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1.
首次确认区内金红石的主要矿化层位为毛集群左老庄组一段地层,主要矿化集中区位于南召云阳—方城清河间30 km地段,并在宽坪群中也发现了新的矿化层位和矿化类型.首次发现大型粗粒易选矿体,突破了前人“呆矿”的结论.预测区内50 m以浅范围内金红石资源总量大于5 000万吨,为一世界级的超大金红石矿产地.  相似文献   

2.
东秦岭褶皱带河南段发现超大型金红石矿床   总被引:1,自引:0,他引:1  
首次确认区内金红石的主要矿化层位为毛集群左老庄组一段地层,主要矿化集中区位于南召云阳一方城清河间30km地段,并在宽坪群中也发现了新的矿化层位和矿化类型。首次发现大型粗粒易选矿体,突破了前人“呆矿”的结论。预测区内50m以浅范围内金红石资源总量大于5000万吨,为一世界级的超大金红石矿产地。  相似文献   

3.
首次确认区内金红石的主要矿化层位为毛集群左老庄组一段地层 ,主要矿化集中区位于南召云阳—方城清河间 30km地段 ,并在宽坪群中也发现了新的矿化层位和矿化类型。首次发现大型粗粒易选矿体 ,突破了前人“呆矿”的结论。预测区内 5 0m以浅范围内金红石资源总量大于 5 0 0 0万吨 ,为一世界级的超大金红石矿产地。  相似文献   

4.
对上庄与夏甸金矿的含矿花岗岩、绢英岩以及黄铁绢英岩中的金红石化学成分标型特征进行了详细的研究,探讨了其中Fe、Si、Ti、W元素含量变化的规律。研究表明,上庄金矿与夏甸金矿中的金红石为变质成因,主要通过黑云母蚀变释放Ti而形成金红石,此类金红石主要赋存在黑云母的边缘、解理及裂隙之间。金红石中Ti含量存在由绢英岩向黄铁绢英岩的下降趋势。矿体周围能够形成Ti晕,可作为强烈矿化的标志。另外,金红石中W的含量从花岗岩到绢英岩再到黄铁绢英岩呈现不断富集的趋势,表明金红石中W的含量变化可指示金矿化的强弱,高W金红石的出现指示金矿的形成,这为胶东金矿的找矿研究提供了新的思路。  相似文献   

5.
首次在陕西省镇安下寒武统水沟口组地层中发现了铌(钽)金红石矿化层,该层赋存于下寒武统水沟口组第一岩段(C-s1)中的方解石绿泥石绢云母片岩层中,严格受层位控制,延伸较稳定。  相似文献   

6.
山西代县碾子沟金红石矿床地质特征及经济意义研究   总被引:5,自引:0,他引:5  
金红石在国民经济中用途广泛,我国每年需要大量进口.山西碾子沟金红石矿床位于五台西段草垛山分岭背斜南翼,金红石矿体赋存于碾子沟上段地层中,矿体产状与地层产状一致,矿体规模、产状和形态严格受岩体控制,矿化是吕梁期热液活动强烈影响的结果,使得金红石叠加富集.矿床含矿岩石主要为阳起透闪岩、绿泥透闪岩等.金红石呈半自形粒状结构,多分布于透闪石矿物之间.采用金红石(TiO2)边界品位1.0%、工业品位1.6%计算,共求得金红石(TiO2)资源/储量163万t,属于大型矿山.  相似文献   

7.
查册桥矿区位于江南过渡带,包括牛头高家金矿床、程檀金矿床、路源金矿点和东边金矿化点、杨梅尖金矿点.其中牛头高家金矿是安徽省首次发现的具一定规模的红土型金矿.研究区主体位于东至断裂与高坦断裂带交汇处及其两侧,三岗尖-杨美桥背斜核部及北翼.区内存在多个重要的赋矿层位,主要包括南华系休宁组、南沱组,震旦系蓝田组,寒武系黄柏岭组、杨柳岗组,奥陶系仑山组、东至组.高坦断裂带、兰程畈断裂带、奥陶系/志留系间的推覆-滑覆断层界面均是重要的控岩控矿构造,区内岩浆岩主要受其控制,物化探异常也主要沿其分布.通过对矿床地质特征总结,并结合前人研究成果,对找矿潜力进行分析,认为区内具有寻找低温热液型-叠改型、层控夕卡岩型、岩浆热液脉型金、铜、钨、钼、银、铅锌等矿化的潜力.  相似文献   

8.
金红石是TiO2的高温高压相变体,在工业上具广泛用途.我国钛资源丰富,储量居世界首位,但其中98.9%是钛铁矿,金红石仅占1%左右(王立平等,2004),因此,金红石资源在我国十分紧缺.上世纪80年代后期以来,在江苏北部新沂-东海一带的榴辉岩中陆续发现了重要的金红石矿床,资源总量达数千万吨(黄建平等,2003),最近实施的中国大陆科学钻探工程(Chinese Continental Scientific Drilling,简写为CCSD)进一步揭示东海地区金红石矿床具有层位多、厚度大、品位高等特点(徐珏等,2004),因此,苏北新沂-东海一带有望成为我国原生金红石矿床的又一重要产地.本文以CCSD主孔0~2000m岩芯中的榴辉岩为对象,通过对榴辉岩中主要造岩矿物(石榴石和绿辉石)、以及榴辉岩全岩化学组成的全面分析,系统对比了高钛(TiO2>2%)与低钛(TiO2<2%)榴辉岩元素组成特征的差异,并据此探讨了该区榴辉岩型金红石矿床成矿的地球化学制约因素.  相似文献   

9.
内蒙古中部大青山东段二道洼岩群分布区金矿找矿方向   总被引:2,自引:0,他引:2  
古元古代二道洼岩群分布区已发现一批金矿床和金矿化点。它们均赋存于该岩群上部层位内。主要控制金矿成矿的因素为层位 +岩性 +剪切变形变质带。因此只要有该岩群上部层位的存在 ,又有金化探异常 ,那就可能找到新的金矿床。  相似文献   

10.
安徽金寨县沙坪沟钼矿区铌赋存状态研究   总被引:1,自引:0,他引:1  
阳珊  王波华  王枫  遇祯 《岩矿测试》2013,32(2):269-277
安徽金寨县沙坪沟特大型钼矿在勘察过程中发现部分样品的铌含量达到100~350μg/g,钽矿化不明显,目前该矿床即将结束勘探工作,查明铌、钽的赋存状态及其有关物质组分,以确定其是否为钼矿伴生矿床是本文研究的重要内容.本文对矿区的样品应用化学分析、光薄片岩矿鉴定、单矿物分析、电子探针分析等大型现代仪器相结合的分析手段,研究了岩石中铌、钽的赋存状态.化学分析确定钼矿体上部石英正长岩及碱长花岗斑岩中铌平均含量为172.9 μg/g,钽平均含量为10.6 μg/g;钼矿体中正长岩及花岗斑岩中铌平均含量为84.5 μg/g,钽平均含量为5.2 μg/g.该分析表明本区为单一原生铌矿化,且铌矿化主要发生在钼矿体上部石英正长岩中;偏光显微镜下观察未发现独立铌钽矿物.单矿物及电子探针分析结果显示铌主要赋存于榍石蚀变的金红石中,钽矿化不明显.金红石呈它形粒状-半自形板状,结晶粒度<0.2 mm,集合体呈榍石假象,Nb2O5平均含量为9.224%.铌在各矿物中的分配计算显示,金红石中铌占有率为75.13%.综合分析表明本区铌钽矿化强度弱,不具有工业价值,不能成为钼矿的伴生矿种选矿开采.  相似文献   

11.
CSAMT 法在辽西康杖子区深部探矿中的应用   总被引:5,自引:0,他引:5  
于泽新 《地质与勘探》2009,45(5):600-605
可控源音频大地电磁法(CSAMT)具有探测深度大、横向分辨率高、抗干扰能力强的特点,在深部找矿勘探中有着重要的指导意义。肖家营子铜钼矿床是辽西地区一个大型矽卡岩型金属矿床,大部分矿体是隐伏矿体,矿区外围的康杖子区与本区有相似的成矿地质环境,成矿地质条件优越.矿体与围岩电性差异明显,通过应用CSAMT,矿体具有低电阻特点,根据成果推断解释,对深部有利成矿部位进行了钻探验证,取得了理想的探矿效果,在矿区外围取得第二深度空间找矿重大突破。  相似文献   

12.
13.
Julie Okpala 《GeoJournal》1990,20(1):37-43
This paper traces the development of geographic education in Nigeria and examines the views of geographers, other academics, students and the public at large about the importance of geography. Geography's value is immense despite the non-professional nature of the discipline. Nevertheless, there is a need to define geography's status and ensure career prospects for students. The Nigerian Geographical Association (from classroom teaachers to top geographers) must promote geography, improve its status in schools and universities, and continuously restructure its content and methods to address pertinent social needs.  相似文献   

14.
Trends in landslide occurrence in Nepal   总被引:2,自引:0,他引:2  
Nepal is a mountainous, less developed kingdom that straddles the boundary between the Indian and Himalayan tectonic plates. In Nepal, landslides represent a major constraint on development, causing high levels of economic loss and substantial numbers of fatalities each year. There is a general consensus that the impacts of landslides in countries such as Nepal are increasing with time, but until now there has been little or no quantitative data to support this view, or to explain the causes of the increases. In this paper, a database of landslide fatalities in Nepal has been compiled and analysed for the period 1978–2005. The database suggests that there is a high level of variability in the occurrence of landslides from year to year, but that the overall trend is upward. Analyses of the trends in the data suggest that there is a cyclicity in the occurrence of landslide fatalities that strongly mirrors the cyclicity observed in the SW (summer) monsoon in South Asia. Perhaps surprisingly the relationship is inverse, but this is explained through an inverse relationship between monsoon strength and the amount of precipitation in the Hill District areas of Nepal. It is also clear that in recent years the number of fatalities has increased dramatically over and above the effects of the monsoon cycle. Three explanations are explored for this: land-use change, the effects of the ongoing civil war in Nepal, and road building. It is concluded that a major component of the generally upward trend in landslide impact probably results from the rural road-building programme, and its attendant changes to physical and natural systems.  相似文献   

15.
2010年,美国铀矿总共施工7 209个钻孔,总进尺1 493 520 m;生产铀1 628.55 t;铀矿业总支出费用为2.773亿美元,其中铀矿地勘费支出为3 450万美元,占铀矿业总费用的12.44%。铀矿地勘钻探费用为4 460万美元,占铀矿业总费用的16.08%。  相似文献   

16.
硫代砷是富硫化物地下水中砷的重要形态,对环境和人类健康有潜在威胁。目前硫代砷研究程度尚低,本次主要针对国内外地下水(地热水)中硫代砷的存在形态,水文—生物—环境地球化学过程,样品保存,定量检测方法等方面进行研究。结论如下:pH, 氧化还原电位,硫化物含量和微生物作用等是影响地下水中硫代砷稳定存在和形态分布的重要因素。含铁矿物能与水中的硫代砷形成配位键对其进行吸附,吸附性普遍弱于(亚)砷酸盐,因此,地下水中硫代砷可能表现出更强的迁移性。用于硫代砷检测的自然水样在采集中可采取过滤,速冻,厌氧和低温短期保存的操作流程,以减缓该形态的转化甚至消失。色谱联用ICP-MS系统可用于自然水样中硫代砷的分离定量检测,紫外—可见分光光度法和X射线吸收光谱法在不同场景下也可对硫代砷进行定量和表征分析。地热水和浅层地下水中均可能存在硫代砷,由于水样中硫代砷的不稳定性,室内检测和分析难以准确反映现场过程,因此,野外样品保存技术和现场检测方法的更新可能在未来有更大研究空间,值得进一步探索。  相似文献   

17.
通过对泰安市岱岳区花岗岩地区地下水的形成条件、地下水类型、分布状况、水文地质特征以及地下水补给、径流、排泄条件的分析,指出了花岗岩地区供水方向。  相似文献   

18.
Conclusions During the last ten years, aquaculture, especially mariculture has undergone remarkable expansion to counter-balance the gap between the supply and demand of fishery products in Japan. Its expansion has also been supported by the traditional preference of the Japanese people for seafood. Mariculture is now being forced to change its structure due to adverse economic circumstances such as the rise in the cost of energy, feeds and other materials for culture, low market prices, deterioration of environmental conditions, and many other factors. Before these constraints can be resolved, advanced scientific knowledge and technologies must be integrated to develop new types of aquaculture. Expansion of maricultural activities to more open-sea and off shore areas would be one route to follow. Technologies for the development of formulated diets not only for young but also for adults and larvae, establishment of feeding standards, prevention of epizootic diseases must support the establishment of modern aquaculture.The culture-based fisheries, or marine ranching, is becoming a subject for further development in Japan. Much research work has been conducted with a great degree of governmental support. Establishment of a net work of seedstock production farms has made it possible to carry out releasing experiments on a large scale. A newly integrated restoration system could be developed on the basis of these experiments, even though the profits resulting from the artificial restoration of stocks is not thouroughly verified at present. The commencement of a national scheme for culture-based fisheries would be a manifestation of the enthusiasm of the Japanese fish industry.  相似文献   

19.
Radon is a radioactive gas emanating naturally from uranium rich granites and shales. It may be emitted from the ground surface into the atmosphere as a gas, or it may be dissolved into stream water and transported over distance. The levels of radon gas in soils at ground surface depend on a number of factors relating to the source of the gas and to its transmission. Igneous rocks contain the highest mean concentrations of radium and uranium. The depth of cover is relevant also. Surveys over the years by the National Radiological Protection Board (NRPB) and others have indicated that the highest concentrations in the United Kingdom occur in Cornwall, Devon and northeast Scotland. However, recent reports have indicated that high concentrations of the gas may be detected in small pockets in counties outside of those considered at high risk. This survey relates to a series of measurements taken in and around Darlington, County Durham. The results showed the presence of small areas with strong concentrations of radon in soil gas, but only minor levels of dissolved gas in stream waters.  相似文献   

20.
内蒙古苏尼特地下水氟污染形成机理研究   总被引:4,自引:1,他引:3  
为了研究内蒙古苏尼特地区地下水氟污染机理,本文运用水文地球化学分类方法,从水文地质、水化学特征两方面研究其地下水的水质特征、氟的起源、分布规律及污染形成机理。研究结果发现:高氟地下水的主要水质类型为HCO3—Na型,pH值在7.08~9.38之间,氟浓度与井深有关,即井越浅,氟浓度越高;地下水中氟浓度最高达14.78mg/L,5~9月地下水氟浓度相对增长率在7.8~23.1之间;F-浓度与Li+、Br-相关系数达0.89和0.82,受断层影响的深层地下水中F-浓度几乎与Li+、Br-没有相关关系,这暗示着氟来源于浅部,并受到强烈的蒸发作用影响而使水中的氟浓缩;地质调查发现该地区还有数个萤石矿存在,显微镜分析结果证实表层土壤中普遍存在CaF2,地下水中的氟来自CaF2。高氟地下水存在于潜水层,深部含水层的地下水可供开采。从断层带涌出的水对潜水层有稀释作用。  相似文献   

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