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1.
钟良水 《江西地质》1997,11(1):52-59
文中概述了江西九瑞武山铜金矿床(体)地质特征,建立了块状硫化物型、矽卡岩型,斑岩型铜金矿床(体)综合信息找矿模式;运用数学地质方法着重分析研究了武山铜金矿床不同类型矿体的空间变化规律,介绍了矿床(体)立体定量预测及靶区优选的找矿预测效果  相似文献   

2.
江西银山九区南段铜硫金矿床地质特征   总被引:1,自引:0,他引:1  
刘小滨 《江西地质》1997,11(3):28-33
九区南段铜硫金矿床位于江西银山矿九区铜硫金矿床的南段,为一隐伏矿床。本文在前人资料的基础上,根据钻孔和现场施工的见矿情况,探讨了九区南段铜硫金矿床的地质特征。  相似文献   

3.
研究表明黄狮涝山铁帽型金矿床、马山金(硫)矿床和金口岭铜金矿床的勘查史表明,物探工作特别是磁测发挥了重要的作用。  相似文献   

4.
<正>流沙山钼金矿床属于斑岩矿床,相对于斑岩铜金矿床、斑岩铜钼矿床来讲比较少见,又由于钼和金的化学及物理性质差异比较大,钼金伴生成矿比较难,所以说通过对成矿区地质背景等相关的描述,分析流沙山钼金矿床的成因,为以后的找矿工作提供新的思路,由于钼金矿床的稀少,笔者大胆的提出猜想:斑岩型钼金矿床其实是在斑岩型铜(钼)矿床基础上被含金热液穿插侵入形成的或者是斑岩型铜金以及铜钼矿床的叠加作用产生的这种矿床。即在流沙山钼金矿床附近很可能会有铜矿有待发现。  相似文献   

5.
紫金山铜金矿床地质地球化学特征   总被引:20,自引:5,他引:20       下载免费PDF全文
张江 《地质与勘探》2001,37(2):17-22
紫金山铜金矿床具有“上金下铜”的垂直分带特征,近矿围岩存在一套中低温热液蚀变,金矿与强硅化关系密切,铜矿与硅化一明矾石化关系密切,下部伴生金的铜矿床属岩浆期后中低温高硫热液型矿床,上部金矿床属岩浆期后中低温-低温高硫热液-氧化次生富集叠加型矿床。  相似文献   

6.
通过对白弄铜金矿床详细的地质构造背景、含矿岩石及产出特征等研究表明,测区班怒结合带内铜金矿不具有斑岩型矿床特征,其与班怒洋在早白垩世双向俯冲、碰撞形成的闪长岩、石英闪长岩关系密切,依此把测区内班怒结合带内的铜金矿床确定为白弄闪长岩型-矽卡岩型铜金矿床,进一步完善了班怒结合带西段铜金矿矿床的类型,为今后在班怒结合带内寻找铜金矿矿床提供了新的资料。  相似文献   

7.
阿尔金成矿带主要金属矿床地质地球化学特征及成因初探   总被引:7,自引:1,他引:7  
本文简要介绍了阿尔金成矿带近年来发现的主要金属矿床的地质地球化学特征,研究了矿床S、Pb、H、O等同位素地球化学,测定了部分矿床的流体包裹体成分和温度,并在此基础上讨论了矿床的成因。该带主要矿床类型有火山喷流块状硫化物铅锌铜多金属矿床(喀腊大湾)、叠加改造型铅锌铜多金属矿床(更新沟和拉配泉)、斑岩型铜矿床(索拉克)、卡林型金矿床(祥云和盘龙沟)、与火山作用有关的浅成低温热液金矿床(采石沟)、韧性剪切带型金矿床(红柳沟)、与钾长花岗岩侵入作用有关的热液金矿床(大平沟)等。  相似文献   

8.
<正>1 IOCG的定义IOCG矿床是英文Iron Oxide-Copper-Gold矿床的缩写,中文翻译为铁氧化物铜-金矿床或氧化铁铜-金矿床。铁氧化物铜金矿床(IOCG)于1992年被正式提出(Hitzman et al.,1992),是目前全球最新的重要矿床类型。经过20年的发展,正与斑岩型、VMS、SEDEX、MVT等矿床类型一样被大家广为所知。Williams et al.(2005)提出了一个基于实践经验的定义,他认为IOCG矿床具有以下特征:(1)成矿元素以铜为主,  相似文献   

9.
江西九瑞地区铜金成矿系列模式   总被引:11,自引:0,他引:11  
崔彬 《矿床地质》1995,14(1):44-50
九瑞铜金矿田是长江中下游铁,铜金在矿带的一个重要组成部分。区内不同的沉积建造,由于其物理化学性质的不同,控制了不同类型矿床的形成(斑岩型,隐爆角砾岩型、层控型、矽卡岩型和石英脉型等);区内岩浆的演化控制了不同的矿种(铜、金、钼等)它们互相叠加组合构成了区内不同矿床类型和不同矿化种类的矿床及其组合(斑岩型铜、钼矿床、隐暴角砾岩型铜、金矿床、矽卡岩型铜钼矿床、层控型铜、金矿床以及矽卡岩型-层控型矿床组  相似文献   

10.
鄂东鸡冠嘴铜(铁)金矿床的地质特征及成因   总被引:5,自引:0,他引:5  
本文通过对鸡冠嘴铜(铁)金矿床的地质特征及成矿机制的研究,认为该矿床明显受构造,地层和岩浆活动控制,在时空及成因上具有“一体多矿”、“一体多带”的成矿特点,为高、中温热液-接触交代矽卡岩型铜(铁)金矿床。  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.
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   

13.
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   

14.
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   

15.
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   

16.
17.
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   

18.
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   

19.
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   

20.
GEOCHEMISTRY     
正20142002 Wei Hualing(Institute of Geophysical and Geochemical Exploration,Chinese Academy of Geological Sciences,Langfang065000,China);Zhou Guohua Element Content and Mineral Compositions in Different Sizes of Soil in Tongling Area,Anhui Province(Geological Bulletin of China,ISSN1671-2552,CN11-4648/P,32(11),2013,p.1861  相似文献   

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