標(biāo)題: Titlebook: Digital Seismology and Fine Modeling of the Lithosphere; R. Cassinis,G. Nolet,G. F. Panza Book 1989 Springer Science+Business Media New Yo [打印本頁] 作者: NERVE 時(shí)間: 2025-3-21 19:53
書目名稱Digital Seismology and Fine Modeling of the Lithosphere影響因子(影響力)
書目名稱Digital Seismology and Fine Modeling of the Lithosphere影響因子(影響力)學(xué)科排名
書目名稱Digital Seismology and Fine Modeling of the Lithosphere網(wǎng)絡(luò)公開度
書目名稱Digital Seismology and Fine Modeling of the Lithosphere網(wǎng)絡(luò)公開度學(xué)科排名
書目名稱Digital Seismology and Fine Modeling of the Lithosphere被引頻次
書目名稱Digital Seismology and Fine Modeling of the Lithosphere被引頻次學(xué)科排名
書目名稱Digital Seismology and Fine Modeling of the Lithosphere年度引用
書目名稱Digital Seismology and Fine Modeling of the Lithosphere年度引用學(xué)科排名
書目名稱Digital Seismology and Fine Modeling of the Lithosphere讀者反饋
書目名稱Digital Seismology and Fine Modeling of the Lithosphere讀者反饋學(xué)科排名
作者: 拱形面包 時(shí)間: 2025-3-21 22:41
https://doi.org/10.1007/978-3-642-14840-8ervations of travel time anomalies. The deployment of broad-band instrumentation and advances in analysis methods now permit more extensive use of waveform data to model slab effects, including those that are non-geometrical.作者: GIST 時(shí)間: 2025-3-22 04:14
Very-Broad-Band Seismometry,ists in Japan in 1880. Most of their instruments were designed to record the largest possible range of periods. The Japanese seismologist Omori recorded beautiful broad-band seismograms of large earthquakes around 1900 which until recently one could not have obtained with modern seismographs.作者: Ceramic 時(shí)間: 2025-3-22 06:19
Wave Propagation in Subducted Lithospheric Slabs,ervations of travel time anomalies. The deployment of broad-band instrumentation and advances in analysis methods now permit more extensive use of waveform data to model slab effects, including those that are non-geometrical.作者: expeditious 時(shí)間: 2025-3-22 11:09 作者: Callus 時(shí)間: 2025-3-22 14:34 作者: Callus 時(shí)間: 2025-3-22 18:02 作者: grandiose 時(shí)間: 2025-3-22 21:45 作者: 征兵 時(shí)間: 2025-3-23 01:48
Francesco Massari,Hildegard Westphalthat processing. Although every seismic line has its own individual processing problems, the standard processes appropriate to almost all marine deep reflection data are shown here, so that this paper may serve both as a tutorial to workers entering this field and as a reivew of a standarized processing sequence presently in use at BIRPS.作者: 表皮 時(shí)間: 2025-3-23 09:01 作者: 寡頭政治 時(shí)間: 2025-3-23 11:36 作者: 糾纏,纏繞 時(shí)間: 2025-3-23 14:01 作者: intention 時(shí)間: 2025-3-23 19:40
Digital Seismology and Fine Modeling of the Lithosphere作者: 混合 時(shí)間: 2025-3-24 00:16
Digital Seismology and Fine Modeling of the Lithosphere978-1-4899-6759-6作者: plasma-cells 時(shí)間: 2025-3-24 03:20 作者: Asparagus 時(shí)間: 2025-3-24 09:22
Aspects of Acquisition and Interpretation of Deep Seismic Sounding Data,at present much more time has to be spent to digitize the analogue field data, which are still collected in Europe mostly with the same type of frequency-multiplex recording system MARS 66 or minor technical modifications thereof (Berckhemer, 1970), than for the preparation and realization of the fi作者: 混雜人 時(shí)間: 2025-3-24 14:12
Reference Model for Tomographic Imaging of the Upper Mantle Shear Velocity Structure Beneath Europeblems are to be expected. Fewer S data are available from the ISC and S delays are subject to larger errors due to identification problems and inaccuracies in the readings of the exact onsets. The choice of the starting or reference model to be used for tomographic inversions should be considered ca作者: Deject 時(shí)間: 2025-3-24 16:01
Broad-Band P-Wave Signals and Spectra from Digital Stations,e earthquake. For this reason, the spectral method in which the observed spectra are corrected for instrument response is probably a more reliable method for estimating seismic moments. Of course, if the instrument response of the seismograph does not include the corner frequency in its bandpass the作者: entrance 時(shí)間: 2025-3-24 22:08 作者: 辭職 時(shí)間: 2025-3-25 00:19
Spencer G. Lucas,Lawrence H. Tannerat present much more time has to be spent to digitize the analogue field data, which are still collected in Europe mostly with the same type of frequency-multiplex recording system MARS 66 or minor technical modifications thereof (Berckhemer, 1970), than for the preparation and realization of the fi作者: 神刊 時(shí)間: 2025-3-25 04:32 作者: ingrate 時(shí)間: 2025-3-25 08:58
Massimiliano Lucci,Ivan Colantonie earthquake. For this reason, the spectral method in which the observed spectra are corrected for instrument response is probably a more reliable method for estimating seismic moments. Of course, if the instrument response of the seismograph does not include the corner frequency in its bandpass the作者: 遺忘 時(shí)間: 2025-3-25 14:08
https://doi.org/10.1007/978-1-4899-6759-6lithosphere; modeling; seismology作者: affect 時(shí)間: 2025-3-25 18:58
978-1-4899-6761-9Springer Science+Business Media New York 1989作者: Lice692 時(shí)間: 2025-3-25 21:01
Overview: 978-1-4899-6761-9978-1-4899-6759-6作者: invert 時(shí)間: 2025-3-26 03:48 作者: 憤憤不平 時(shí)間: 2025-3-26 06:31
https://doi.org/10.1007/978-3-658-36073-3e to the large dynamic range of digital instruments allowing high quality recording of ground motion over a wide amplitude interval. Consequently, a new generation of techniques applied to time and frequency domain digital data has been developed which have the objective to increase the resolution on the estimate of source and medium parameters.作者: carotenoids 時(shí)間: 2025-3-26 08:35 作者: 不可磨滅 時(shí)間: 2025-3-26 14:51
Einführung in die Produktdatentechnologie“Were it not for the intrinsic attenuation of sound in the earth’s interior, the energy of earthquakes of past would still reverberate through the interior of the earth today.” In this way Knopoff in his classical paper entitled Q (Knopoff, 1964) nicely describes the importance of the anelastic behavior of the Earth.作者: lymphoma 時(shí)間: 2025-3-26 20:03 作者: 物種起源 時(shí)間: 2025-3-26 22:23
Purnima Srivastava,Vinod Chandra TewariIn conventional 2-D seismic the energy emitted from a source S and backscattered from a layer R towards the surface where it is picked up by a receiver G is supposed to travel only on a vertical plane passing through S and G (plane of the section).作者: 混合,攙雜 時(shí)間: 2025-3-27 02:55 作者: SPECT 時(shí)間: 2025-3-27 07:18 作者: Anterior 時(shí)間: 2025-3-27 11:37
Imaging with Teleseismic Data,For the first time in history, seismological data are becoming available in sufficient quantity, and with sufficient accuracy, to attempt a realistic, three dimensional modeling of the elastic properties of the deep Earth’s interior.作者: START 時(shí)間: 2025-3-27 14:48
Attenuation Measurements by Multimode Synthetic Seismograms,“Were it not for the intrinsic attenuation of sound in the earth’s interior, the energy of earthquakes of past would still reverberate through the interior of the earth today.” In this way Knopoff in his classical paper entitled Q (Knopoff, 1964) nicely describes the importance of the anelastic behavior of the Earth.作者: Mobile 時(shí)間: 2025-3-27 20:26 作者: 灰心喪氣 時(shí)間: 2025-3-27 22:56 作者: 招待 時(shí)間: 2025-3-28 02:29 作者: 窗簾等 時(shí)間: 2025-3-28 08:26
A Simple Linearized Method for Inversion of Travel Time Data in Two-Dimensional Heterogeneous MediaThe broad complexity of geological situations in regions of economical or geotechnical interest requires the development and implementation of numerical and computational techniques that allow to handle many, if not all, these situations adequately. The analysis of data may be carried by solving either the direct or the inverse problem, or both.作者: 綁架 時(shí)間: 2025-3-28 14:05
Synthetic Seismograms for 3-D Inhomogeneous Media, calculations. Strong multiples such as generated at the sea bottom or the basement, are ignored in this approach. These multiples, however, also include information about the model and should not be neglected.作者: 動(dòng)作謎 時(shí)間: 2025-3-28 17:32 作者: 大范圍流行 時(shí)間: 2025-3-28 22:30 作者: adjacent 時(shí)間: 2025-3-29 02:18 作者: 亞麻制品 時(shí)間: 2025-3-29 03:26 作者: Precursor 時(shí)間: 2025-3-29 09:25 作者: 是貪求 時(shí)間: 2025-3-29 13:28
https://doi.org/10.1007/978-3-642-14840-8ing slabs can lead to compositional variations and to seismic velocities up to 10 percent higher than the surrounding mantle. These major sources of heterogeneity are known to have significant effects on the travel times and ray trajectories of waves travelling within them (e.g., Sleep, 1973; Davies作者: 為敵 時(shí)間: 2025-3-29 15:55
Spencer G. Lucas,Lawrence H. Tannerpic, causal relaxation function . .(., .). Then, the wave equation operator is not necessarily symmetric (‘self-adjoint’), but the reciprocity property is still satisfied. The representation theorem contains a term proportional to the history of strain. The dual problem consists in solving the wave 作者: 可互換 時(shí)間: 2025-3-29 20:14 作者: Supplement 時(shí)間: 2025-3-30 00:10 作者: seruting 時(shí)間: 2025-3-30 04:48 作者: Project 時(shí)間: 2025-3-30 12:04 作者: 滔滔不絕地說 時(shí)間: 2025-3-30 13:10
,: ricaduta sull’attività didattica calculations. Strong multiples such as generated at the sea bottom or the basement, are ignored in this approach. These multiples, however, also include information about the model and should not be neglected.作者: 最低點(diǎn) 時(shí)間: 2025-3-30 20:11 作者: 消滅 時(shí)間: 2025-3-30 20:58
https://doi.org/10.1007/978-3-658-36073-3e to the large dynamic range of digital instruments allowing high quality recording of ground motion over a wide amplitude interval. Consequently, a new generation of techniques applied to time and frequency domain digital data has been developed which have the objective to increase the resolution o作者: assail 時(shí)間: 2025-3-31 03:01 作者: Anecdote 時(shí)間: 2025-3-31 06:22
Portable Short Period Vertical Seismic Stations Transmitting Via Telephone or Satellite,n efficient tool to investigate the earth: they provide a way to understand how rocks break through the accumulation of stress in some particular places, as well as a tool to map the P- and S-velocity structure in the medium in between sources and receivers. The wealth of information accessible by r作者: fledged 時(shí)間: 2025-3-31 11:39
Waveform Synthesis by Ray Theoretical Methods,e. The simplest and most widely used of the high frequency methods is classical geometrical ray theory, which is the basis of most practical methods for the modeling of seismograms and the inversion of travel times in seismology and applied geophysics. A comprehensive discussion of several aspects o作者: 激怒 時(shí)間: 2025-3-31 14:16 作者: Paleontology 時(shí)間: 2025-3-31 18:45
Theoretical Background for the Inversion of Seismic Waveforms, Including Elasticity and Attenuationpic, causal relaxation function . .(., .). Then, the wave equation operator is not necessarily symmetric (‘self-adjoint’), but the reciprocity property is still satisfied. The representation theorem contains a term proportional to the history of strain. The dual problem consists in solving the wave 作者: LAPSE 時(shí)間: 2025-3-31 23:01 作者: Flawless 時(shí)間: 2025-4-1 02:03 作者: neuron 時(shí)間: 2025-4-1 07:56 作者: Gerontology 時(shí)間: 2025-4-1 12:38
Reference Model for Tomographic Imaging of the Upper Mantle Shear Velocity Structure Beneath Europeures in exploration seismics. In studies of large areas they often make use of the delay time data provided by the International Seismological Centre. Many results have been obtained using P delays. For instance, Spakman (1986) has used 500,000 ISC P delays to derive a tomographic model of the Upper作者: graphy 時(shí)間: 2025-4-1 16:40
Synthetic Seismograms for 3-D Inhomogeneous Media, calculations. Strong multiples such as generated at the sea bottom or the basement, are ignored in this approach. These multiples, however, also include information about the model and should not be neglected.作者: 刺穿 時(shí)間: 2025-4-1 19:09
