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71.
辽西地区义县组湖泊沉积层中产出著名的“热河生物群”化石,对于此时期古环境的研究一直是诸多学者关注的焦点.本文对大康堡层湖相纹泥展开研究,重建此时期古环境.通过野外及室内对纹泥组成、类型、厚度等方面的观测,对此时期古气候有了新的认识.纹泥厚度特征变化表明沉积期降水量和沉积速率逐渐减小,统计洪水沉积间纹层数量可指示沉积期洪水事件的频率和规模.结合近现代纹泥形成和保存条件,可知该地区沉积期湖泊水体较深,湖水分层,存在一个缺氧环境,具有较小的表面积/深度比,湖盆形态适合,未受到风的侵扰. 相似文献
72.
《Journal of Natural History》2012,46(1):197-213
An extensive survey of the deep-living fishes of the Catalan Sea (western Mediterranean) recorded 31 species in 19 families and 29 genera from 100 samples at depths between 960 and 2251 m. Chlorophthalmidae, Moridae and Macrouridae accounted for nearly 85% of all specimens taken. In biomass terms, Hexanchidae, Moridae, Alepocephalidae and Chlorophthalmidae were the most important families. A quantitative model of the bathymetric distribution of the species is presented. The ‘centre of gravity’ of species’ distribution and the habitat width, a measure of the distribution heterogeneity, are also given. Out of the 31 demersal species caught, the distributions of only 13 are centered below 1000 m. The Mediterranean deep-sea ichthyofauna is very impoverished in comparison with the adjacent Atlantic Basin fauna. 相似文献
73.
YILINUER Tuhudahong 《科学通报(英文版)》2011,(Z1)
Well-crystallized MgFeSiO4 microparticles were synthesized at different temperatures by a simple molten salt method using KCl flux. As a new cathode for rechargeable magnesium batteries,the material shows a reversible Mg2+ intercalation-deintercalation process. In 0.25 mol/L Mg(AlCl2EtBu) 2/THF electrolyte,MgFeSiO4 synthesized at 900°C can deliver a 125.1 mAh/g initial dis-charge capacity and a 91.4% capacity retention on the 20th cycle at a rate of 0.1C(about 15.6 mA/g) . The results show that MgFeSiO4 cou... 相似文献
74.
在质量比为41.5∶48.5∶10的MgCl_2-KCl-AlF3熔盐体系中加入质量分数为0.6%La_2O_3,利用电解法制备了Al-Mg-La合金.用ICP-OES(电感耦合等离子体光谱仪)和XRD进行了合金的组成和物相分析.研究结果表明,在电解温度800℃,阴极电流密度6.92A/cm2,槽电压5.3~5.4V,电解时间为1h的条件下,电流效率为86.2%,得到的合金主相为α-Mg基体、β-Al12Mg17相与Al11La3相.高的阴极电流密度有利于合金中镁含量的增加. 相似文献
75.
Zircon U-Pb ages of granites at Changba and Huangzhuguan in western Qinling and implications for source nature 总被引:2,自引:0,他引:2
Mesozoic granitoids are widespread in the Qinling-Dabie-Sulu orogenic belt. Precise U-Pb dating on these granitoids can reveal
the evolution of the continental collision orogen and thus provide information on the nature of magma sources. This study
presents zircon LA-ICP-MS U-Pb dating and whole-rock geochemical analyses for two intrusions at Changba and Huangzhuguan in
western Qinling. Zircon U-Pb ages for central and marginal phases of the Huangzhuguang intrusion are 214±1 Ma and 213±3 Ma,
respectively. Zircons from the Changba intrusion yield a dominant cluster with an U-Pb age of 213±2 Ma. Collectively, these
ages are younger than ages of 220 to 240 Ma for ultrahigh-pressure metamorphism due to the continental collision between the
South China Block and the North China Block, corresponding to syn-exhumation magmatism. Some inherited zircons occur in the
Changba intrusion, yielding a weighted mean of 206Pb/238U ages at 757±14 Ma. This indicates that the Changba intrusion has the crustal source of mid-Neoproterozoic ages and a tectonic
affinity to the South China Block. Geochemically, the two intrusuons are both rich in LILE and LREE but depleted in HFSE and
HREE, similar to arc-type igneous rocks. The Huangzhuguang intrusion exhibits linear correlations between SiO2 and the other major oxides, implying chemical evolution from a cognate magma source. It contains mafic enclaves, suggesting
possible mixing of felsic-mafic magmas. The Changba granite is rich in Si and K but poor in Fe and Mg as well as has a high
value of Fe*, suggesting strong differentiation of granitic magma. Therefore, the two intrusions were derived from the Late
Triassic anatexis of the continental crust of different compositions in the northern margin of South China Block. This process
may be coupled with exhumation of the subducted continental crust in the stage of late collision. 相似文献
76.
XinMiao Lü LiPing Zhu Mitsugu Nishimura Yoshimune Morita Takahiro Watanabe Toshio Nakamura Yong Wang 《科学通报(英文版)》2011,56(27):2931-2940
A 380-cm-long sediment core was acquired from the deep water area of Pumoyum Co, southern Tibet. Twenty-five plant residue
samples were selected, and organic carbon stable isotopes were obtained using the AMS 14C chronological method. The 14C age and carbon reservoir effect were calibrated with surface sedimentation rate measurements using 210Pb dating. Results showed that the core sediment deposited over 19 cal ka BP. Based on a multi-proxy analysis of TOC and IC
contents, grain size and pollen assemblage data, the palaeoclimatic evolution of Pumoyum Co was reconstructed since the last
glacial. Pumoyum Co was a shallow lake prior to 16.2 cal ka BP; although the glacier around the lake began to melt due to
increasing temperatures, climate was still cold and dry. In the interval of 16.2–11.8 cal ka BP, the sedimentary environment
fluctuated drastically and frequently. Two cold-events occurred at 14.2 and 11.8 cal ka BP, and these may correspond to the
Older Dryas and the Younger Dryas events, respectively. After 11.8 cal ka BP, Pumoyun Co developed into the deep lake as it
is now. The lake water temperature was relatively lower at that time because of influx of cold water from glacial meltwater
entering the lake. As a result, the multi-proxy indicators showed no sign of warm conditions. Comparisons between the sedimentary
record of Pumoyum Co with that of other lakes of the same age in southern Tibet indicate a warmer climate following the last
deglaciation influenced the southeastern Tibetan Plateau. These results imply that the southwest Asian monsoon gradually became
stronger since the deglaciation during its expansion to the inner plateau. The glacial-supplied water of the lake responded
sensitively to cold-events. The entire southern Tibet region was dominantly influenced climatically by the southwest Asian
monsoon during the Holocene. 相似文献
77.
断陷湖盆扇三角洲、近岸水下扇及湖底扇的识别特征 总被引:3,自引:0,他引:3
根据大量的岩心、测井及化验分析等资料,对板桥凹陷沙三段的沉积相进行了研究,所指近岸水下扇为深湖重力流成因.总结了这几种重要沉积相在岩性、沉积构造、测井曲线、生物化石、沉积序列及沉积组合等几个方面的识别特征,该方法可用于类似断陷型盆地的沉积相研究中. 相似文献
78.
基于傅里叶变换近红外光谱技术,通过主成分分析(PCA),可较好地区分不同品牌的榨菜酱油样本.利用偏最小二乘法(PLS)建立了测定榨菜酱油成分的定量分析模型,校正集样本中总酸、氨基酸态氮和食盐的分析模型决定系数(R2)分别为98.44,98.74和98.48,交叉验证均方差(RMSECV)分别为0.001 3,0.008 44和0.355.预测集样本中总酸、氨基酸态氮和食盐的外部验证决定系数(R2)分别为96.04,95.90,96.27,预测集标准偏差(RMSEP)分别为0.017 4,0.012 9,0.48.实验结果具有较高的预测精度,可以用于测定榨菜酱油主要成分的质量浓度. 相似文献
79.
对采自于山西运城盐湖区白骨顶(Fulica atra)羽毛铅、铜、镉含量进行了测定,并对这几种重金属在各个部位羽毛中的浓度进行了比较.结果表明,白骨顶羽毛的Pb含量为0.53~6.26μg/g、Cu含量为0.56~9.18μg/g、Cd含量0.002~0.24μg/g.铅在白骨顶羽毛中以背羽含量为最高,腹羽最低;铜含量以初级飞羽最高,背羽最低;镉含量背羽最高,腹羽最低. 相似文献
80.
红枫湖水库富营养化现状分析 总被引:3,自引:0,他引:3
根据红枫湖自然环境特点,采用现场调查、地况分析、水样测试以及历史资料综合分析相结合的方法,对其特有的污染源群体进行了不同的分类研究,对红枫湖水体中的污染物来源作详细调查,结果表明:红枫湖近年来主要是氮超标,氮源主要来自于尚末彻底拆除投饵养殖业、入湖的工业废水、湖区居民生活及水上娱乐、自然降水等.其中网箱养殖源是最大的污染源. 相似文献