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1.
中蒙边境沙麦盆地水文地球化学特征与砂岩铀矿预测   总被引:1,自引:0,他引:1  
通过水文地球化学调查,分析了沙麦盆地水文地质条件、水化学类型、放射性异常分布特征,并根据地下水中与铀相关的水文地球化学环境因素等研究,确定了铀的成矿远景区。  相似文献   

2.
黎伟  陈贵海  崔建华 《铀矿地质》2007,23(3):156-163,169
文章通过对找矿目的层铀源、水文地质特征、水文地球化学环境、氢氧同位素特征的分析,阐明了海浪坳陷铀成矿水文地球化学特征,并结合盆地演化史对古水文地质条件进行了初步分析。依据砂岩型铀成矿理论,优选出有利的铀成矿远景地段。  相似文献   

3.
顶山地区铀成矿水文地球化学条件研究   总被引:1,自引:1,他引:1  
谭鸿赞 《新疆地质》2002,20(2):126-129
层间氧化带铀矿床的形成与水文地球化学条件密切相关,本文采用水文地球化学的分析方法,对顶山地区地下水的水文地球化学特征进行了研究,确定了顶山地区下水中铀主要以UO2(PO4)2^2-形式存在,并研究了铀的饱和沉淀条件,指出了铀成矿有利地区。  相似文献   

4.
吐哈盆地水文地球化学分带与铀矿化关系浅析   总被引:4,自引:0,他引:4  
确立了吐哈盆地水中铀的存在形式,分析了铀在水中的迁移规律和沉淀条件。并运用层间氧化带的成矿机理,阐述了各地球化学分带的水文地球化学特征,引用“饱和指数”把铀在水中的饱和程度给予量化,从而确定了盆地水中铀的沉淀区间。利用γNa+/γCl─和γCa++/γCl─划分出水文地球化学分带及综合岩石地球化学分带,为寻找层间氧化带型铀矿提供了水文地球化学依据。指出艾丁湖自流水斜地为形成层间氧化带型铀矿的有利地段。  相似文献   

5.
本文介绍了深部铀矿床勘探中的水文地球化学方法,即应用铅同位素,铀同位素比值,铀活度比值和矿物饱和指数的方法,说细分析了它们的应用范围,找矿效果及各自的局限性,指出在铀矿勘探中不存在万能的水文地球化学方法,而最有效的方法是采用互补的和结合的技术。  相似文献   

6.
郝进庭 《铀矿地质》2013,(1):24-30,46
文章采用PHREEQC模式程序,对研究区地下水的水文地球化学环境进行了模拟,确定水中铀的存在形式、水中沥青铀矿饱和指数(SI)和反应条件指数(RCI)等水文地球化学参数;分析了地层中铀所处状态与水中Eh值、pH值、铀浓度的关系;证明了水的Eh值是控制铀成矿作用的最主要因素;对砂岩型铀矿床的形成及其定位的水文地球化学条件进行了较系统研究和探讨;对砂岩型铀矿成矿水文地球化学机理进行了论证和计算;阐述了铀活化迁移、沉淀富集的本质规律;也为水文地球化学方法研究砂岩型铀矿的成矿预测和矿床定位提供了重要依据。  相似文献   

7.
潮水盆地铀成矿水文地球化学研究   总被引:1,自引:0,他引:1  
在分析潮水盆地自然地理、地质背景及水文地质特征的基础上,对盆地铀成矿水文地球化学特征进行了探讨。结果表明:潮水盆地为-渗入型自流水盆地,其深层地下水中铀存在形式为UO2(CO3)n^2-2n。;从盆地边缘到盆地中心具有明显从氧化环境到还原环境的水文地球化学分带特征,水中铀经历了由溶滤迁移到还原沉淀的矿化过程;在盆地北缘的照壁山-白芨芨、阿右旗-陶家井地区,西南部的平易-平山湖地区具备十分有利的铀成矿条件和良好的铀成矿远景。  相似文献   

8.
蒙其古尔地区水文地球化学特征与铀成矿关系   总被引:3,自引:0,他引:3  
介绍了蒙其古尔地区水动力条件及水文地球化学条件,运用铀水文地球化学理论,分析了铀在水中存在形式.按不同水质类型将该区地下水划分为4个带.利用水成铀矿理论对水文地球化学条件进行分析,为寻找层间氧化带砂岩型铀矿提供了水文地球化学依据.  相似文献   

9.
柴达木盆地西北部铀成矿水文地球化学条件分析   总被引:3,自引:1,他引:3  
陈贤春  李启荣 《铀矿地质》2001,17(6):348-353
根据水成铀矿理论,本文结合研究区水化学特征,论述了柴达木盆地西北部铀成矿水文地球化学条件。冷湖地区具备铀成矿的水化学条件,是形成层间氧化带砂岩型铀矿的有利地区。  相似文献   

10.
水成铀矿床的形成受控于水文地球化学环境的变化,水-岩体系的pH、Eh值和水化学成分的改变是铀富集成矿的关键因素。笔者根据地质、水文及水化学分析资料,应用PHREEQC软件对伊犁盆地蒙其古尔铀矿床三工河组地下水系统中发生的水文地球化学过程进行模拟,以期确定:1)层间水在径流过程中与含水层发生的化学反应;2)水-岩化学反应发生的条件及进行的程度;3)体系中铀的水文地球化学行为及其成矿的有利条件。  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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