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951.
<正>In order to study the accumulation mechanism of"barkinite",eight Late Permian channel benches(approximately 15-cm across and 10-cm deep) were taken from the Jinshan Mine,Anhui Province,China.The samples were analyzed by microscopical and geochemical methods.The microscopical observations indicate that the occurrence modes of"barkinite"in this area are different from those in other areas of China.The ratios of structureless"barkinite"are much higher in the Jinshan Mine,probably due to the flow-water and marine influenced environments.Furthermore, vitrinite macerals also show a strong fluorescence.The vitrinite fluorescence characteristics have not been observed in the Permian"barkinite"coals from northern China.The composition and variation of minerals in the column section also showed that the swamps in the study area were seriously influenced by seawater in the early and late stage during the peat accumulation. 相似文献
952.
953.
Crustal Composition of China Continent Constrained from Heat Flow Data and Helium Isotope Ratio of Underground Fluid 总被引:3,自引:1,他引:2
Based on conservation of energy principle and heat flow data in China continent, the upper limit of 1.3 μW/m3 heat production is obtained for continental crust in China. Furthermore, using the data of heat flow and helium isotope ratio of underground fluid, the heat productions of different tectonic units in China continent are estimated in range of 0.58–1.12 μW/m3 with a median of 0.85 μW/m3. Accordingly, the contents of U, Th and K2O in China crust are in ranges of 0.83–1.76 μg/g, 3.16–6.69 μg/g, and 1.0%–2.12%, respectively. These results indicate that the abundance of radioactive elements in the crust of China continent is much higher than that of Archean crust; and this fact implies China’s continental crust is much evolved in chemical composition. Meanwhile, significant lateral variation of crustal composition is also exhibited among different tectonic units in China continent. The crust of eastern China is much enriched in incompatible elements such as U, Th and K than that of western China; and the crust of orogenic belts is more enriched than that of platform regions. It can also be inferred that the crusts of eastern China and orogenic belts are much felsic than those of western China and platform regions, respectively, derived from the positive correlation between the heat production and SiO2 content of bulk crust. This deduction is consistent with the results derived from the crustal seismic velocity data in China. According to the facts of the lower seismic velocity of China than the average value of global crust, and the higher heat production of China continent compared with global crust composition models published by previous studies, it is deduced that the average composition models of global continent crust by Rudnick and Fountain (1995), Rudnick and Gao (2003), Weaver and Tarney (1984), Shaw et al. (1986), and Wedepohl (1995) overestimate the abundance of incompatible elements such as U, Th and K of continental crust. 相似文献
954.
针对铜聋山矿区的地质特征及成矿地质条件,应用卫星遥感技术方法对该区进行了综合研究。利用美国陆地卫星Landsat-5的TM多波段数据对研究区的构造信息进行了综合解译,结合主成分分析与波段比值法对矿化蚀变信息进行了提取。结果表明,该区的主要成矿构造为NE向断裂,线环构造的交汇部位是成矿的最佳环境;遥感矿化蚀变信息得到了有效的增强,与已知矿点具有很好的一致性,能够反映有利的找矿目标。 相似文献
955.
956.
957.
详细描述了四川名山建山大邑砾岩实测剖面,讨论了大邑砾岩的岩性组合特征及沉积环境。认为大邑砾岩主要为一套位于风化壳之上的河流-冲积扇沉积,自下而上由细变粗,属于物源区总体不断上升过程中的近源沉积。通过大邑砾岩中的孢粉组合,讨论了其地质时代。该剖面孢粉组合以水龙骨科孢子为主,年代地层归属于新近系上新统。 相似文献
958.
959.
We developed an HPLC method for analysis of the monosaccharide composition of fucoidans.The fucoidan was hydrolyzed into monosaccharides with 2 mol/L trifluoroacetic acid.Using ribose as the internal standard,the monosaccharide derivatives,obtained with 1-Phenyl-3-methyl-5-pyrazolone(PMP),were separated by reverse-phase HPLC using a gradient elution process,and monitored by ultraviolet detection at 245 nm.In the concentration range of 0.1-2.0 mmol/L,the peak area of each monosaccharide had a good linear rel... 相似文献
960.
根据2013—2014年在钦州湾及其邻近海域获取的夏、秋、冬、春4个季节的环境调查资料,分析了表层海水中溶解态重金属的时空变化特征,并运用主成分分析法研究了影响重金属分布的因素。结果表明,Cu、Pb、Zn、Cd、Cr、Hg、As含量范围分别为0.214~1.510、nd~0.979、0.132~4.160、0.005~0.106、0.014~2.580、0.012~0.049、1.2~2.2 μg/dm3,各重金属元素含量均处于历史较低水平;夏、秋季重金属的平均含量依次是As>Cu>Zn>Cr>Pb>Cd>Hg,冬、春季则是As>Zn>Cu>Pb>Cr>Cd>Hg;入海径流量受控于降水,使得雨季时Cu、Zn、Cd、Hg、As的含量通常高于干季;东北季风期间大气沉降可能是Pb含量由夏季到春季逐步增高的主要原因;除夏季Pb、Cd和冬季Pb、Cd、Zn外,其它重金属之间具有显著的同源性。陆源输入是钦州湾及其邻近海域重金属的重要来源,咸淡水混合过程(酸碱度变化及物理混合)是影响重金属分布的最主要因素,潮流作用也是影响重金属分布的重要因素。 相似文献