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On the basis of the research on shape of fish-head boudin and the difference between layer and matrix, and by means of the method of physical modeling, the author modeled different shapes of fish-head boudin, and came out the relationship between shape of fish-head boudin and viscosity ratio between layer and matrix, which can be called an experience rheological gauge.

在深入研究鱼嘴构造形态与能干层基质流变性差异的基础上,运用物理模拟的方法,模拟出不同形态的鱼嘴香肠构造,反演出能干层基质粘度比与香肠形态之间的关系,进而得出一种关於鱼嘴香肠构造的经验流变计。

On the basis of the research on shape of fishhead boudin and the difference between layer and matrix, and by means of the method of physical modeling, the author modeled different shapes of fishhead boudin, and came out the relationship between shape of fishhead boudin and viscosity ratio between layer and matrix, which can be called an experience rheological gauge.

在深入研究鱼嘴构造形态与能干层基质流变性差异的基础上,运用物理模拟的方法,模拟出不同形态的鱼嘴香肠构造,反演出能干层基质粘度比与香肠形态之间的关系,进而得出一种关于鱼嘴香肠构造的经验流变计。

Based on the above results of macro expansion and microstructure studies, the limitation of the early ASR expansion mechanism has been noted, and the new ASR models for aggregates with various texture and structure have been put forward.

为进一步研究集料结构构造和集料尺寸对鉴定集料ASR活性的影响,用光学显微镜、XRD和SEM/EDS等方法研究了集料的岩石学、矿物学特征及其ASR反应特征,发现除集料中活性组分的类型和数量外,集料的物理构造特征对ASR过程和膨胀行为有显著影响,而且集料的尺寸不同,物理构造的影响程度有差异。

Tectonic subsidence play dominant role in their geometric shapes, basin fillings, sequence evolution and sediment distribution in the Wushi Sag. Outline of the sequences are in shape of box-wedge or sheet-wedge and boundaries of sequences are varied from bilateral fault to monoclinal fault overlap, so that the sequences show distinct semigrabens which overlay in different ways. Seven sequences were formed in different stage of tectonic evolution. The sequence of SQ1 formed in initial rift stage and deposited alluvial sequence. Sequences SQ2-SQ4 developed in intense rift stage and sediment lacustrine sequence. Sequences SQ5-SQ7 formed in late period of rift before thermal subsidence and deposit mere and delta sediment. The place adjacent to the synsedimentary fault is the subsidence center and depocenter; meanwhile, controlling fracture migrates in horizontal made subsidence and sedimentary center of the sag changed.

构造沉降是控制层序几何形态,充填叠置方式、演化及沉积体系分布的最重要因素:凹陷由多个半地堑在不同层序发育时期以不同方式叠置联结而成;受断层控制,层序外部形态有箱状-楔形、楔形-席状披覆型,边界终止方式有双断终止型、单断终止超覆型;不同构造演化阶段层序内部充填的沉积体系各具特征,初始断陷阶段的SQ1沉积冲积层序,强烈断陷阶段的SQ2-SQ4充填湖相层序,晚期断陷阶段SQ5-SQ7内部充填浅湖和河流三角洲沉积;同沉积断层陡坡带沉降迅速、可容纳空间快速增长,是凹陷的沉积和沉降中心,断陷期主控断裂活动时间和空间的变化导致了凹陷沉积和沉降中心的迁移。

The paper has analysed the charactors of the mylonitic faultage in Yanmenguan Tunnel, especially in different structure stress field and different structure movement.

本文重点研究了发育在雁门关隧道左线糜棱岩构造破碎带的特征,分析了它形成、发展的规律,着重研究了该断层在不同构造应力场的作用下,所产生的不同期次、不同性质的构造运动的力学行为,并由此推断出该断层对隧道施工可能造成的影响,提出了行之有效的治理措

From the Late Carboniferous to the Permian, Junggar region into the post-collision tectonic evolution stage, in the stage of the post-collision, the early subduction slab rupture and separate, asthenosphere decompression melting, basalt magma take place underplating, because the underplating of the basalt magma, low crust melt by the high temperature forming the acid crust-magma, the basic magma from mantle and acid one from crust mixing at the vicinity of the crust-mantle boundary, formed the Huangyangshan magma mixing plution, the dioritic microgranular enclaves are the recorder of the crust and mantal magma mixing process.

从晚石炭世到二叠纪,准噶尔地区进入后碰撞构造演化阶段,在后碰撞构造阶段,早期的俯冲板片断离,软流圈减压熔融,玄武质岩浆底侵至下地壳底部,底侵基性岩浆带来的巨大热量,导致地壳物质熔融,形成大规模的花岗质岩浆,两种岩浆在壳-幔边界附近发生不同程度的混合,其中闪长质微细粒包体就是基性的幔源岩浆和酸性的壳源岩浆不同程度的混合的记录者。

Fault activities reconstructed the structural framework of the basin in different stages, the substructural unit es of the basin changed too.

构造活动使不同时期的盆地格局发生改变,不同阶段盆地的次级构造单元也随之变化。

So the elevating and plunging between these three anticlinal belts imply the displacement transfer in the southnorth direction. The deep structures of the second and third rows of antclinal belts in the Southern Junggar Basin are composed of several imbricate hinge wedgeshaped fault blocks, which usually have small lateral extension, but may have independent reservoir system and different hydrocarbongaswater characteristics.

准噶尔盆地南缘第二、三排背斜带中-新生界内部发育多个小型的构造楔形体,这些互相叠置的楔形构造横向延伸不大,但有可能构成独立的成藏系统,具有不同的油气水特征,从而造成同一个背斜带不同部位的含油气性迥异。

Referencing to the internal and external documents, we have plotted the balanced evolutions for the various typical structures by computer, which is the first time at home; applied the balancing technique by computer to the representative structures in Sichuan Oil and Gas Basin, and also established the geological modellings on three different structural elements and their own balanced evocutions in Sichuan Basin.

借鉴国内外的资料,在国内首次用计算机绘制出各种典型构造的平衡演化剖面,并应用机制平衡技术对四川油气盆地内的代表构造作了详细的平衡计算,建立起四川盆地内三个不同构造单元的地质模型以及构造平衡演化剖面。

With the help of these conditions, computer efficiently searches out many quasi-perfect and double quasi-perfect punctured binary array pairs. The relationships among perfect punctured binary array pair, quasi-perfect and double quasi-perfect punctured binary array pair is presented. Specially, when first and second dimension period of the punctured binary ar

定义了非周期屏蔽二元序列偶的自相关函数、屏蔽二元互补序列偶和最佳屏蔽二元互补序列偶,给出并证明了屏蔽二元互补序列偶的变换性质;和它存在的组合允许条件,用计算机搜索出若干最佳屏蔽二元互补序列偶;给出了屏蔽二元互补序列构造出新的屏蔽二元互补序列偶的四种构造方法;并且,给出了利用不同长度的二元互补序列和屏蔽二元互补序列偶构造出新的屏蔽二元互补序列偶的四种构造方法。

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