【摘 要】
:
On account of increasingly frequent rock burst hazards at present,the theoretical basis of rock burst determination through P-wave velocity was analyzed based on the experiment relation model of stres
【机 构】
:
State Key Laboratory of Coal Resources and Safe Mining,School of Mines,China University of Mining an
【出 处】
:
2014年中国地球科学联合学术年会
论文部分内容阅读
On account of increasingly frequent rock burst hazards at present,the theoretical basis of rock burst determination through P-wave velocity was analyzed based on the experiment relation model of stress and P-wave velocity.Meanwhile,the technology of rock burst risk assessment was established using the combination of tomography and microseismic monitoring system (called mine tremor seismic velocity tomography).It contains assessment parameters of wave velocity anomaly An and wave velocity gradient anomaly VG.The criterion of these parameters was documented.Finally,the assessment technology was verified by practical application.The results show that the P-wave velocity can reflect the strength criterion,energy criterion,and dynamic load criterion for rock burst as for the rock mass with the same properties.The mine tremor seismic velocity tomography is feasible for rock burst risk assessment.It can give guidance on the implement of risk relief measures and check the effect of the measures.
其他文献
本文发展了一种从球坐标系到笛卡尔坐标系的H-W方法,来反演浅层地壳中的速度分布.我们利用走时曲线斜率的直接积分反演随深度变化的一维速度结构.为避免积分的不稳定性,采用局部勒让德多项式逼近法得到一条单调连续的走时曲线.
为了探究陆陆相互碰撞过程中不同块体之间的接触关系及缝合带边界的结构形态,我们跨东昆仑造山带布设了北东方向宽频带流动台站观测剖面,共22 个记录仪,台间距10~15km,数据记录时间从2010年11 月至2011 年6 月.剖面横跨上述两条重要缝合带和三个块体.远震P波接收函数的结果表明,柴达木-东昆仑地体具有偏低的Vp/Vs,松潘-甘孜地体的Vp/Vs则相对较高,剖面自北往南莫霍面逐渐增加,支持青
SRME适用于压制长周期的海底相关多次波,其最大优势在于预测过程不需要知道地下介质信息,而且是同时估计出所有表面相关的多次波,DWD适用于压制短周期的海底相关多次波,主要根据白相关获得海底相关多次波模型。在浅海区,采用DWD+SRME方法来压制浅水多次波,其效果比常规SRME方法要好。
Vere-Jones branching crack model was developed in 1970s.In this model,the earthquake source is regarded as the result from the total population of crack elements in a critical or near-critical branchi
汤加克马德克俯冲带是一直是全球板块研究的热点区域,该地区Wadati-Benioff带深震分布明显、震源机制解丰富.本研究中,将反演应力场的网格搜索法应用于汤加克马德克Wadati-Benioff带深部应力场研究,结果表明:第一,得到的汤加克马德克Wadati-Benioff带的走向约为N20°E,倾角约为50°。第二,浅部(100-300km),压轴方位变化较强烈,在23°N以北,压轴方位大致为
通过对页岩油气领域所面临的关键难题的梳理和分析,提出要认识页岩油气的成藏机理、指导甜点区的选定及有效开发需要首先认识以下三方面的关键科学问题(1,2,3)和两方面的关键技术问题(4,5):1)致密油气的可流动性及其表征,2)致密岩石的成储机理,3)致密油气的赋存机理和赋存状态,4)致密岩石无机非均质性的评价和预测,5)致密岩石有机非均质性的评价和预测。初步的探究表明,在纳米材料固-流吸附剂定量表征
The solid inner core of the Earth consists of heavy minerals Fe and Ni with a fraction of light elements such as O,S,Si.During the inner core formation,these light elements escape and rise up through
The Tianshan orogenic belt is one of the youngest and highest inland orogenic belts in the world.In order to investigate the detailed structure of the crust and uppermost mantle of the eastern Tiansha
Combining the newly collected teleseismic body waves recorded by Cuoqin-Dangxiong passive seismic array of 59 broadband stations with waveforms from several previous temporary local seismic arrays of
Anthropogenic activities like oil and gas production or geothermal field exploitation are known to induce small magnitude earthquakes (usually M5.5) on nearby active tectonic faults3,4 – which has bee