阴极发光

辽宁复县金刚石的阴极发光特征及其意义

Cathodoluminescence features of diamond in fuxian , Liaoning Province and their implications

阴极发光光谱在金矿床评价中的应用

Application of cathodoluminescence Spectroscopy to the evaluation of gold deposit

直流等离子体CVD金刚石膜的阴极发光性质的研究

Cathodeluminescence Study of Diamond Films by DC Plasma CVD

通过阴极发光法（CL）可以研究这些区域的光学性能。

The optical property of these sectors was studied by cathodoluminescence ( CL ) .

其分类方法主要依赖于地球化学特征的研究，包括阴极发光、电子探针、碳氧同位素、稀土元素以及X射线衍射分析。

The classification method depends on mainly the study of geochemical characteristics , which includes cathodeluminescence , electron probe , carbon-oxygen isotope , rare earth element and X-ray diffraction analysis .

对Allende陨石的富钙铝包裹体中的斜长石，用电子探针和扫描电镜进行阴极发光的研究。

Cathodoluminescence with scanning electron microscopy and electron microprobe is applied to the study of some plagioclases in CAIs of the Allende chondrite .

Mn／Sr比值在考虑了控制碳酸盐阴极发光性的Mn含量的同时，兼顾了海相和陆相元素的相对含量，因而是一种较全面的成岩蚀变性判断标准。

The Mn / Sr value considers the Mn content for control factors of cathodoluminescence and the relative content of the marine versus terrigenous elements . So the Mn / Sr ratio is the relatively comprehensive discrimination criterion for controlling the alteration of marine carbonate .

这些紫外阴极发光谱在天然钻石和人工处理后的天然钻石中都没有发现，可能是Chatham合成钻石的特征谱，因而可能具有一定鉴定价值。

We did not find the same ultraviolet cathodoluminescence peaks with natural diamonds , and believe that they may be characteristic peaks and valuable fingerprints of Chatham synthetic diamonds .

结合片麻岩中锆石阴极发光图像特征，说明该地区的变质作用和岩浆作用的时间范围在293±6Ma～271±5Ma期间。

Combined with characteristics of cathodoluminescence images of zircons from this gneiss , it is indicated that metamorphism and magmatism could be happened during period of 293 ± 6Ma ~ 271 ± 5Ma .

阴极发光和红外光谱技术在金刚石研究中的应用

Application of cathodoluminescence and FTIR analysis in diamond studies

次生石英的紫外阴极发光机理及意义

UV-Cathodoluminescence Mechanism of Secondary Enlarged Quartz and Its Importance

缅甸翡翠阴极发光光谱表征

Characteristics of Cathodoluminescence Spectra of Jadeite Jades from Burma

辐照处理彩色钻石的缺陷中心及阴极发光谱

CL spectrum and defect centres of irradiated colour diamonds

应用阴极发光鉴定蓝色托帕石

Application of Cathodoluminescence to Identification of Blue Topaz

阴极发光仪在变质岩和花岗岩类岩石中的应用

Application of Cathodoluminescence to Metamorphic and Granitic Rocks

阴极发光技术在成岩成矿作用研究中的应用

Application of Cathodoluminescence to Mineralization and Lithogenesis Studying

海相碳酸盐矿物的阴极发光性与其成岩蚀变的关系

Cathodoluminescence and diagenetic alteration of marine carbonate minerals

滇西昌宁-孟连带硅质岩的阴极发光特征及其意义

Characteristics and significance of cathodoluminescence of siliceous rocks in Changning-Menglian belt , southwestern Yunnan

512砂岩型铀矿床赋矿砂岩的阴极发光特征及其研究意义

Cathodoluminescent Characteristics of Sandstone and the Implications for Sandstone Type No. 512 Uranium Deposit

阴极发光在古生物地层工作中的应用

Application of cathodoluminescence to Paleontology and stratigraphy

碳酸盐矿物阴极发光性的控制因素分析

Controlling factors of cathodeluminescence of carbonate minerals

扫描电镜中的阴极发光技术及其在地学中的应用

The cathodoluminescence technique and its geological application

阴极发光图像可以提供锆石成因类型及相应岩体经历的演化历史等信息。

The cathodoluminescence images provide information on genesis and evolution histories of the host rocks .

阴极发光在湘西北地区二叠&三叠系界线事件及地层对比中应用的尝试

Application of cathodoluminescence to the Permian-Triassic boundary events and stratigraphic correlation in northwestern hunan , china

本文对引起阴极发光的物理机制也进行了讨论。

The possible physical mechanism of cathodoluminescence in anorthite is also discussed in the present paper .

结论：利用阴极发光技术进行储层地质研究已初见成效，有待进一步推广应用。

The purpose is to make more guide for researchers in the study of reservoir andsedimentare facies .

用阴极发光显微术研究YAG：Nd~（3+）晶体中的缺陷

Study of defects in YAG : Nd ~ ( 3 + ) crystals by means of cathodoluminescence micrography

明显的轻、重元素分馏和铕异常则表明碎屑岩源区地壳内有较的深熔作用。锆石Th/U比和阴极发光表明它们基本上来自岩浆岩物源区。

The Th / U values and cathodoluminescence of zircons indicate that most zircons were derived from the magmatite provenance .

锆石中的矿物包体分布特征与相应的阴极发光图像存在十分完好的对应关系。

There is an evidently corresponding relationship between the distributing feature of mineral inclusions and the cathodoluminescence image of zircon .

样品主要显示蓝白色、黄绿色的阴极发光，局部出现紫色、粉红色发光区。

Samples mainly display a blue and white , yellow green cathode luminescence , local appears purple , pink light district .