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1.
潘建强  孔佑华 《矿物学报》1993,13(4):293-302
通过对我国64个二八面体含铝蒙皂石矿物化学及晶体化学数据的统计分析,研究了它们的矿物化学及晶体化学的基本特征,并得出八面体组分是影响蒙皂石矿物学及物理化学性质的主要因素,在此基础上,利用AlAl-AlFe-AlMg三角图划分了我国二八面体含铝蒙皂石的晶体化学类型,并对原分类图进行了模式化处理,使AlAl-AlFe-AlMg图更具实际意义,蒙皂石的阳离子交换容量与晶体化学模型有对应性,并受八面体三价  相似文献   

2.
河北沧州地区天然水的氯同位素组成   总被引:3,自引:1,他引:3  
周炼  刘存富 《地球科学》1996,21(5):563-566
利用加速器质谱仪和高精度热离子质谱仪对沧州地区地下水的宇宙成因核素36Cl以及稳定同位素37Cl/35Cl进行了测试,并利用氯同位素有效地确定了沧州地区咸水成因.同时,根据36Cl资料计算出该区第四纪第三含水组(Q2)地下水36Cl年龄为250ka,第四含水组(Q1)地下水36Cl年龄为300ka.  相似文献   

3.
华北晚古生代煤系高岭岩微量元素和稀土元素地球化学研究   总被引:19,自引:4,他引:15  
刘钦甫  丁述理 《地球化学》1998,27(2):196-203
通过华北晚古生代煤系高岭岩微量元素和稀土元素研究,以及利用Ti/Al、Cr/Al、Zr/Al、Ni/Al和Zr/Hf比值,探讨了研究区煤系高岭岩形成时的地质条件和成岩物质来源。  相似文献   

4.
高精度测定稳定氯同位素的制样方法   总被引:1,自引:0,他引:1  
以Taylor和Grimsrud(1969)提出的^37Cl测量的测样原理为基础,介绍了不同地质样品的化学处理方法,研究了CH3I的纯化技术,将AgCl转化为CH3Cl的过程以及用气相色谱(GC)法分离CH3Cl和CH3I的技术。文中详述的制样方法可用来查明近地表地下水和岩石系统中δ^37Cl的天然变化。  相似文献   

5.
河北沧州和山东烟台地区某些天然水的稳定氯同位素组成   总被引:3,自引:1,他引:3  
氯元素有两个稳定同位素:^35Cl(75.77%)和^37Cl(24.23%)。过去一直认为稳定氯同位素的比值(^37Cl/^35Cl)几乎不变。80年代以来利用高精度质谱法成功地发现了自然界氯同位素分馏作用。各地不同深度海水的氯同位素组成极为一致,故以标准平均海水氯(SMOC)作为对比标准。河北沧州和山东烟台地区地下淡水和热水的δ^37Cl为-1.50 ̄+0.80‰,深层油田卤水的δ^37Cl为  相似文献   

6.
原子荧光光谱法测定铜矿中硒和碲   总被引:11,自引:7,他引:11  
张厚兰  郭居媛 《岩矿测试》1993,12(4):287-289
介绍了铜矿中Se,Te的测定方法,样品经HNO3-HClO4分解,以含HClO4的0.2mol/LHCl溶液通过743型阳离子树脂分离Cu,原子荧光光谱法测定Se,Te。  相似文献   

7.
加速器质谱计测定地下水中的36Cl及其应用   总被引:1,自引:0,他引:1  
介绍了加速器质谱计测定36Cl的原理和方法以及应用前景,并对沧州地区第四纪地下水的36Cl进行了测定,利用氯同位素确定了沧州地区的咸水成因,同时根据36Cl资料计算出该区第四系第三含水组地下水的年龄为250ka,第四含水组地下水年龄为300ka。  相似文献   

8.
周炼  蒋菘生 《岩矿测试》1999,18(2):92-96
介绍了加速器质谱计测定^36Cl的原理和方法以及应用前景,并对沧州地区第四纪地下水的^36Cl进行了测定,利用氯同位素确定了沧州地区的咸水成因,同时根据^36Cl资料计算出该区第四系第三含水组地下水的年龄为250ka,第四含水组地下水年龄为300ka。  相似文献   

9.
柴达木盆地氯同位素组成特征   总被引:13,自引:0,他引:13  
刘卫国  肖应凯 《地球化学》1996,25(3):296-303
采用正热电离高精度测定Cl同位素的方法对我国柴达木盆地水体及盐类沉积的Cl同位素组成进行了精确测定,结果表明,柴达木盆地Cl同位素组成存在着明显的变化。各种水体的平均δ^37Cl值顺序为:河水(0.94‰)〉咸水湖水(-0.2‰)〉油田水(-0.62‰)〉盐湖卤水(-0.97‰)。卤水具有低的δ^37Cl值,这是盐湖卤水蒸发析盐的结果。盐湖卤水与共存盐类矿物间的分馏系数为1.0001-1.0021  相似文献   

10.
一种新型高效复合消毒剂:二氧化氯消毒剂虞承伟(地质矿产部山西省中心实验室)1ClO_2为强氧化剂在酸性条件下,ClO_2有很强的氧化性:ClO_2+4H ̄++5e=Cl ̄-+H_2O在水处理条件下(pH=7),ClO_2+e=,E_0=0.95V+2...  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.
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   

16.
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   

17.
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   

18.
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   

19.
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   

20.
正20141266Fan Chaoyan(Guangdong Provincial Key Laboratory of Mineral Resources and Geological Processes,Guangzhou 510275,China);Wang Zhenghai On Error Analysis and Correction Method of Measured Strata Section with Wire Projection Method(Journal of  相似文献   

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