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The main contributions of the second part of this dissertation are focused on the cryptographic properties of logical functions over finite field, with the help of the properties of trace functions, and that of p-polynomials, as well as the permutation theory over finite field: The new definition of Chrestenson linear spectrum is given and the relation between the new Chrestenson linear spectrum and the Chrestenson cyclic spectrum is presented, followed by the inverse formula of logical function over finite field; The distribution for linear structures of the logical functions over finite field is discussed and the complete construction of logical functions taking on all vectors as linear structures is suggested, which leads to the conception of the extended affine functions over finite field, whose cryptographic properties is similar to that of the affine functions over field GF (2) and prime field F〓; The relationship between the degeneration of logical functions and the linear structures, the degeneration of logical functions and the support of Chrestenson spectrum, as well as the relation between the nonlinearity and the linear structures are discussed; Using the relation of the logical functions over finite field and the vector logical functions over its prime field, we reveal the relationship between the perfect nonlinear functions over finite field and the vector generalized Bent functions over its prime field; The existence or not of the perfect nonlinear functions with any variables over any finite fields is offered, and some methods are proposed to construct the perfect nonlinear functions by using the balanced p-polynomials over finite field.

重新定义了有限域上逻辑函数的Chrestenson线性谱,考察了新定义的Chrestenson线性谱和原来的Chrestenson循环谱的关系,并利用一组对偶基给出了有限域上逻辑函数的反演公式;给出了有限域上随机变量联合分布的分解式,并利用随机变量联合分布的分解式对有限域上逻辑函数的密码性质进行了研究;给出了有限域上逻辑函数与相应素域上向量逻辑函数的关系,探讨了它们之间密码性质的联系,如平衡性,相关免疫性,扩散性,线性结构以及非线性度等;讨论了有限域上逻辑函数各类线性结构之间的关系,并给出了任意点都是线性结构的逻辑函数的全部构造,由此引出了有限域上的"泛仿射函数"的概念;考察了有限域上逻辑函数的退化性与线性结构的关系、退化性与Chrestenson谱支集的关系;给出了有限域逻辑函数非线性度的定义,利用有限域上逻辑函数的非线性度与相应素域上向量逻辑函数非线性度的关系,考察了有限域上逻辑函数的非线性度与线性结构的关系;利用有限域上逻辑函数与相应素域上向量逻辑函数的关系,揭示了有限域上的广义Bent函数与相应素域上的广义Bent函数的关系,以及有限域上的完全非线性函数与相应素域上向量广义Bent函数之间的关系;给出了任意有限域上任意n元完全非线性函数存在性与否的完整证明,并利用有限域上平衡的p-多项式的性质给出了有限域上完全非线性函数的一些基本构造方法。

We make use of a normal element and circular permutations to construct polynomials over the intermediate extension field between F_q and F_ denoted by F_ where s divides t. The polynomials we constructed are F_q-linearly independent and return elements in F_q when they are evaluated at elements of the extension fields.

结合Reed-Solomon码的构造特点,我们将Chaoping Xing与San Ling所构造的线性码的方法推广到有限域的任意次扩张上,首先利用正规元和循环排列来构造系数属于F_q和F_q的任意次扩域F_之间的中间域的具有特殊性质的多项式,中间域记为F_,其中s为t的真因子,由正规元的选择可以保证所构造多项式的F_q-线性无关性,并且这些多项式在扩域F_中取值都属于F_q,从而构造出一类q元线性码。

Located in the west Liaoning province,jin 45 region is on the second fault bench of the huanxiling monoclinal structure,which is on the west pitch of liaohe fault basin.

中文摘要:锦45块地处辽宁省凌海市闫家镇大有地区,其构造上位于辽河断陷盆地西部凹陷西斜坡欢喜岭单斜构造带的第二断阶带上。

And these folds could be produced by the orogeny movement acting in the early Paleozoic.

然而这并不表明我们已经完全准确地认识了该构造带,恰恰相反,在一些问题上还存在着许多争论,如对早古生代该地区的构造变动及样式认识不清,对鄂尔多斯西缘逆冲褶皱带缺乏统一的认识等等,这些都直接影响到对该构造带的正确认识,因此对该构造带的研究还有待于进一步的深入。

The generally southward paths for oil to migrate out of Taibei depression can be two ways. One of them is from Taibei depression to Yubei structural zone and the other is from Taibei depression to Lukeqin structural zone. By the both ways, oil migrated upward along the faults and southeastward along the structural axis to concentrate in either Permian or Triassic system.

油气运移路径的总趋势,一是由台北凹陷由北往南运移直抵玉北构造带,再沿断层向上进入二叠系和三叠系运载层,二是由台北凹陷运移至鲁克沁构造带西端进入三叠系运载层,进入两构造带的油气沿构造轴部由西北向东南上倾方向运移。

Based on core measurements from IODP expedition 316 of the first stage of the NanTroSEIZE program, we analyze deformational and sedimentary structures at the core scale at four sites, C0004, C0006, C0007 and C0008, at the toe the accretionary prism along the Nankai Trough. We also discuss the relationships between structures at the core scale and large scale structures like splay fault and frontal thrust fault.

通过参加IODP的日本南海海槽发震带研究项目第一阶段316航次所收集到的大量第一手数据和资料,分别在4个站位上(C0004,C0006,C0007,C0008)对日本南海海槽增生楔前缘岩芯尺度上的构造变形进行了详细分析,并且讨论了岩芯尺度上的构造变形与增生楔中大尺度的非序列分支逆冲断层和前缘逆冲断层的构造变形之间的关系。

Five types of traps, including compressional, extensional, shearing, gravitative and strata litholoical types, were divided on studying the feature of different tectonic movements , seismic sequences and depositional property in Wan an Basin.

作者在分析该含油气区地质构造特征、地层划分和沉积特征的基础上,划分了压缩型、伸展型、剪切型3 种构造类圈闭和重力、地层-岩性两种非构造型的圈闭,并选用南、北两条典型地震剖面模拟了典型圈闭形成过程及其与构造运动之间的演化关系,可为在该区中寻找同类型含油气圈闭和进行构造演化史的研究提供可靠依据。

Based on the field deposit-geological investigations, structural analysis and petrochemistry studies, this paper presents a Miocene intraplate thermo-upwelling extensional metallogenic model of the Zhunuo porphyry copper deposit which is tectonically controlled by the nearly east-west and north-south extensive faults related to lower crustal flow. The ore-bearing porphyries have the characteristics of typical adakitic rock.

野外基础地质和矿床地质调查、构造分析和岩石化学的研究表明,朱诺斑岩铜矿床在构造上受近EW向和近SN向伸展断裂控制,时间上属于中新世青藏高原南部板内构造过程,含矿斑岩具有典型的埃达克质岩特征。

Combining the actual rockburst status after excavation, based on the previous research data in the earlier stage, the character of the tectonic stress in Cangling Tunnel is studied. Finite element method is adopted to simulate the site excavation steps. At the same time, the tectonic stress is changed on the boundary of the model to simulate the actual rockburst areas; and the most proximal area's value is adopted to decide the section tectonic stress. Then, other sections' values are revised.

从苍岭隧道的构造应力场特征入手,结合现场开挖后岩爆实际发生状况,在前期研究资料的基础上,利用有限元计算分析,模拟现场实际施工步骤的同时不断改变模型边界上的构造应力来拟合实际岩爆区,以最接近实际破坏范围的计算结果界定区段构造应力值,据此对隧道各区段的构造应力进行修正。

During early and middle Jurassic period, as a northern boundary, the fault zone controlled a seires of sedimentation of coal basins and magma activity. A lot of nappes developed during Ⅰ,Ⅱ and Ⅲ phase of the Yanshan movement. The strongest structural activity during the Yanshan movement is the Ⅱ phase, It had three pulsation and formed large-scale tectonic system with dextral strike slip.

早、中侏罗世,断裂带作为北界,控制了由西向东一系列煤系盆地的沉积作用和岩浆活动;在燕山运动的Ⅰ、Ⅱ、Ⅲ幕中分别形成了一系列逆冲构造;其中,以燕山Ⅱ幕构造活动最强,并至少经历了三次脉动作用,形成的逆冲构造不是由盆缘到盆内的&对冲&,而是受本断裂带限制,并以之为主滑面构成了区域上的大型右行走滑斜压式构造系统。

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