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1.
众所周知,金在地壳中的平均含量很低,在岩石矿物中,主要以自然金状态存在。因此无论在从事地质研究,普查找矿和勘探施工中,人们难以用肉眼判断金在岩石矿物中的存在情况,由于金的分析周期长使工作很被动。针对这一情况,本文试验了金的快速鉴定法。 本法基于用泡沫塑料吸附金后,直接用TMK显色的斑点法,进行金的目视测定。还制备了一套模仿标准色阶,以利于长期使用,适合于野外地质人员现场应用。测定范围为0.1—5.0微克金。  相似文献   

2.
野外快速鉴定金   总被引:1,自引:0,他引:1       下载免费PDF全文
众所周知,金在地壳中的平均含量很低,在岩石矿物中,主要以自然金状态存在。因此无论在从事地质研究,普查找矿和勘探施工中,人们难以用肉眼判断金在岩石矿物中的存在情况,由于金的分析周期长使工作很被动。针对这一情况,本文试验了金的快速鉴定法。 本法基于用泡沫塑料吸附金后,直接用TMK显色的斑点法,进行金的目视测定。还制备了一套模仿标准色阶,以利于长期使用,适合于野外地质人员现场应用。测定范围为0.1—5.0微克金。  相似文献   

3.
近年来,作者发展了七种以上重要找矿指示元素的野外快速分析法,此乃其一。文中提出一种新的金样冷浸技术,引进了新的光导光度检测方法,样品经溴化钠—硫酸—过氧化氢冷浸,用经丙酮—MIBK处理的泡沫塑料富集金,经混合解脱剂解脱并直接取解脱液用改进的微珠析出法或用光导光度法测定。取10g样品,可测定0.0005-50g/t范围内的金。方法简便、快速,可在普查分队驻地进行,每一工作日可测定80多个样品,由于废弃了王水分解样品和泡沫塑料的灰化,具有广阔的应用前景。  相似文献   

4.
遥感筛选评价区化异常的初步探索   总被引:1,自引:0,他引:1  
近年来,作者发展了七种以上重要找矿指示元素的野外快速分析法,此乃其一。文中提出一种新的金样冷浸技术,引进了新的光导光度检测方法,样品经溴化钠—硫酸—过氧化氢冷浸,用经丙酮—MIBK处理的泡沫塑料富集金,经混合解脱剂解脱并直接取解脱液用改进的微珠析出法或用光导光度法测定。取10g样品,可测定0.0005- 50g/t范围内的金。方法简便、快速,可在普查分队驻地进行,每一工作日可测定80多个样品,由于废弃了王水分解样品和泡沫塑料的灰化,具有广阔的应用前景。  相似文献   

5.
金的野外快速分析,是金矿地质普查找矿长期探索要解决的一个技术难题,经我们近年来反复实验得到解决。本方法的理论基础可靠,操作简单易学,适用性强,分析成本低。  相似文献   

6.
野外快速测金——目视比色法   总被引:1,自引:0,他引:1  
许晓光 《广西地质》1998,11(4):65-67
文章通过对比实验,总结出了一套野外快速测金的方法-目视比色法,为普查找金提供一个简单,快速,较准确,易掌握的可靠分析方法,并根据此方法做出了“金野外快速分析箱”供野外测金者使用。  相似文献   

7.
以多年逾万件不同金矿区、金矿普查区不同级次含量样品的野外分析测试为依据,提出了对痕量金野外快速测试方法的系统改进,提高了原分析方法的速度和效率,减省了不必要的操作流程,改装了部分设备,使其更易采购和便于携带,在降低劳动强度的同时也不降低分析的精密度和准确度。根据切乔特公式,结合对(超)微细粒金矿的认识提出了针对不同工作目的,痕量金野外快速测试称样的解决方案,既可分析痕量金,也可对目标金矿区作出快速准确的圈定,进而现场指导金矿的勘查开发。  相似文献   

8.
薛光 《岩矿测试》1990,9(4):296-298
黄原酯棉(CCX)是金的良好的吸附体,本文将吸附了金的CCX用灰化法解脱。操作简单快速、成本低,灰化时无臭味、残渣少。浸取液用三正辛胺-TBP(1:3)混合萃取-金试剂液珠比色法测定Au,其液珠凝聚好,灵敏度高,选择性和稳定性都比单用TBP有所提高。方法的测定范围0.0005-xx g/t、配备金的野外快速分析箱,可作现场分析。  相似文献   

9.
我们在学习各地质勘探队先进经验的基础上,经过反复实践,试验了铜、铝、镍、砷现场特快分析方法,装备成68-1野外特快分析箱.此箱经过野外试验,证明它不仅适合于大面积分散流及次生晕普查找矿,而  相似文献   

10.
微珠析出比色法成为九十年代野外地质找矿重要测试手段可实行野外无电,无设备,快速,定量测试金,银,铜,铊等元素的化控样品,地质勘探开发样品,具有广泛的实用价值。  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.
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   

15.
16.
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   

17.
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   

18.
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   

19.
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   

20.
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   

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