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会“演”故事的魔方
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《有色金属再生与利用》 2004年第4期40-40,共1页
关键词 魔方 虚拟现实 新力波 玩具 故事魔方 教育魔方
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Bond interface crack propagation of fresh foundation concrete and rock under blasting load 被引量:1
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作者 WU Liang LU Wen-bo ZHONG Dong-wang 《Journal of Coal Science & Engineering(China)》 2009年第1期61-65,共5页
According to concrete age, the dynamic stress intensity factors of bond interface crack of concrete-rock was calculated. Result shows that the propagation of concreteinterface crack is mainly caused by tensile stress ... According to concrete age, the dynamic stress intensity factors of bond interface crack of concrete-rock was calculated. Result shows that the propagation of concreteinterface crack is mainly caused by tensile stress and shear stress for stress wave reflection. With the growth of concrete age, interface crack fracture toughness increases, and itscapacity of resisting blasting load strengthens. Therefore, blasting vibration should bestrictly controlled for fresh concrete. 展开更多
关键词 fresh concrete dynamic stress intensity factors numerical calculation
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Using Long-Period Body Wave to Inverse Moment Tensors of the M_S6.8 Jiashi,Xinjiang Earthquake in 2003 and the Moderate and Small Earthquakes before and after It
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作者 Tu Hongwei Wan Xiuhong +2 位作者 Zhao Cuiping Wang Haitao Luo Guofu 《Earthquake Research in China》 2008年第4期460-469,共10页
An M_S6.8 strong earthquake took place in Jiashi,Xinjiang on February 24 of 2003.The digital wave form data recorded in Kashi and Wushi stations are selected to inverse the moment tensor solutions for the strong earth... An M_S6.8 strong earthquake took place in Jiashi,Xinjiang on February 24 of 2003.The digital wave form data recorded in Kashi and Wushi stations are selected to inverse the moment tensor solutions for the strong earthquake and the moderate and small earthquakes before and after it(108 earthquakes in 2001~2004).67 focal mechanism solutions have been calculated,and the results agree with those from Harvard University and USGS.The analysis reveals that before the strong earthquake,the moderate and small earthquake distribution was dispersed,and after the event the distribution was mainly concentrated around the strong earthquake.Before the strong earthquake,the seismic faults of the mid and small events had the character of strike-slip and normal faulting,and after the event,they exhibit strike-slip and thrust faulting.The region is dominated by near-NS horizontal compression from the southern block after the strong earthquake. 展开更多
关键词 Long-period body wave Inversion of seismic moment tensor Reliability analysis Jiashi of Xinjiang
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