共查询到20条相似文献,搜索用时 859 毫秒
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胶南造山带及邻近地区的重磁场特征及地质解释 总被引:2,自引:0,他引:2
胶南造山带的重磁场特征为一条醒目的重力低、磁力高值带,走向北东-西南,陆上部分长约450m,宽40-70km。其重磁场值一般为0×10^-5m/S^2-20×10^-5M/s^2、0-300nT,反映胶南造山带的轮廓及带内低密度的早元古代晋宁期花岗岩基和中强磁性的中性代燕山晚期岩浆岩的分布。 相似文献
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华北中元古代火山岩Sm—Nd同位素年代及其构造环境的地球化学依据 总被引:2,自引:1,他引:2
刘波 《成都理工学院学报》1996,23(2):35-42
由于缺乏合适的测年对象,华北地区中上元古界的年龄值主要是从沉积财及脉岩中获得。该文据近来从辽北中元古界凡河群中识别出的一套同期喷发玄武岩,获得其Sm-Nd等时线年龄为1199±39Ma.FeO(全-MgO,Ti/100-Zr-Y.3,TiO2-K2O-P2O5,TiO2-Y/Nb和TiO2-Zr图解指地了其大陆内部的裂谷构造环境。^87Sr/^86Sr=0.7030,ε^(T)Nd=-9.5-11 相似文献
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珠江口沉积柱样^210Pb法年龄测定结果及其环境地球化学意义 总被引:22,自引:3,他引:19
提供了珠江河口及河道10个沉积柱^210Pb法的CF模式(稳恒放射性通量模式)和CA模式(稳恒初始放射性模式)的年龄测定结果,并据此讨论珠江三角洲近百年来沉积环境的演化,研究结果表明,西江河道和珠江广州河道1980年以前沉积速率为0.5-1.0cm/a.1980年以后沉积速率增长加快,90年代达到4-6cm/a,沉积通量为4-6g/(cm^2.a)河口沉积速率逐年增长趋势,但一般比河道柱样小得多, 相似文献
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2—胂酸基—4—甲基苯基重氮氨基偶氮苯与镍的显色反应研究及应用 总被引:2,自引:0,他引:2
作者将新合成的显色剂2-胂酸基-4-甲基苯基重氮氨基偶氮苯用于Ni的分光光度分析。在pH11.2的Na2B4O7-NaOH缓冲介质中,非离子型表面活性剂OP存在下,试剂与Ni(Ⅱ)生成组成为2:1的稳定红色配合物,其最大吸收波长位于538nm,表观摩尔吸光系数ε538=1.92×10^5L.mol^-^1.cm^-^1,Ni量在0-0.32μg/ml范围符合比尔定律。用该法测定了铝合金及硫化镍矿石 相似文献
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云南大硐厂铅锌矿床中的硫碲铋矿A 总被引:1,自引:0,他引:1
硫碲铋矿A产于云南省大硐厂铅锌矿床,与自然铋、辉铋铅矿共生。晶体呈柱状,粒度0.02 ̄0.3mm。反光显微镜下呈淡黄色,弱非均质性,反射率Rc′=52.4%,R0=48.8%(波长为540nm),显微压入硬度Hv=46 ̄72kg/mm^2。主要粉晶谱线:3.065(10),2.120(7),1.346(5),2.220(4)。三方晶系,空间群为D3d^5-R3↑-m,晶胞参数a=0.4241nm, 相似文献
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2,4—二溴—6—羧基苯重氮氨基偶氮苯光度法测定痕量铊的研究 总被引:2,自引:0,他引:2
研究了新试剂2,4-二溴-6-羧基苯重氮氨曲偶氮苯与Tl(Ⅲ)的高灵敏显色反应。在非离子表面活性剂TritonX-100存在下,于pH10.5的NH3.H2O-NH4Cl缓冲介质中,Tl(Ⅲ)与该试剂生成红色配合物,其配合物的最大吸收波长位于520nm处,摩尔吸光系数为1.83×10^5L.mol^-^1.cm^-^1。Tl(Ⅲ)量在0-0.64μg/ml范围内符合比尔定律。方法用于废水中痕量Tl 相似文献
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由灰色关联分析、模糊聚类结果,提取出反映四川盆地水化学主要特征的最有效特征指标:二叠系为三维荧光指纹图形、顶空气总烃与重烃、矿化度、Na^+含量、Ca^2+/Ca总、Mg^2+/Mg总;上三叠统为三维荧光指纹图形、顶空气C1-C3的D函数、Li^+/Na^+、矿化度、Ca^2+/Ca总、Mg^2+/Mg总、Na^+含量。由上述特征指标及成因指标δ^18O、水溶甲烷δ^13C,构成了天然气保存的水化 相似文献
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双指示催化光度法测定天然水中痕量锰 总被引:1,自引:0,他引:1
研究表面活性剂在下双指示动力学法测定痕量锰的新方法,考察了测定条件。方法灵敏度较高,ε=7.8×10^7L.mol^-1cm^-1.RSD=2.7%。已用于天然水中痕量锰的测定。 相似文献
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Muriel Rocher Stéphane Baize Stéphane Jaillet Edward Marc Cushing Yannick Lozach Francis Lemeille 《Comptes Rendus Geoscience》2003,335(8):701-708
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
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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
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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
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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
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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
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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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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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正20141768 An Shaopeng(Institute of Rock and Soil Mechannics,Chinese Academy of Sciences,Wuhan 430071,China);Wei Lide Experimental Study on Mechanical Behavior of Xigeda Formation Siltstone and Structure Interface(Journal of Engineering Geology,ISSN1004-9665,CN11-3249/P,21(5),2013,p.702-708,9illus.,1 table,16 refs.) 相似文献
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正20140985Chen Liang(Post-Doctoral Research Station of Mining Engineering,School of Nuclear Resources and Nuclear Fuel Engineering,University of South China,Heng-yang 421001,China);Huang Wei Composition of Major and Correlated Elements with Organic Matters and Paleoclimatic Implication for Lower Paleogene Sediments in Sanshui Basin 相似文献