Chinese translation for "地震波速"

seismic velocity
velocity of seismic wave

Related Translations:

地震波:  earthquake wave; tidal wave; seismic wave

地震波速度:  velocity of seismic wave

地震波折射:  seismic refractionseismicrefraction

地震波导:  seismic waveguide

地震波射线:  seismic ray

地震波谱:  seismic ectrumseismic spectrum

地震波形:  seismic wave formseismic waveformseismic waveshape

地震波发生器:  seismic wave generator

地震波曲线:  seismogram

连续地震波:  csw

Example Sentences:

	1.	Seismic velocity can occasionally be affected by porosity and temperature . 孔隙率和温度有时也能影响地震波速。
	2.	Lattice preffered orientation and seismic anisotropy of ultramafic xenoliths in damaping , hebei province 河北大麻坪超基性岩包体的岩石组构和地震波速各向异性
	3.	Velocity variation is positively correlated with crust thickness and negatively correlated with earth ' s heatflow . the linear regression equation of velocity , crust thichness and heatflow is obtained . the regression coefficient dv / dp convert 同时地震波速厂与地壳厚度h呈明显的线性正相关关系，与大地热流呈负相关关系，并得到三者的线性回归方程，回归系数dv dh换算成bv op ？
	4.	Directions are obtained by two means : calculation and measure . our investigations are summed as follows : 1 the lpo relations between olivine and orthopyroxene are different from usually situations : 100ol 001opx , 010ol 100opx , 001ol 010opx ; 2 the seismic anisotropy of the ultramafic rocks in damaping is obvious . their characters are consistent with the structures of the rocks and fabrics of minerals , which means seismic anisotropy is mainly controlled by rocks fabrics ; 3 seismic velocities suggest that the composition of upper mantle in damaping region is resemble to the xenoliths , which major component is lherzolite 不同2大麻坪地区幔源包体的波速各向异性显著，岩石的波速各向异性特征与其宏观构造和微观组构一致，说明岩石组构是造成地震波速各向异性的决定因素3由地震波速推测的大麻坪地区的上地幔成分与包体出露的情况一致，即主体为二辉橄榄岩。
	5.	The main contents of this paper are as follows : the research of principle of testing the strength of abamurus using earthquake wave velocity , the research of principle of testing the geometrical dimension of abamurus using gpr method , the research of laboratory test of the correlation of the strength of abamurus with wave velocity and the field test and estimation 本论文的主要内容有：地震波速法检测挡墙强度原理的研究，地质雷达法检测墙体几何尺寸的原理的研究，挡墙材料强度与波速的相关关系的室内试验研究，现场挡墙检测和评价。
	6.	This paper puts forward a method of fast , handy , no - destructive and effective testing which can be used to test the strength and geometrical dimension of subgrade abamurus using the method of earthquake wave velocity and gpr ( ground penetrating radar ) . this method can be used to definite the dimension and strength of abamurus by determining some physical parameters ( such as elastic wave velocity and electromagnetic wave velocity etc , ) and by the correlation of these physical parameters with mortar flag stones 本论文提出使用地震波速法和地质雷达法检测路基挡墙的强度和几何尺寸，是一种快速、简便、无损、有效的检测方法。此方法通过测定某些适当的物理量(如：弹性波速度、电磁波速度等) ，并通过这些物理量与浆砌片石的相关性，确定墙体的尺寸、强度等性能。
	7.	The main contents of testing the strength of subgrade abamurus using earthquake wave velocity are as follows : the influence of the lithology and strength of flag stones and the shape of block upon wave velocity , the influence of the strength of cement mortar upon earthquake wave velocity , the estimation standards of the strength and completion of abamurus . this paper puts forward an accurate no - destructive testing using the different reflect of elastic wave velocity for abamurus stones , the strength of mortar , the plumpness of mortar and the type of abamurus , on the basis of laboratory tests and field tests . it can be used to accurately distinguish the completion of abamurus 地震波速法检测路基挡墙强度，研究的主要内容有：片石岩性和强度及块体形体对波速的影响；水泥砂浆强度对墙体波速的影响；挡墙整体强度和完整性的评估标准。应用弹性波速度对挡土墙石材、砂浆强度、砂浆饱满度及挡墙类型的不同反映，在室内外模型试验和现场生产试验的基础上，提出了一种正确的无损检测法，可以正确判别浆砂片石挡墙墙身的完整性。
	8.	The velocity ratio or poisson ratio variaton can be obtained by comparing pn and sn velocities . 3 , in comparing pn and sn velocity variation with geology , we will find that high velocity regions always exist in old stable basin and terra , but low velocity regions lie in active extensional basin , volcano area and magmatic rock regions 中国大陆上地慢顶部体波速度层析成像3 、将pn波速度和sn波速度横向变化与地质构造对比发现，地震波速高的地区往往是构造上比较稳定的古老盆地、地台等，而地震波速低的地区是在构造上比较活动的张性盆地，火山活动区和岩浆岩分布区。

Similar Words：

"地震波曲线图" Chinese translation, "地震波散" Chinese translation, "地震波射线" Chinese translation, "地震波试验" Chinese translation, "地震波衰减" Chinese translation, "地震波速等值线" Chinese translation, "地震波速度" Chinese translation, "地震波速度突变面" Chinese translation, "地震波速异向性" Chinese translation, "地震波探矿" Chinese translation