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远程应力
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     From the numerical result, it is concluded that the mechanics of tensile-compression coupling in the north China block is probably not initiated by regional stress field associated with plate-boundary interactions, but mainly by local stress variation caused by the crust ductile flow.
     华北东部盆地北西西 -南东东的挤压主要受太行山地壳厚度转变带下地壳流变所造成的动力学制约 ,与区域板块作用导致的远程应力场可能无直接联系 .
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     The authors present some factors that influence the geometry of the displacement-distance profiles of normal faults,such as the plastic deformation in the end of faults,host-rock stiffness, remote tensile stresses, and the interaction and linkage of faults.
     讨论了影响正断层位移距离剖面形态的主要因素 :断层端的脆韧性变形、围岩强度、远程应力以及断层之间的相互作用和连接等。
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     Distance Learning
     远程教育
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     DISTANCE DEUCATION
     远程教育
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     ,Reynolds stress(?) ,(?)
     ,雷诺应力(?)
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     Stress Chemistry
     应力化学
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  remote stress
It is found that the combined effects of void size and void shape are mainly controlled by the remote stress triaxiality.
      
It is interesting that rc is a material constant independent of the initial void shape and the remote stress triaxiality.
      
To this end, a 3-D finite element analysis was conducted and the stress around the borehole was examined for boreholes arbitrarily oriented to three principal axes of remote stress.
      
A fatigue crack can be effectively retarded by heating a spot near the crack tip under nil remote stress condition.
      
In this paper, we show that a three-phase elliptic inclusion under uniform remote stress and eigenstrain in anti-plane shear admits an internal uniform stress field provided that the interfaces are two confocal ellipses.
      
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In Gansu province,Jiuxi Cretaceous Basin is a monotype basin, in which grows sedimentary system of fan shaped alluvial fan delta, subgravity flow, lacustrine and fluvial facies. It was made up of some patterns combined by sedimentary system of fan shaped alluvium fan delta shallow lakeshore gravelly braided stream, subgravity flow mid deep lacustrine fan delta and fan delta mid shallow fluvial facies. According to isochronic surface, filled sequences in lacustrine basin can be divided into three tectonic...

In Gansu province,Jiuxi Cretaceous Basin is a monotype basin, in which grows sedimentary system of fan shaped alluvial fan delta, subgravity flow, lacustrine and fluvial facies. It was made up of some patterns combined by sedimentary system of fan shaped alluvium fan delta shallow lakeshore gravelly braided stream, subgravity flow mid deep lacustrine fan delta and fan delta mid shallow fluvial facies. According to isochronic surface, filled sequences in lacustrine basin can be divided into three tectonic sequences corresponding respectively to three evolutionary stages of embryonic rift, spread rift thermal attenuationary subsidence and basin shrinkage closure. On the basis of these evidences, it can be seen that either formation and attenuation of mantle's thermal column or remote stress ,such as Yanshan movement, etc.,controlled the evolution of the Jiuxi Cretaceous Basin.

甘肃酒西白垩纪盆地是酒西含油气盆地的一个单型盆地 ,发育了冲积扇、水下重力流扇、扇三角洲、湖泊、河流沉积体系 ,并在湖盆演化的不同阶段分别形成冲积扇—扇三角洲—滨浅湖—砾质辫状河、近岸水下重力流扇—中深湖—扇三角洲、扇三角洲—中浅湖—河流沉积体系组合型式。依据等时界面 ,湖盆充填序列可划分为三个构造层序 ,相对应于初始裂陷、扩张裂陷—热衰减沉降、湖盆萎缩关闭三个演化阶段。研究证明 ,地幔热柱的形成和衰减、燕山运动等远程应力作用控制盆地的演化

The West Jiuquan Cretaceous basin, a monotypic petroliferous basin in Gansu is composed of alluvial fan, subaqueous gravity flow fan, fan delta, lake, fluvial depositional systems. The depositional system associations such as alluvial fanfan deltalittoral to shallowlakegravelly braided river, nearshore subaqueous gravity flow fanmoderate to deep lakefan delta, and fan deltamoderate to shallow lakefluvial associations record the distinctive phases of the basin evolution. The infilling sequences of the...

The West Jiuquan Cretaceous basin, a monotypic petroliferous basin in Gansu is composed of alluvial fan, subaqueous gravity flow fan, fan delta, lake, fluvial depositional systems. The depositional system associations such as alluvial fanfan deltalittoral to shallowlakegravelly braided river, nearshore subaqueous gravity flow fanmoderate to deep lakefan delta, and fan deltamoderate to shallow lakefluvial associations record the distinctive phases of the basin evolution. The infilling sequences of the basin may be divided, in the light of isochrous surfaces, into three tectonic sequences corresponding to the initial rifting, extension and subsidencethermal subsidence, and basin collapse and closure phases. The evolution of the basin is controlled by the distal stresses such as the waxing and waning of the mantle thermal plumes and Yanshanian movement.

酒西白垩纪盆地是酒西含油气盆地的一个单型盆地,发育了冲积扇、水下重力流扇、扇三角洲、湖泊、河流沉积体系。在湖盆演化的不同阶段形成冲积扇 扇三角洲 滨浅湖 砾质辫状河、近岸水下重力流扇 中深湖 扇三角洲和扇三角洲 中浅湖 河流沉积体系组合型式。依据等时界面,将湖盆充填序列划分为3个构造层序,相对应于初始裂陷、扩张裂陷 热衰减沉降和湖盆萎缩关闭3个演化阶段。地幔热柱的形成和衰减、燕山运动等远程应力作用控制着盆地的演化。

Displacement-length relationship is a common method in research on normal faults in recent years. It provides a basis for extrapolating a two-dimensional view of faults into the third dimension. The authors present some factors that influence the geometry of the displacement-distance profiles of normal faults,such as the plastic deformation in the end of faults,host-rock stiffness, remote tensile stresses, and the interaction and linkage of faults. According to the geometry of the displacement-distance profiles...

Displacement-length relationship is a common method in research on normal faults in recent years. It provides a basis for extrapolating a two-dimensional view of faults into the third dimension. The authors present some factors that influence the geometry of the displacement-distance profiles of normal faults,such as the plastic deformation in the end of faults,host-rock stiffness, remote tensile stresses, and the interaction and linkage of faults. According to the geometry of the displacement-distance profiles and the stages in the development of normal faults, the authors separate the pattern of displacement into three classes: (1) symmetrical elliptical or bell shaped for single simple faults; (2) asymmetrical elliptical or bell shaped for interactive faults; (3) serrated shaped for linked faults. The authors describe some structures that are formed simultaneously with the fault, for instance the relay ramps, the intrabasin high, and so on. These structures are corresponding to the position of the interaction and linkage of faults. There are two kinds of method of measuring the displacement and length of faults as follows: measuring is done on the surface, and the other is on the subsurface. Note that the eroded part needs to be reconstructed before the faults are measured. It is of great significance to study the displacement-length relationship for faults in the development of basin, the evolution of faults and hydrocarbon exploration.

正断层位移长度关系是近年来研究正断层的一种常用方法 ,它将断层的研究从二维扩展到三维。研究正断层位移长度关系对于研究正断层演化、盆地演化以及油气勘探等方面具有重要意义。讨论了影响正断层位移距离剖面形态的主要因素 :断层端的脆韧性变形、围岩强度、远程应力以及断层之间的相互作用和连接等。根据正断层位移距离剖面的几何形态和断层发育阶段 ,可将断层的位移模式分为 3个类型 :(1)对称的椭圆状或钟状代表简单的单条断层 ;(2 )不对称的似椭圆状或钟状代表断层间的相互作用 ;(3)不规则的锯齿状代表由多条断层连接而成的断层。介绍了伴随正断层发育的传递斜坡、盆内高地等构造单元以及断层位移距离剖面的测量制作方法。测量时应注意恢复其剥蚀部分。

 
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