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991.
992.
Study on crust-mantle tectonics and its velocity structure along the Beijing-Huailai-Fengzhen profile 总被引:2,自引:0,他引:2
tudyoncrustmantletectonicsanditsvelocitystructurealongtheBeijingHuailaiFengzhenprofileZHIPINGZHU(祝治平)XIANKANGZHANG(张先康)... 相似文献
993.
994.
低应变反射波法桩基完整性检测波形分析 总被引:1,自引:0,他引:1
曹俊昌 《华东地质学院学报》1997,20(4):358-361
本文简述了反射波法检测波形的分析方法,并通过工程实例说明其应用效果。 相似文献
995.
X射线管辐射谱线分析 总被引:1,自引:0,他引:1
经Ni滤波片过滤的CuKa射线,并非为真正的单色X射线,其中含部分白色X射线和非CuKa特征谱线。用石英分析晶体(101)衍射面网将混入CuKa射线中的各种波长的谱线分离开,并测定其波长的范围,确定在CuKa射线中含有铁、镍、钴、铬四种元素的K系列谱线和钨的L系列谱线。发现在X射线粉末图谱中用CuKa(或Kβ)无法解释的弱衍射线却是由铁、镍等元素的特征谱线混入引起的。 相似文献
996.
997.
The Kirchhoff-Helmholtz (KH) integration has been used to model the reflected and the diving waves from an interface with a positive velocity gradient. The modelling is carried out for a spherical boundary and for a sinusoidal topography with a long-scale wavelength.
An artefact, which is a major problem in modelling the seismic response using the KH integration, has been reduced by introducing a Hilbert transform sign manipulation. Cleaner synthetic seismograms with correct amplitudes have been produced by this method. A discretization in larger surface elements has been made possible by introducing a smoothing factor that suppresses the noise that normally follows the constructed signal if a large element size is taken. 相似文献
An artefact, which is a major problem in modelling the seismic response using the KH integration, has been reduced by introducing a Hilbert transform sign manipulation. Cleaner synthetic seismograms with correct amplitudes have been produced by this method. A discretization in larger surface elements has been made possible by introducing a smoothing factor that suppresses the noise that normally follows the constructed signal if a large element size is taken. 相似文献
998.
Reweighting strategies in seismic deconvolution 总被引:2,自引:0,他引:2
Mauricio D. Sacchi 《Geophysical Journal International》1997,129(3):651-656
Reweighting strategies have been widely used to diminish the influence of outliers in inverse problems. In a similar fashion, they can be used to design the regularization term that must be incorporated to solve an inverse problem successfully. Zero-order quadratic regularization, or damped least squares (pre-whitening) is a common procedure used to regularize the deconvolution problem. This procedure entails the definition of a constant damping term which is used to control the roughness of the deconvolved trace. In this paper I examine two different regularization criteria that lead to an algorithm where the damping term is adapted to successfully retrieve a broad-band reflectivity.
Synthetic and field data examples are used to illustrate the ability of the algorithm to deconvolve seismic traces. 相似文献
Synthetic and field data examples are used to illustrate the ability of the algorithm to deconvolve seismic traces. 相似文献
999.
A model of a fault where the two faces do not exactly conform is characterized by a distribution of approximately circular contacts; elsewhere, the faces are stress-free. This contrasts with most earlier models, which have assumed the contact geometry to be equivalent to a plane distribution of approximately circular cracks. The contact regions in the present model are taken to be sparsely distributed, and averaged interface conditions are derived that are accurate to second order. At lowest order they agree with established formulae for the normal stiffness of non-conforming surfaces. These averaged, or mean, conditions are expected to hold at wavelengths long compared with the radii and spacing distance of the contact points. Unsurprisingly, they are equivalent to the continuity conditions for a thin elastic layer whose properties are given here in terms of the parameters of the contact surface. 相似文献
1000.
以地震资料为主要依据进行了综合研究,完善了下第三系济源群的地层层序,将它重新划分为韩庄组、聂庄组、泽峪组、丁庄组和冢头组;纠正了以往钻井地层的错误对比,将济2井的济源群叠置于济3井的济源群之上;证实下第三系济源群的厚度不止3000m,最大厚度可能达8500m。 相似文献