纤维的大小及交织结构均存在明显差异。在显微镜下观察发现,“水线”部分中的透闪石纤维与软玉主体部分呈突变接触关系,纤维长轴方向与“水线”延伸方向近乎垂直。由此认为,青海软玉中的“水线”是由含矿流体沿软玉中的微裂隙充填形成,并据此认为,“水线”并非青海软玉所独有的产地鉴别特征。Abstract: The XRD analysis shows the "water line" in Qinghai nephrite jade is mainly composed of tremolite. The tremolite fibers in the "water line" part is thinner and longer (several mm) than that of tremolites in the nephrite part, and they parallel to each other. The tremolite fibers in the "water line" is in abrupt contact with the nephrite part. The arrange direction of the fibers is upright to the extend direction of the "water line". The "water line" is formed by filling of ore fluid along cracks in nephrite jade. And the "water line" can not be regarded as the identification characteristic of its origin.
-
Keywords:
- Qinghai nephrite jade /
- "water line" /
- genesis /
- identification characteristic
-
-
[1] 中国科学院贵阳地球化学研究所.矿物X射线粉晶鉴定手册[M].北京:科学出版社,1978. [2] S ibson R H.Fau lt structure and mechan ics in relation to green-stone gold deposits[A].Robert F,Sheahan P A,Green S B.G reenstone gold and crust evolution.NUMA Conference Volum[C].Canada:Geological Association of Canada,1990.54-60.
[3] 陈柏林.从成矿构造动力学探讨脉状金矿床成矿深度[J].地质科学,2001,36(3):380-384. [4] AП谢克林.关于在褶皱区找软玉问题[J].锁林译.国外地质科技,1996,(2):50-52. [5] 王春云,任国浩,谢源章,等.龙溪软玉矿床地质及物化特征[J].矿产与地质,1993,7(35):201-205. [6] 王时麒,段体玉,郑姿姿.岫岩软玉(透闪石玉)的矿物岩石学特征及成矿模式[J].岩石矿物学杂志,2002,21(增刊):79-90. [7] 唐延龄,陈葆章,蒋壬华.中国和田玉[M].台北:台湾地球出版社,1994. [8] 钟华邦.梅岭玉地质特征及成因探讨[J].宝石和宝石学杂志,2000,2(1):39-44.
计量
- 文章访问数: 22
- HTML全文浏览量: 0
- PDF下载量: 3