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1988年澜沧—耿马地震大地形变特征 被引量:3
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作者 刘玉权 邵德盛 +1 位作者 黎炜 樊友心 《地壳形变与地震》 CSCD 1993年第1期69-76,共8页
1988年11月6日发生在云南省澜沧—耿马地区的两次强烈地震,其构造分型属雁列地震。7.6级地震的地表形变带呈“入”字形展布;7.2级地震的地表形变带反映单一发震构造特征。根据大地水平形变资料,主压应变轴为北东方向,地表形变带上存在... 1988年11月6日发生在云南省澜沧—耿马地区的两次强烈地震,其构造分型属雁列地震。7.6级地震的地表形变带呈“入”字形展布;7.2级地震的地表形变带反映单一发震构造特征。根据大地水平形变资料,主压应变轴为北东方向,地表形变带上存在明显的水平剪切错动;根据大地垂直形变资料,地表形变带无垂直向弹性差异形变,仅表现出一种重力堑的作用。本次地震序列所反映出来的大地形变基本特征与中国历次大陆地震相同。 展开更多
关键词 澜沧-耿马 地震 大地变形 震级
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兰天武地区现今大地垂直形变场演化与地壳运动特征 被引量:5
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作者 王双绪 江在森 唐传芬 《地壳形变与地震》 CSCD 1995年第1期62-70,共9页
用分段线性速率整体动态平差法处理了兰天武地区20多年来的多期水准资料,分析了该区现今大地垂直形变场演化与地壳运动特征。研究结果表明:该区垂直形变七十年代曾表现出山间盆地大幅度上升的强烈逆继承性运动;八十年代华家岭等两... 用分段线性速率整体动态平差法处理了兰天武地区20多年来的多期水准资料,分析了该区现今大地垂直形变场演化与地壳运动特征。研究结果表明:该区垂直形变七十年代曾表现出山间盆地大幅度上升的强烈逆继承性运动;八十年代华家岭等两北部山地上升、东南部盆地下沉的继承性运动增强;而目前基本恢复了正常的继承性运动状态。进一步分析认为:强烈逆继承性运动和继承性运动增强是区域应力场趋于强化的标志;正常继承性运动的恢复可能是应力场调整的结果。 展开更多
关键词 南北构造带 地壳运动 大地变形
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Anchoring effect and energy-absorbing support mechanism of large deformation bolt 被引量:14
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作者 ZHAO Tong-bin XING Ming-lu +2 位作者 GUO Wei-yao WANG Cun-wen WANG Bo 《Journal of Central South University》 SCIE EI CAS CSCD 2021年第2期572-581,共10页
To research the anchoring effect of large deformation bolt,tensile and drawing models are established.Then,the evolution laws of drawing force,bolt axial force and interfacial shear stress are analyzed.Additionally,th... To research the anchoring effect of large deformation bolt,tensile and drawing models are established.Then,the evolution laws of drawing force,bolt axial force and interfacial shear stress are analyzed.Additionally,the influence of structure element position on the anchoring effect of large deformation bolt is discussed.At last,the energy-absorbing support mechanism is discussed.Results show that during the drawing process of normal bolt,drawing force,bolt axial force and interfacial shear stress all gradually increase as increasing the drawing displacement,but when the large deformation bolt enters the structural deformation stage,these three values will keep stable;when the structure element of large deformation bolt approaches the drawing end,the fluctuation range of drawing force decreases,the distributions of bolt axial force and interfacial shear stress of anchorage section are steady and the increasing rate of interfacial shear stress decreases,which are advantageous for keeping the stress stability of the anchorage body.During the working process of large deformation bolt,the strain of bolt body is small,the working resistance is stable and the distributions of bolt axial force and interfacial shear stress are steady.When a rock burst event occurs,the bolt and bonding interface cannot easily break,which weakens the dynamic disaster degree. 展开更多
关键词 rock burst large deformation bolt numerical simulation pull-out test anchoring effect energy-absorbing mechanism
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Characteristics of microseismic b-value associated with rock mass large deformation in underground powerhouse caverns at different stress levels 被引量:13
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作者 LI Biao DING Quan-fu +3 位作者 XU Nu-wen DAI Feng XU Yuan QU Hong-lue 《Journal of Central South University》 SCIE EI CAS CSCD 2022年第2期693-711,共19页
Rock mass large deformation in underground powerhouse caverns has been a severe hazard in hydropower engineering in Southwest China.During the development of rock mass large deformation,a sequence of fractures was gen... Rock mass large deformation in underground powerhouse caverns has been a severe hazard in hydropower engineering in Southwest China.During the development of rock mass large deformation,a sequence of fractures was generated that can be monitored using microseismic(MS)monitoring techniques.Two MS monitoring systems were established in two typical underground powerhouse caverns featuring distinct geostress levels.The MS b-values associated with rock mass large deformation and their temporal variation are analysed.The results showed that the MS bvalue in course of rock mass deformation was less than 1.0 in the underground powerhouse caverns at a high stress level while larger than 1.5 at a low stress level.Prior to the rock mass deformation,the MS b-values derived from both the high-stress and low-stress underground powerhouse caverns show an incremental decrease over 10%within 10 d.The results contribute to understanding the fracturing characteristics of MS sources associated with rock mass large deformation and provide a reference for early warning of rock mass large deformation in underground powerhouse caverns. 展开更多
关键词 underground powerhouse caverns rock mass large deformation stress level microseismic monitoring bvalue
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