首页 | 本学科首页   官方微博 | 高级检索  
相似文献
 共查询到20条相似文献,搜索用时 62 毫秒
1.
梁细荣  李献华 《岩矿测试》1999,18(4):253-258
建立了一种利用激光探针等离子体质谱技术同时原位测定锆石Pb-Pb及Pb-U年龄和25个微量元素的快速分析方法。P的检出限为14μg/g,Sc的检出限为3μg/g,Rb、Nb、Ba稀土元素Nd、Gd、Dy、Er及Yb的检出限为0.1 ̄0.3μg/g,Pb的检出限0.5μg/g,其它稀土元素及Sr、y、Hf、Ta、Th和U的检出限为10 ̄90ng/g。方法对绝大多数微量元素的相对标准偏差为5 ̄15%;  相似文献   

2.
研究了多种络合剂及组络合剂萃取水中微量元素的条件,拟定了吡咯烷荒氨酸和二乙基二硫代氨基甲酸钠混合络合剂络合,甲基异丁基酮和乙酸异戊酯混合溶剂萃取,原子吸收光谱法测定天然水中Ag、Cd、In、Tl、Cu、Pb、Zn、Co、Ni、Cr、Mn、Fe等12种痕量元素的方法。取水样50ml,预富集10倍,用无火焰法可检测:Ag为0.05μg/L,Cd为0.01μg/L,In为1.8μg/L,Tl为0.4μg  相似文献   

3.
云南墨江金矿床含金硅质岩的地球化学特征和成因   总被引:22,自引:1,他引:21  
应汉龙  蔡新平 《地球化学》1999,28(4):307-317
中石炭统金厂组(C2j)下部含金硅质岩是云南墨江金矿庆的主要围岩之一,具有沉积结构构造,含热水沉积矿物。岩石的FeO、Fe2O3、Au和Ag含量高;Cr、Ni和Co含量高、变化大;MnO/TiO2和TFe/TiO2比值较大;Au含量与NiCr含量相关性低,Au可能不是后期热液作用带入的。在判别硅质岩形成作用的一系列元素和微量元素关系图上,含金硅质岩位于热水沉积作用的范围内或接近于热水沉积作用。岩石  相似文献   

4.
四川会东小街金矿床为川西产于元古宙绿片岩地层中的菱铁矿型金矿床的典型代表。金矿体呈脉状产于中元古界会理群青龙山组碳质板岩、流纹质凝灰岩、变粗面炭和花岗斑岩的内外接触带中,受EW向基底断裂的次级断裂和层间破碎带的严格控制。矿石矿物组合为黄铁矿、毒砂、黄铜矿、黔铜矿族、Au-Ag系列矿物,石英和菱铁矿。其成矿元素组成为Au-Cu-Ag-Pb-Sb-As-Fe。围岩蚀变以硅化、粘土化和碳酸盐化(菱铁矿化  相似文献   

5.
李建平  赖亮 《地质实验室》1997,13(3):185-188
在PH3.5的Britton-Robinson缓冲溶液中,Cu-亚硝基R盐体系在-0.14V可产生较为灵敏的极谱流。二阶导皮高与Cu浓度在0-0.6μg/ml范围内线性关系。检出限为0.003μg/ml,研究了极谱波性质及电极反应机理,证明其为同时受扩散控制的络合附附波本法已用于土壤、人发样中Cu的测定。  相似文献   

6.
汤志勇  敖愫 《岩矿测试》1998,17(4):285-289
建立了一个碱性体系在线氢化物发生原子荧光光谱法测定铜矿石中痕量砷、锑、铋的分析方法。设计了在线氢化物发生流路及操作程序。选择了碱性体系氢化物发生的各项最佳条件,避免了Cu、Fe等大量基体元素的干扰。方法检出限为As0.6μg/L,Sb0.4μg/L,Bi0.9μg/L,As、Sb、Bi的工作曲线均在0~400μg/L内呈良好的线性,经铜矿石国家一级标准物质分析验证,砷锑铋的测定结果与标准值吻合,相对标准偏差(RSD,n=5)在4.2%~8.8%。  相似文献   

7.
周丽沂  张勤 《岩矿测试》1995,14(1):45-48
在0.2mol/L HCl-1.0mol/LNaCl-0.15mol/L抗坏血酸介质中,用电流氧化微分溶出计时电位法直接测定地质物料中微量Cu。富集电位-0.55V,时间20~40s;电极转速2500r/min;溶出电流0.2~1μA;记录电位范围-0.2~-1.20V;清洗电位-0.10V,时间10s。方法检出限0.2μg/g,线性范围2~400ng/ml,精密度(RSD,n=11,4.1μg/  相似文献   

8.
周达孙 《广西地质》1998,11(1):19-24
中国东部地区不同类型的金矿床中大多可见到Au,Ag,Cu,Pb,Zn,As,Hg,Mo等元素的异常,除Mo外,其它元素的异常与Au元素的异常为正相关。各类型矿床的异常元素组合,矿物组合及黄铁矿中微量元素的含量,氧硫同位素变化等均有一定的差异。成矿环境总的来说是富硅或富钙,贫氧的碱性环境。  相似文献   

9.
张生华 《地质实验室》1995,11(5):309-313
留龙金矿床中,大部分金以显微金的形式赋存于黄铁矿和毒砂中,银主要以独立矿形式存在。方铅矿是银的最主要载体矿物。不同矿化阶段的矿石中,金银含量高低与载体矿物的生成世、晶形、粒度和微量隙发育程度有关。Ag和Sb元素有关,与As无明显关系。As是Au的标型指示元素。  相似文献   

10.
本文介绍低温、中等盐分的饱和氧流体中和Au和Ag可溶性的热力学计算结果,基于Au和Ag的溶解度,论证了流体运移的金量取决于原生矿石中Ag的含量。在Ag/Au比值高(1 ̄〉10)的矿石里,流体饱和Ag而不能溶解有地质意义的Au量。在Ag/Au比值低(〈1)的矿石里,流体不饱和Ag而能溶解有地质实际意义的Au和Ag量。当氧化流体向下流动被原生矿石中含Fe^2+矿物还原时,开始沉淀Au和Ag。红土剖面中  相似文献   

11.
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   

12.
Some olistolites reworked in a Tertiary flysch of Mount Parnon (Peloponnesus, Greece) exhibit a Late Permian assemblage, dominated by Paradunbarula (Shindella) shindensis, Hemigordiopsis cf. luquensis and Colaniella aff. minima. This association corresponds to the Late Wuchiapingian (=Late Dzhulfian), a substage whose algae and foraminifera are generally little known. Contemporaneous limestones crop out in the middle part of the Episkopi Formation in Hydra, but they are rather commonly reworked in Mesozoic and Cainozoic sequences. The palaeobiogeographical affinities shared by the foraminiferal markers of Greece, southeastern Pamir, and southern China, are very strong (up to the specific level), and are congruent with the Pangea B reconstructions. To cite this article: E. Skourtsos et al., C. R. Geoscience 334 (2002) 925–931.  相似文献   

13.
PALEONTOLOGY     
正20141596 Liu Yunhuan(School of Earth Sciences and Resources,Chang’an University,Xi’an 710054,China);Shao Tiequan Early Cambrian Quadrapyrgites Fossils of Xixiang Boita in Southern Shaanxi Province(Journal of Earth Sciences and Environment,ISSN1672-6561,CN61-1423/P,35(3),2013,p.39-43,3 illus.,20 refs.)  相似文献   

14.
正20141719 Chen Zhijun(State Key Laboratory of Geological Processes and Mineral Resources,China University of Geosciences,Wuhan 430074,China);Chen Jianguo Automated Batch Mapping Solution for Serial Maps:A Case Study of Exploration Geochemistry Maps(Journal of Geology,ISSN1674-3636,CN32-1796/P,37(3),2013,p.456-464,2 illus.,2 tables,10 refs.)  相似文献   

15.
正20140962 Chen Fenning(Xi’an Institute of Geology and Mineral Resources,Xi’an710054,China);Chen Ruiming Late Miocene-Early Pleistocene Ostracoda Fauna of Gyirong Basin,Southern Tibet(Acta Geologica Sinica,ISSN0001-5717,CN11-1951/P,87(6),2013,p.872-886,6illus.,56refs.)  相似文献   

16.
PETROLOGY     
正1.IGNEOUS PETROLOGY20142008Cai Jinhui(Wuhan Center,China Geological Survey,Wuhan 430205,China);Liu Wei Zircon U-Pb Geochronology and Mineralization Significance of Granodiorites from Fuzichong Pb-Zn Deposit,Guangxi,South China(Geology and Mineral Resources of South China,ISSN1007-3701,CN42-1417/P,29(4),2013,p.271-281,7illus.,  相似文献   

17.
正20141205Cheng Weiming(State Key Laboratory of Resources and Environmental Information System,Institute of Geographic Sciences and Natural Resources Research,CAS,Beijing 100101,China);Xia Yao Regional Hazard Assessment of Disaster Environment for Debris Flows:Taking Jundu Mountain,Beijing as an  相似文献   

18.
正20141266Fan Chaoyan(Guangdong Provincial Key Laboratory of Mineral Resources and Geological Processes,Guangzhou 510275,China);Wang Zhenghai On Error Analysis and Correction Method of Measured Strata Section with Wire Projection Method(Journal of  相似文献   

19.
正20140582 Fang Xisheng(Key Lab.of Marine Sedimentology and Environmental Geology,First Institute of Oceanography,State Oceanic Administration,Qingdao 266061,China);Shi Xuefa Mineralogy of Surface Sediment in the Eastern Area off the Ryukyu Islands and Its Geological Significance(Marine Geology Quaternary Geology,ISSN0256-1492,CN37  相似文献   

20.
正20141810 Bian Yumei(Geological Environmental Monitoring Center of Liaoning Province,Shenyang 110032,China);Zhang Jing Zoning Haicheng,Liaoning Province,by GeoHazard Risk and Geo-Hazard Assessment(Journal of Geological Hazards and Environment Preservation,ISSN1006-4362,CN51-1467/P,24(3),2013,p.5-9,2 illus.,tables,refs.)  相似文献   

设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号