1×8DCT图像压缩编码的理论分析和计算机模拟结果

本文首先介绍了正交变换的性质和变换编码的原理，然后将图像序列作为平稳马尔柯夫序列，对１×８ＤＣＴ图像压缩编码作了理论分析和计算机模拟。模拟结果与分析是一致的。     

Banach空间中完全齐次基的一些特性

给出了ｎ－平均规范分块基序列的定义，得到了Ｂａｎａｃｈ空间中完全齐次基的一些等价条件。     

作为投射模的向量空间

Ｒ－模是Ｆ上向量空间的推广，而投射模是一类很重要的模，将投射模的一些性质用到向量空间上去，得到了一些相应结论。     

Fibonacci数列和Lucas数列的若干性质

本文用组合分析中的计算方法得到了关于Ｆｉｂｏｎａｃｃｉ数列的一系列基本性质；同时导出Ｌｕｃａｓ数列的相关结果。     

一类Banach空间范数的单调性

本文给出了一类Ｂａｎａｃｈ格空间范数的单调性及局部一致单调性的条件，进一步得到了该空间是弱序列完备的充要条件。     

Fe_3O_4氧化制备γ－Fe_2O_3磁粉过程动力学

通过对文题的研究，发现反应初期为动力学控制，对［Ｆｅ２＋］为三级反应，频率因子为３．８７×１０１２１ｍｉｎ－１，活化能为１０９．８ｋＪ／ｍｏ１；反应后期为传质控制，对［Ｆｅ２＋］为一级反应，频率因子为５．８７×１０６ｍｉｎ－１，活化能为３５．５ｋＪ／ｍｏｌ。氧分压对宏观反应速率影响不显著，在整个反应过程中反应速率对［Ｏ２］为０．２级反应。还得到了氧化过程的优化串级温度序列。     

关于填补构造——以马角坝地区多级序不协调叠瓦式构造为例

本文根据四川江油马角坝地区大量实例提出的填补构造,是指充填岩层虚脱空间补偿那里压应力不足的层间构造。填补有多种形式。其中,填补褶皱是区别于寄生褶皱的另一类从属褶皱,填补角砾岩是构造角砾岩之一。马角坝地区三个级序的不协调构造中,Ⅱ,Ⅲ级分别是高一级序构造的填补构造,Ⅰ,Ⅱ级为叠瓦式构造,Ⅰ级构造组成的叠瓦式构造是一个大型推覆体上盘系统中的无根薄皮构造。     

序列图象实时消噪声处理中的递归算法

本文针对图象噪声问题,提出了一种适合于实时处理的递归加权算法。该方法运算量小,不增大存贮容量,硬件实现方便,并且通过选取合适的加权系数发,使图象的质量有显著改善。文中简述了最佳加权系数的选择,分析了这种处理方法的性能,并给出了计算机模拟结果。     

Composition of sandstone and heavy minerals implies the provenance of Kuqa Depression in Jurassic, Tarim basin, China

The petrological characteristics and heavy mineral assembly of the Jurassic System in Kuqa Basin are consistent with the tectonic evolution, which is the major factor controlling the filling process of Kuqa Basin. Controlled by the source areas at the both sides of the Basin, the matrixes are dominated by sedimentary rock, high-grade metamorphic rock, acid magmatic rock, and the highest heavy mineral assemblage of zircon-garnet-magnetite in the content. According to heavy mineral indexes, the Jurassic strata can be classified into three rhythmic units of heavy mineral. The lower sequence contains abundant heavy minerals and relatively high content of detritus and its matrixes primarily came form the recycling orogen. The assemblage of “zircon-garnet-magnetite” indicates that the sedimentary area in the early evolution period of the basin is relatively near the provenance. The middle sequence is different from the lower sequence in the heavy mineral assemblage and has the different characteristics from that of source rock. The heavy mineral assemblage is “garnet-zircon” with the highest content of garnet and its main matrices are the high-grade metamorphic rock, acid magmatic rock and hydrothermal vein at the northeastern edge of the basin. The middle and upper sequences are characterized by the clast provenance, which is primarily from the recycling orogen at the northern edge of the basin and secondarily from the southern uplift. As a result of the two provenances, the strata with apparent changes of heavy mineral assemblage and index better coincides with the interfaces of the secondary strata sequences, which reflects the denudation history and the filling process of the orogen at the northern edge of the basin.     

Addition Sequence Method of Scalar Multiplication of Elliptic Curve over OEF

A new elliptic curve scalar multiplication algorithm is proposed. The algorithm uses the Frobenius map on optimal extension field (OEF) and addition sequence. We introduce a new algorithm on generating addition sequence efficiently and also give some analysis about it. Based on this algorithm, a new method of computing scalar multiplication of elliptic curve over an ()EF is presented. The new method is more efficient than the traditional scalar multiplication algorithms of elliptic curve over OEF. The comparisons of traditional method and the new method are also given.