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Music: presentational symbolisim, open symbols can only be understood by the whole, with the relations with others.

音乐元素是表现式的,只有从音乐整体来看这个元素才有意义

The results show that the samples are of calc-alkaline series, the primitive mantle normalized trace element patterns are characterized by relative enrichment in large ion lithophile elements and depletion in high field strength elements (Nb, Ta, Ti, P etc.). REE patterns are of slightly right inclined type with unobvious Eu anomaly.

分析得出样品为钙碱性;原始地幔标准化微量元素分布型式显示相对富集大离子亲石元素K、Rb等,亏损高场强元素Nb、Ta、Ti、P等;稀土元素具有略向右倾的配分型式,且铕异常不明显,显示其具有与消减作用有关的岛弧火成岩的特征。

The gabbro-diorites have high light rare earth elements, low heavy rare earth elements and weakly positive Eu anomalies in chondrite-normalized rare earth element curves, and with high LILEs and relative low HFSEs in primitive mantle-normalized trace element spider diagram.

稀土元素球粒陨石标准化曲线显示其具有富含轻稀土元素、贫重稀土元素以及微弱的Eu的正或负异常的特点。微量元素原始地慢标准化蛛网图上,岩体具富含大离子亲石元素,明显亏损高场强元素(Nb、Ta、Zr、Hf和Ti)等特点。

The geochemical characteristics of basic to intermediate-basic igneous rocks indicate that they belong to a tholeiite suite. Their chondrite-normalized REE patterns are of nearly flat and slightly LREE-enriched type, and their primitive mantle-normalized and MORB-normalized trace element spidergrams are generally similar; the LILEs Cs, Ba, Sr, Th and U are enriched, while Rb and K and the HFSEs Nb, P, Zr, Sm, Ti and Y are depleted. All these show comagmatic evolutionary and genetic characteristics.

基性—中基性岩浆岩的地球化学特征表明其属于拉斑玄武岩系列,稀土元素分布型式呈REE近平坦型—LREE轻微富集型,微量元素原始地幔标准化的蛛网图和MORB标准化蛛网图上的分布型式总体很相似,富集大离子亲石元素Cs,Ba,Sr,Th,U而相对亏损Rb,K和高场强元素Nb,P,Zr, Sm,Ti和Y,显示同源岩浆演化成因特征。

The PGE distributive patterns are the PtPd type, the Pt/Pd ratios of 0.32-0.68 are between the values of enriched sulfide tholeiite (0.38) and primitive upper mantle (1.36), and the similarity of partition patterns of chondritenormalized REE, MORB-normalized trace element and primitive mantle normalized PGE for the rocks of the three phase zones, indicate the Baimazhai intrusive body I formed by the evolution, liquation, intrusion and diagenesismetallogenesis of basaltic magma.

铂族元素配分模式为Pt-Pd型,w/w比值为0.32~0.68,介于富硫化物拉斑玄武岩(0.38)和原始上地幔(1.36)之间,以及稀土元素配分模式、微量元素蛛网图和铂族元素配分模式中不同岩石配分曲线的相似性揭示3个相带不同岩石之间的高度一致性,展示基性-超基性岩形成于玄武质岩浆演化、熔离及岩浆一次性侵入、分异成岩成矿的特征。

Using the estimates of character sums over Galois rings and the trace de scription of primitive sequences over Zpe, we obtain an estimate for the frequency of the occurrences of any element in Zpe in one period of a primitive sequence, which is better than Kuzmin's results[1] if n > 4e, where n is the degree of the generating polynomial of the primitive sequence.

范淑琴 ,韩文报文研究了Zpe上本原序列的元素分布。利用Ga,lois环上的指数和估计和本原序列的迹表示,得到了Zpe中各元素在本原序列的一个周期中出现频率的一个估计。当n>4e时(n为本原序列生成多项式的次数)。我们的估计优于Kuzmin的结果[1]。

In this article author measured the principal element and trace element of Maifanshi with X-ray fluorescence spectrometric method of analysis.

本文用X-射线荧光光谱分析法对麦饭石中的主元素和微量元素进行了测定,测定结果达到检出线的有24种,其中有些是人体所必需的元素

Promethium is number 61 in the periodic table of elements and finds itself most useful in nuclear reactors as an alpha emitter.

钷是元素周期表中第61号元素,在原子核反应堆中作为阿尔法放射源。

Following are summary of our works:(1)The powders of LaCr_(0.9)Co_(0.1)O_3, LaCr_(0.9)Fe_(0.1)O_3, LaCr_(0.9)Ni_(0.1)O_3, LaCr_(0.95)Sn_(0.05)O_3 and LaCr_(1-x)Ti_xO_3(x=0.0-0.3) were single perovskite phase with orthorhombic structure. The gas-sensing properties of their thick film sensors were tested in the acetone, ethanol, normal propyl alcohol, carbinol and formaldehyde organic gases. The sensitivity of the sensors can not be enhanced effectively by doping Co、Fe、Ni、Sn elements in B-site of LaCrO_3. Ti dopant with proper concentration can greatly improve the gas-sensing properties, which make the sensor display higher sensitivity and quicker response-recovery characteristics.

所得结果摘要如下:(1)LaCr_(0.9)Co_(0.1)O_3、LaCr_(0.9)Fe_(0.1)O_3、LaCr_(0.9)Ni_(0.1)O_3、LaCr_(0.95)Sn_(0.05)O_3和LaCr_(1-x)Ti_xO(来源:ABfd1dC论文网www.abclunwen.com)_3(x=0.0-0.3)粉体为正交单相钙钛矿结构,其厚膜型气敏元件在350℃时对丙酮、乙醇、正丙醇、甲醇、甲醛等有机气体的气敏性能测试表明:0.1mol Co、Fe、Ni和0.05mol Sn元素在LaCrO_3的B位进行掺杂后,不能有效提高材料对以上测试气体的气敏性能;而Ti元素的适量掺杂可以极大地改善LaCrO_3的气敏性能,使之显示出对丙酮气体的高灵敏度和快速响应恢复能力。

Because of this, the top and bottom margins of the contained children appear to protrude from the containing element.

因此,包含的子元素的顶部和底部空白边就突出到容器元素的外边。

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