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1.
应用放射性同位素X射线荧光方法,可以在现场测量金矿中指示元素砷、铜或其他元素的荧光强度。金与其指示元素之间具有相当好的相关性。放射性同位素X射线荧光法利用这种相关性,在普查和勘探金矿体时,通过直接测量指示元素的荧光强度来发现矿化地区和隐伏矿体。使用这种方法在现场不必取样送化学分析,从而加速了地质调查的进程并降低了勘探成本。  相似文献   

2.
应用轻便X射线荧光仪和X射线荧光测井仪,在我国某锑矿上进行了试验.对锑矿粉末样品、锑的化探样品、原始产状锑矿X射线取样、块状岩心及充满泥浆的锑矿钻孔进行了分析测量,并与化学分析比较,结果十分一致.特别是在消除基体效应方面取得了良好的效果. 放射性同位素X射线荧光技术在地质勘探工作中应用的特点是:仪器轻便,射线防护简单,操作容易,便于现场使用,测量速度快,对样品中元素含量能进行定量或半定量测定.在普查找矿阶段,可用来对某些地质远景地段进行及时检查,从而加速岩体评价.在化探工作中,可对中等强度以上的化探分散晕异常地段和水系底部沉积物的淘洗重矿物进行半定量或定量测量,  相似文献   

3.
本文主要介绍了应用 X射线荧光方法在狮子山铜矿进行岩壁 X取样的技术和工作过程 ,提出了一些克服岩壁 X取样影响因素的方法。并对使用效果进行了评价  相似文献   

4.
X射线荧光技术在胶东地区现场勘查金矿的研究   总被引:2,自引:0,他引:2  
应用核物探X射线荧光技术,可以利用轻便型X射线荧光仪在野外原生产状条件下(在土壤中或原生露头上)直接测量,了解金矿的指示元素或指示元素总量(如砷、亲铜元素组和银组)的分布规律。由于金与其指示元素或其总量具有密切的相关关系,而且指示元素的分布范围宽广和深远,因  相似文献   

5.
安庆骧  巢志瑜 《岩矿测试》1992,11(3):252-255
将国家级标样GSR-1至GSR-7研磨至颗粒度<2μm,在大气光路中以光斑尺寸为100μm×l00μm的同步辐射X射线(白光)激发,si(Li)半导体探测器采集荧光信号。研究了这些岩石标样中元素(K、Ca、Ti、Mn、Fe、Zn、Rb、sr、Zr)的X射线荧光强度平均值的相对标准偏差与取样量(点数或面积)的关系,测算了使用这套国家岩石标准样的取样量(点数或面积),并确定了实用的测量方法。为同步辐射X射线荧光微探针扫描技术提供一套(7个)适用的岩石标准样。  相似文献   

6.
利用NITON XL3t 500型便携式X射线荧光光谱仪,选择云南会泽县金牛厂铅锌矿区进行样品分析条件试验.试验中分别对实验室分析与X射线荧光光谱仪分析结果,以及不同湿度条件下分析结果进行了对比研究,确定了最佳的应用条件.结果表明,实验室分析与X射线荧光光谱仪分析结果相近,但湿度因素会降低元素含量.所以应用便携式X荧光光谱仪进行试验不失为一种方便快捷和行之有效的方法.  相似文献   

7.
X射线荧光方法在矿区环境地球化学研究中的应用   总被引:1,自引:0,他引:1  
采用白行研制的高灵敏度能量色散X射线荧光分析仪分析了攀枝花矿区水系沉积物中微量元素的浓度,并根据分析结果研究了矿区元素分布的地球化学特征,本项研究的主要目的是探讨X射线荧光分析技术在矿区环境地球化学研究中的可行性,探索矿区环境地球化学研究的方法技术.结果表明,XRF方法可以有效分析沉积物中元素的含量,进而进行环境地球化学研究.  相似文献   

8.
刘勇  方方  冯民  徐长明 《四川地质学报》2012,32(1):104-105,109
介绍了现场X射线荧光勘查技术的理论基础、仪器设备和运用X荧光分析仪测量伴生或共生元素含量找金的方法应用。应用X射线荧光法在野外现场直接测定多元素含量的变化,列出金与其指示元素之间密切相关关系,可在野外现场圈定金矿远景区和追索隐伏矿体,具有重要意义。  相似文献   

9.
X-射线荧光技术的现场测量,原理基本上和室内样品分析是相同的,这就是根据特征X-射线能量的不同来区别不同的元素,根据元素的特征X-射线强度来测定该元素的含量。  相似文献   

10.
核地球物理勘查技术发展概况   总被引:2,自引:0,他引:2  
章晔 《物探与化探》1997,21(5):321-330
本文简要叙述了80年代以来,国内外发展较快的几种主要核地球物理勘查技术的概况。这些方法有:中微子在地球科学中的应用;应用核技术探测纳米级微粒和气体;航空伽马能谱测量;应用核技术原位测品位并计算线储量(包括X射线荧光辐射取样;中子活化辐射取样和伽马射线辐射取样);地面伽马能谱测量;互射线荧光测井;水底和海底天然放射性方法测量;水底和海底中子活化方法测量;水下X射线荧光测量;核磁共振方法;在工程中应用核技术;反射宇宙中子法;以及在环境科学中应用核技术等。  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.
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   

15.
HYDROGEOLOGY     
正20141756 Chen Ruige(Mathematical College,China University of Geosciences,Beijing100083,China);Zhou Xun Numerical Simulation of Groundwater Level Fluctuation in a Coastal Confined Aquifer with Sloping Initial Groundwater Level Induced by the Tide(Geological Bulletin of China,ISSN1671-2552,CN11-4648/P,32(7),2013,p.1099-1104,6 illus.,16 refs.) Key words:confined water,groundwater level  相似文献   

16.
正20141408 Cai Jia(Institute of Geology,Chinese Academy of Geological Sciences,Beijing100037,China);Liu Fulai Petrogenesis and Metamorphic P-T Conditions of Garnet-Spinel-Biotitebearing Paragneiss in Danangou Area,Daqingshan-Wulashan Metamorphic Complex Belt(Acta Petrologica Sinica,ISSN1000-0569,CN11-1922/P,29(7),  相似文献   

17.
18.
正20142386An Guoying(China Aero Geophysical Survey and Remote Sensing Center for Land and Resources,Beijing 100083,China)Application of Satellite Remote Sensing in Regional Hydrogeological Investigation:Taking Cenozoic Strata in Wenquan Sheet(1∶250 000)of Karakoram Range as an Example(Geosci-  相似文献   

19.
正20141016An Chengbang(Key Laboratory of Western China’s Environmental Systems,Ministry of Education,Lanzhou University,Lanzhou 730000,China);Zhao Yongtao Lake Records during the Last Glacial Maximum from Xinjiang,NW China and Their Climatic Impli-  相似文献   

20.
正20141538 Cao Qing(School of Earth Sciences and Engineering,Xi’an Petroleum University,Xi’an 710065,China);Zhao Jingzhou Characteristics and Significance of Fluid Inclusions from Majiagou Formation,Yichuan Huangling Area,Ordos Basin(Advances in Earth Science,ISSN1001-8166,CN62-1091/P,28(7),2013,p.819-828,7 illus.,3 tables,43 refs.)  相似文献   

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