Red River fault zone
- 网络红河断裂带
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Study on activity of the Red River Fault Zone
红河断裂带活动性研究
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Geophysical research on deep structure feature in study region of red river fault zone
红河断裂带研究区深部结构特点的地球物理研究
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Seismic activities of Red River fault zone at present also show this trend .
红河断裂带上当今地震活动也表明这一趋向。
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Gravity effect from present activity of northern segment of Red River Fault Zone
红河断裂带北段现今活动的重力效应
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Processing about quantitative study of large-scale strike-slip movement on Red River Fault Zone
红河断裂带大型右旋走滑运动定量研究的若干问题
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Gravity measurement along Red River Fault Zone
红河断裂带上的重力测量
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The development of the offset drainage system and the seismic activities on the Red River Fault Zone
红河断裂带的断错水系发育与地震活动问题
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Geological and geomorphological features of neotectonic movement of Red River Fault Zone
红河断裂带新构造活动的地质地貌特征
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Study on fractal characteristic of hydrographic nets and activity of the Red River Fault Zone
水系的分形特征与红河断裂带活动性关系初探
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Earthquake focal mechanism and its tectonic significance along the two sides of the Red River Fault Zone
红河断裂带两侧地震震源机制及构造意义
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X ray measurements of PALEOTECTONIC RESIDUAL STRESS with depth along the Red River Fault Zone
红河断裂带测区古构造残余应力随深度分布X射线测量
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Deformation mechanism of Red River fault zone during Cenozoic and experimental evidences related to Yinggehai basin formation
红河断裂带的新生代变形机制及莺歌海盆地的实验证据
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The Yinggehai basin developed on the seaward elongation of the Red River Fault Zone .
莺歌海盆地发育于红河断裂带海上延伸带上。
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Relocation Results of Moderate-small Earthquakes in the Red River Fault Zone of Yunnan and Its Relation with Geologic Structure
云南红河断裂带中小地震重定位及其与地质构造的关系
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FT dating of fault rocks in the Central-Southern section of the Red River fault zone and Its Geological Implications
红河断裂带中南段断层岩FT测年及其地质意义
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The Change of density , compressive and shear wave velocity of gouge of the Red River fault zone followed pressure was measured up to 500 MPa .
在500MPa的压力范围内测定了红河断裂带断层泥的密度、纵波速度和横波速度随压力的变化。
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The range of deformation region and the magnitude of deformation show that the eastern plate of the Red River Fault zone is always the active plate for the relative movement of the fault blocks .
变形区的范围大小和变形幅度表明红河断裂的东盘地块始终是作为地块相对运动的主动盘。
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Since the Tertiary period , the Red River Fault Zone suffered both of the sinistral movement and dextral movement , but the activities of the north and the south segment were different .
断裂带自第三纪以来,经历了左旋运动、右旋运动,南北两段的活动性有一定的差异。
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In this tectonic setting , the Red River fault zone along the north-east set a series of rock tend to the North West Department of thrust fault occurred since the North West-South East thrust .
在此构造背景下,红河断裂带北东盘岩体沿一系列倾向北西的逆冲断层发生自北西&南东的逆冲推覆。
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The Red River Fault Zone is a large slide and active fault zone . It controls the tectonic activities of the northwestern South China Sea and also controls the form and evolution of the Yinggehai basin .
南海西北部红河断裂带是一条走滑的活动断裂带,它控制着该区的构造活动,也控制着莺歌海油气盆地的形成和演化。
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The relationship of density and compressive and shear wave velocity is satisfactory to Birch 's law , and so the Birch 's coefficients of gouge of the Red River fault zone have been obtained .
断层泥密度与纵波和横波速度的关系均满足Birch定律,并由此得到了红河断裂带断层泥的Birch系数。