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1.
刘国彬  卢焕章 《地球化学》1985,(3):264-268,i002
晶体中包裹体的形貌、相态、组成及分布特征对宝石矿物鉴定一直起着相当重要的作用。人们不仅能够根据包裹体特征区分出天然宝石和人造宝石,而且可以判断宝石是属于哪一种成因类型的天然矿物,或者指出是用哪种方法生长的人工宝石。这是基于宝  相似文献   

2.
矿物标型学说在宝石鉴定中具有广泛的应用前景。本文的初步分析结果表明,通过矿物标型学说不仅可以为宝石的鉴定特征找到理论依据,而且还有助于指导鉴定天然宝石与合成宝石、天然宝石与人工优化处理宝石;对某些宝石而言,还能帮助鉴定其产地。将矿物标型学说应用于宝石学,有望帮助鉴定工作者找到新的鉴定思路。  相似文献   

3.
成因矿物学的许多理论,如矿物的物理性质标型、矿物化学成分标型、矿物包裹体成分标型等都已经渗透到了宝石学研究的各项工作中,这些理论为鉴定天然宝石与人工宝石、鉴定宝石是否经过处理以及进一步鉴定天然宝石的成因和产地提供了重要的思路和依据,并且对宝石的优化与合成有着重要的指导作用.本文在总结与分析前人研究成果的基础上,根据某些常见宝石的鉴定特征(如钻石、红宝石、蓝宝石、祖母绿以及其他一些常见宝玉石等),归纳和阐述成因矿物学研究在宝石学中的实际应用.  相似文献   

4.
宝玉石产地来源的研究是近几年地质学、宝石学和考古学界的热门话题之一。一方面,不同产地来源的宝玉石可能具有不同的品质特征及经济价值,其研究有助于珠宝首饰价值的判断,为各国海关执法提供技术支持;另一方面,古代宝玉石产地的确定对了解古代宝玉石的开采与古代科技的发展水平及不同区域的文化交流均具有重要意义。在总结前人研究成果的基础上,结合现代微区测试技术的最新研究成果,从微量元素、包裹体以及同位素分析等方面探讨总结了微区测试技术在确定宝玉石产地来源研究中的应用。当前的研究结果显示,不同的技术方法对确定宝玉石的产地来源均有一定的意义,但宝玉石产地来源的最终确定往往需要依赖更大范围和更深入地对宝石矿床的地球化学进行多技术手段的交叉分析。显然,确定各种不同类型宝玉石产地来源的标型特征及建立相关重要宝石产地的地球化学数据库,是最终解决宝玉石产地来源鉴定问题的关键。  相似文献   

5.
项贤彪 《广东地质》2001,16(4):36-39
不同地质条件下产生的宝石的包裹体及其组合不同,深成岩浆产生的包裹体以固相为主;气成热液产生的包裹体三相都有;伟晶岩产生的包裹体以气液相为主,天然宝石的包裹体以自形矿物为主并含少量的气液包裹体,而合成的宝石以人工残残余物为主,优化宝石包裹体都受到后期改造,宝石中的包裹体有的具有指示产地的意义。  相似文献   

6.
陈志 《西北地质》1994,15(4):28-30
几种常见宝石的肉眼鉴定方法陈志(地矿部西安地质矿产研究所,西安,710054)大家都知道,宝石集装饰和保值于一身,宝石品种和质量不同,其差价可达数倍以至上千倍,如果在选购宝石首饰时稍有不慎,就会造成巨大的经济损失。因此,有必要介绍一些宝石的肉眼鉴定知...  相似文献   

7.
黄国君 《地质找矿论丛》2003,18(4):253-256,274
解理面反光和光泽、解理的完全度、解理面组数及其夹角、解理的空间形态、解理面反光与矿物粒度的关系等构成了矿物解理的属性,这些属性在不同种的宝石矿物或同种宝石矿物各个体中性质不同,因此可应用于宝石的鉴定,尤其肉眼对翡翠鉴别时起到关键作用。  相似文献   

8.
新疆锂辉石的鉴定特征张恩彭建平徐利成(中山大学宝玉石矿物材料研究所,广州510275)关键词锂辉石鉴定特征新疆锂辉石是一种少见的天然宝石,主要产于美国、缅甸、巴西、马达加斯加及阿富汗。近年我国新疆也发现了少量宝石级锂辉石。它多产于伟晶岩中,往往与电气...  相似文献   

9.
简敏榕  朱毅 《江苏地质》1998,22(3):161-162
1988年至今,我们宝石鉴定仪器的研制生产已走过10个年头,其中的艰辛、苦涩、甘甜令人难以忘怀。1开端1988年国内珠宝市场尚未发育,但我所已开展了许多宝玉石研究工作。岩矿室也已开展宝石鉴定工作。我们通过他们获知:在某展销会上,有人拿出英国产的二色镜...  相似文献   

10.
包裹体特征在宝石鉴别中的应用研究   总被引:1,自引:0,他引:1  
宝石中的包裹体是宝石产出环境特征的再现,它是宝石鉴别的关键,可以解决人造宝石与天然宝石的鉴别,可以作为鉴别宝石真伪的可靠手段。在研究不同成因类型的宝石包裹体和不同产地的宝石包裹体,以及天然宝石与仿制品中包裹体特征的基础上,进行了包裹体分类,并列举了不同类型包裹体特征鉴别宝石的实例。  相似文献   

11.
Pant-y-ffynnon Quarry in South Wales yielded a rich cache of fossils in the early 1950s, including articulated specimens of new species (the small sauropodomorph dinosaur Pantydraco caducus and the crocodylomorph Terrestrisuchus gracilis), but no substantial study of the wider fauna of the Pant-y-ffynnon fissure systems has been published. Here, our overview of existing specimens, a few described but mostly undescribed, as well as freshly processed material, provides a comprehensive picture of the Pant-y-ffynnon palaeo-island of the Late Triassic. This was an island with a relatively impoverished fauna dominated by small clevosaurs (rhynchocephalians), including a new species, Clevosaurus cambrica, described here from a partially articulated specimen and isolated bones. The new species has a dental morphology that is intermediate between the Late Triassic Clevosaurus hudsoni, from Cromhall Quarry to the east, and the younger C. convallis from Pant Quarry to the west, suggesting adaptive radiation of clevosaurs in the palaeo-archipelago. The larger reptiles on the palaeo-island do not exceed 1.5?m in length, including a small carnivorous crocodylomorph, Terrestrisuchus, and a possible example of insular dwarfism in the basal dinosaur Pantydraco.  相似文献   

12.
Lithostratigraphy, physicochemical stratigraphy, biostratigraphy, and geochronology of the 77–70 Ma old series bracketing the Campanian–Maastrichtian boundary have been investigated by 70 experts. For the first time, direct relationships between macro- and microfossils have been established, as well as direct and indirect relationships between chemo-physical and biostratigraphical tools. A combination of criteria for selecting the boundary level, duration estimates, uncertainties on durations and on the location of biohorizons have been considered; new chronostratigraphic units are proposed. The geological site at Tercis is accepted by the Commission on Stratigraphy as the international reference for the stratigraphy of the studied interval. To cite this article: G.S. Odin, C. R. Geoscience 334 (2002) 409–414.  相似文献   

13.
Robert L. Linnen   《Lithos》2005,80(1-4):267-280
The solubilities of columbite, tantalite, wolframite, rutile, zircon and hafnon were determined as a function of the water contents in peralkaline and subaluminous granite melts. All experiments were conducted at 1035 °C and 2 kbar and the water contents of the melts ranged from nominally dry to approximately 6 wt.% H2O. Accessory phase solubilities are not affected by the water content of the peralkaline melt. By contrast, solubilities are affected by the water content of the subaluminous melt, where the solubilities of all the accessory phases examined increase with the water content of the melt, up to 2 wt.% H2O. At higher water contents, solubilities are nearly constant. It can be concluded that water is not an important control of accessory phase solubility, although the water content will affect diffusivities of components in the melt, thus whether or not accessory phases will be present as restite material. The solubility behaviour in the subaluminous and peralkaline melts supports previous spectroscopic studies, which have observed differences in the coordination of high field strength elements in dry vs. wet subaluminous granitic glasses, but not for peralkaline granitic glasses. Lastly, the fact that wolframite solubility increases with increasing water content in the subaluminous melt suggests that tungsten dissolved as a hexavalent species.  相似文献   

14.
15.
Calcite samples were extracted both from the rock matrix and the superficial coating of a karstified fault plane of an underground quarry, located in the eastern border of the Paris basin. The karstification is dated as Quaternary. Analysis of mechanical calcite twinning reveals that only the calcite matrix has also undergone a compression trending WNW that can be attributed to the Mio-Pliocene alpine collision. Both coating and matrix have undergone a strike-slip regime with σ1 roughly trending north–south, that could correspond to the regional present-day state of stress, a strike-slip compression rather trending NNW, modified by local phenomena. To cite this article: M. Rocher et al., C. R. Geoscience 335 (2003).  相似文献   

16.
正20141520 Bo Ying(Key Laboratory of Metallogeny and Mineral Assessment,MLR,Beijing 100037,China);Liu Chenglin Saline Spring Hydrochemical Characteristics and Indicators for Potassium Exploration in Southwestern and Northern Tarim Basin,Xinjiang(Acta Geoscientica Sinica,ISSN1006-3021,CN11-3474/P,34(5),2013,p.594-602,5 illus.,3 tables,28 refs.)  相似文献   

17.
正20141243Chen Ge(Hangzhou Research Institute of Petroleum Geology,PetroChina,Hangzhou 310023,China);Si Chunsong Study on Sedimentary Numerical Simulation Method of Fan Delta Sand Body(Journal of Geology,  相似文献   

18.
正20142599Chen Sanming(Guangxi Key Laboratory of Concealed Deposits Exploration,Guilin University of Technology,Guilin541004,China);He Yuzhou Block Model and Reserves Estimation of Panzhihua Iron Deposit Based on 3D Geological Modeling(Journal of Guilin University of Technology,ISSN1674-9057,CN45-1375/N,33(4),2013,p.610-615,9illus.,1table,15refs.)  相似文献   

19.
正20140594 Bai Daoyuan(Hunan Institute of Geology Survey,Changsha 410016,China);Zhong Xiang Faults in the Jingzhou Basin and Their Tectonic Settings(Geotectonica et Metallogenia,ISSN1001-1552,CN44-1595/P,37(2),2013,p.173-183,6illus.,59refs.)Key words:basin evolution,tectonic setting,South China In the Upper Paleozoic and Jurassic se-  相似文献   

20.
正20141912Cao Hui(State Key Laboratory for Continental Tectonics and Dynamics,Institute of Geology,Chinese Academy of Geological Sciences,Beijing 100037,China)Gravitational Collapse and Folding during Orogenesis:A Comparative Study of FIA Trends and Fold Axial Plane Traces(Geology in China,ISSN1000-3657,CN11-1167/P,40(6),2013,p.1818-1828,9illus.,35refs.,with  相似文献   

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