標(biāo)題: Titlebook: Upper Mantle Heterogeneities from Active and Passive Seismology; Karl Fuchs Book 1997 Springer Science+Business Media Dordrecht 1997 explo [打印本頁(yè)] 作者: 技巧 時(shí)間: 2025-3-21 16:39
書(shū)目名稱Upper Mantle Heterogeneities from Active and Passive Seismology影響因子(影響力)
書(shū)目名稱Upper Mantle Heterogeneities from Active and Passive Seismology影響因子(影響力)學(xué)科排名
書(shū)目名稱Upper Mantle Heterogeneities from Active and Passive Seismology網(wǎng)絡(luò)公開(kāi)度
書(shū)目名稱Upper Mantle Heterogeneities from Active and Passive Seismology網(wǎng)絡(luò)公開(kāi)度學(xué)科排名
書(shū)目名稱Upper Mantle Heterogeneities from Active and Passive Seismology被引頻次
書(shū)目名稱Upper Mantle Heterogeneities from Active and Passive Seismology被引頻次學(xué)科排名
書(shū)目名稱Upper Mantle Heterogeneities from Active and Passive Seismology年度引用
書(shū)目名稱Upper Mantle Heterogeneities from Active and Passive Seismology年度引用學(xué)科排名
書(shū)目名稱Upper Mantle Heterogeneities from Active and Passive Seismology讀者反饋
書(shū)目名稱Upper Mantle Heterogeneities from Active and Passive Seismology讀者反饋學(xué)科排名
作者: bifurcate 時(shí)間: 2025-3-21 21:42
NATO Science Partnership Subseries: 1http://image.papertrans.cn/u/image/943810.jpg作者: Morose 時(shí)間: 2025-3-22 01:46
https://doi.org/10.1007/978-94-015-8979-6exploration; seismic; seismology作者: ROOF 時(shí)間: 2025-3-22 07:14 作者: 撫育 時(shí)間: 2025-3-22 10:09 作者: Sigmoidoscopy 時(shí)間: 2025-3-22 15:47 作者: Obligatory 時(shí)間: 2025-3-22 19:30 作者: exclamation 時(shí)間: 2025-3-22 22:14
978-90-481-4966-7Springer Science+Business Media Dordrecht 1997作者: 吝嗇性 時(shí)間: 2025-3-23 02:18
Upper Mantle Heterogeneities from Active and Passive Seismology978-94-015-8979-6Series ISSN 1389-1820 作者: Inkling 時(shí)間: 2025-3-23 06:31 作者: Multiple 時(shí)間: 2025-3-23 09:42
I. O. Kitov wavelet packets in speech denoising and biomedical signals. In closing, Chapter 6 highlights applications of wavelets and wavelet packets in image denoising.978-981-13-4375-9978-981-13-0268-8Series ISSN 2364-6748 Series E-ISSN 2364-6756 作者: IRK 時(shí)間: 2025-3-23 14:22 作者: 凝視 時(shí)間: 2025-3-23 21:01 作者: 使迷醉 時(shí)間: 2025-3-23 23:49
J. Cipar,K. Priestleyerent noise models and designs including density estimation, hazard rate estimation, and inverse problems; the use of wavelets for stationary and non-stationary time series analysis; and how wavelets might be u978-0-387-75960-9978-0-387-75961-6Series ISSN 2197-5736 Series E-ISSN 2197-5744 作者: Subjugate 時(shí)間: 2025-3-24 05:05
thogonal wavelets, wavelet packets, affine and quasi-affine frames, MSF multiwavelets, multiwavelet sets, generalized scaling sets, scaling sets, unconditional basis properties of wavelets and shift invariant spaces.?978-981-16-7883-7978-981-16-7881-3Series ISSN 2523-3114 Series E-ISSN 2523-3122 作者: 溺愛(ài) 時(shí)間: 2025-3-24 09:07
L. N. Solodilovsed on the MRA properties of wavelet bases, two-scale multi-level methods are proposed, which generate higher level approximate wavelet solutions from the results of lower level calculations. Adaptive grid refinement can be applied only to regions where the residual at lower level is relatively larg作者: 可觸知 時(shí)間: 2025-3-24 13:07
K. Fuchs,F. Wenzel-dollar and British Pound for forward periods from 1 month to 5 years is analysed. We find that the unbiasedness hypothesis cannot be rejected if the data is reconstructed using medium-term and long term components. This is most prevalent in the forward transaction periods up to 1 year.作者: esculent 時(shí)間: 2025-3-24 17:06 作者: 內(nèi)行 時(shí)間: 2025-3-24 20:38
A. V. Egorkinises this scale’s lowpass image with all the higher frequency subbands produced by decompositions up to this scale.The number of transform coefficients is equal to that of the original image. Clearly, this transform is a natural platform for producing streams of code bits (hereinafter called .) that作者: Dysplasia 時(shí)間: 2025-3-24 23:34
M. Grads contraint serves as an example to show the conceptual strengths of wavelet techniques for some of the above mentioned issues. At this point, I would like to express my gratitude to several people before and during the process of writing this monograph. Most of all, I wish to thank Prof. Dr. Wolfga作者: Gnrh670 時(shí)間: 2025-3-25 04:05 作者: fodlder 時(shí)間: 2025-3-25 08:43 作者: 無(wú)能力之人 時(shí)間: 2025-3-25 14:29
E. Perchu?,H. Thyboks, so far, are written by specialists for specialists, with a heavy mathematical flavor, which is characteristic of the Calderon-Zygmund theory and related research of Duffin-Schaeffer, Daubechies, Grossman, Meyer, Morlet, Chui, and others. Randy Young‘s monograph is geared more towards practitione作者: 凝乳 時(shí)間: 2025-3-25 18:50
I. B. Morozov,E. A. Morozova,S. B. Smithsonstract relations in an infinite dimensional Hilbert space. It was shown that observables of a physical system can be represented by linear symmetric operators in a Hilbert space, and the eigenvalues and eigenfunctions of the particular operator that represents energy are energy levels of an electron作者: GEM 時(shí)間: 2025-3-25 20:02 作者: 思想靈活 時(shí)間: 2025-3-26 01:51 作者: 合乎習(xí)俗 時(shí)間: 2025-3-26 07:43
A. Levander,T. J. Henstock,G. R. Keller,E. D. Humphreys,L. W. Braile,K. G. Duekeralso used in the United States for high bit-rate point-to-point communications over twisted pairs (xDSL) and has been recently adopted for future broadband wireless radio local area networks (e.g. in the ETSI Broadband Radio Access Network: BRAN standardization effort for the air inteface of HIPERLA作者: RODE 時(shí)間: 2025-3-26 09:45
A. L. Halesonstruction after compression or other modification). Such applications include one-dimensional signals (sounds or other time-series), two-dimensional arrays (pictures or maps), and three-dimensional data (spatial diffusion). The ap- plications demonstrated here do not constitute recipes for real implementati978-1-4612-6823-9978-1-4612-0573-9作者: 付出 時(shí)間: 2025-3-26 13:56
G?ran Ekstr?m,Adam M. Dziewonskiares approximation, the discrete Fourier transform, and Fourier series. The third part explains the Fourier transform and then demonstrates how to apply basic Fourier analysis to designing and analyzing mathematical wavelets. Particular attention is paid to Daubechies wavelets. .?.Numerous exercises作者: 影響帶來(lái) 時(shí)間: 2025-3-26 17:02
Upper Mantle Heterogeneities from Active and Passive Seismology作者: 熱心助人 時(shí)間: 2025-3-27 00:52 作者: placebo-effect 時(shí)間: 2025-3-27 03:44 作者: Fester 時(shí)間: 2025-3-27 08:51
Rock Fracturing Processes Due to Nonlinear Shock Waves in Hot Fluid-Pressurized Domainsock with a velocity related to two different phenomena, each with its own velocity. Such propagations were called “B-convection” in the case of very small fluid diffusivity (impervious rocks such as clay or rocksalt), and “N-convection” in the case of higher permeabilities when nonlinear dissipative作者: certitude 時(shí)間: 2025-3-27 13:28 作者: 高談闊論 時(shí)間: 2025-3-27 17:31
Three-Dimensional Velocity Structure of the Earth’s Upper Mantle recent trends are towards smaller grid sizes and higher order expansions. (3) Larger data sets. Increasingly, very large collections of seismograms, and large numbers of observations obtained from seismograms, are incorporated in tomographic studies. The dramatically improved geographical coverage 作者: FRONT 時(shí)間: 2025-3-27 17:57 作者: defeatist 時(shí)間: 2025-3-27 23:19 作者: 新娘 時(shí)間: 2025-3-28 05:14 作者: meretricious 時(shí)間: 2025-3-28 08:29
Observation of teleseismic ,,/,, on super long-range profiles in northern Eurasia and their implicaty and velocity gradient. Long-range observations allow to define discrete velocity contrasts in the mantle, but again the models show a mantle which is mostly homogeneous on the scale of many wavelengths.作者: jovial 時(shí)間: 2025-3-28 11:29 作者: Interim 時(shí)間: 2025-3-28 14:43 作者: 輕打 時(shí)間: 2025-3-28 18:49
1389-1820 eismic models of thelithosphere-asthenosphere system. The two primary purposes ofthe present work are, first, to present these seismic observations onsuper long-range profiles in digitised format, using peaceful nuclearexplosions (PNE) in the former USSR, and, second, to present the jointthoughts of作者: 厚臉皮 時(shí)間: 2025-3-29 01:57 作者: –DOX 時(shí)間: 2025-3-29 03:53
Conservation of Lithospheric DSS-Datascientific community and discussed by experts from around the world for the implications on lithospheric models and the Comprehensive Test Ban Treaty (CTBT). After a brief reminder of the history of deep seismic sounding (DSS) of the lithospheric mantle, we will emphasize the need to conserve the ex作者: CHARM 時(shí)間: 2025-3-29 09:57
Major Features of the Mantle Velocity Structure beneath Northern Eurasia from Long-Range Seismic Recuity in the mantle transition zone (410–660 km depth) at 530–555 km depth. In addition, between 200 and 300 km depth beneath the younger East European platform, Uralides and West Siberian basin a prominent low velocity zone (perhaps the asthenospheric layer) is identified which seems to be absent un作者: 反對(duì) 時(shí)間: 2025-3-29 15:11 作者: 含糊 時(shí)間: 2025-3-29 18:57 作者: Myocarditis 時(shí)間: 2025-3-29 22:36
Central Siberia Upper Mantle Cross-Section from Deep Seismic Sounding Explosions Seismic Sounding profile RIFT. The analyses combine forward travel-time modeling and waveform matching using reflectivity synthetic seismograms. The sub-Moho velocity gradients are weak. A high gradient zone exists between 180 and 250-km depth which we identify with the Lehmann discontinuity. This 作者: 可互換 時(shí)間: 2025-3-30 02:03
Eurasian Mantle Structure Derived from the Records of Nuclear Explosions from nuclear explosions. Hundreds of events were recorded very clearly, particularly on the Baltic (Fennoscandian) shield and on seismic arrays (e.g. NORSAR and Gr?fenberg). The first arrivals and mantle reflections generated by nuclear explosions are usually clearly identified on seismograms due t作者: CRP743 時(shí)間: 2025-3-30 07:22 作者: 冥界三河 時(shí)間: 2025-3-30 11:30 作者: Matrimony 時(shí)間: 2025-3-30 13:57 作者: 滔滔不絕地說(shuō) 時(shí)間: 2025-3-30 17:12
Problems of Active Seismologymic processes and rheological characteristics of anomalous zones of earthquake preparation. Since nuclear explosions are prohibited, the vibroseismic method is the only active method for deep Earth’s sounding [1], [2].作者: 逢迎白雪 時(shí)間: 2025-3-30 21:52 作者: 極大痛苦 時(shí)間: 2025-3-31 04:35
Heterogeneity of the Uppermost Eurasian Mantle along the DSS Profile “Quartz”, Russiamical explosions. Our interpretation shows a 42-kin thick, high-velocity crust under the Baltic Shield, a 29-km thick crust and high-velocity upper mantle under the Mezenskaya depression, 52-km thick crust with high-velocity lower crust and uppermost mantle under the Urals, and 40-km thick crust und作者: 徹底檢查 時(shí)間: 2025-3-31 07:56 作者: 高度贊揚(yáng) 時(shí)間: 2025-3-31 11:12
Joint Inversion of Teleseismic Delay Times and Gravity Anomaly Data for Regional Structuresnship between density and velocity anomalies exists, the value of which is unknown and may vary in different regions of the model, especially with depth. Therefore, the correlation coefficient is treated as additional unknown parameter, leading to a non-linear (quasi Gaussian) inversion scheme. The 作者: Guaff豪情痛飲 時(shí)間: 2025-3-31 13:28
Teleseismic Tomography in Sweden-Denmark-Germany, Project TORthe transition between Proterozoic and Paleozoic Europe, the most prominent geological border line in Europe. It runs through Denmark, Sweden, Poland, Ukraine and Romania and is expected to show large lithospheric differences, based on previous studies. The project goes to depths of 200–300 km. The 作者: alleviate 時(shí)間: 2025-3-31 18:49
The 1995 U.S. Deep Probe Project1.25 km intervals along a roughly north-south line which extended along the North American Cordillera and across the Alberta plains from southern New Mexico to Edmonton, Alberta. The experiment has revealed profound differences in the structure of the crust and upper mantle north and south of the ea作者: Mercurial 時(shí)間: 2025-4-1 01:37 作者: gratify 時(shí)間: 2025-4-1 03:59
Book 1997els of thelithosphere-asthenosphere system. The two primary purposes ofthe present work are, first, to present these seismic observations onsuper long-range profiles in digitised format, using peaceful nuclearexplosions (PNE) in the former USSR, and, second, to present the jointthoughts of experts f作者: visceral-fat 時(shí)間: 2025-4-1 06:56
1389-1820 ience disciplines are presented. ..Audience:. The CTBT community and earth scientists interested inthe 3D structure of the lithosphere-asthenosphere system.978-90-481-4966-7978-94-015-8979-6Series ISSN 1389-1820 作者: 排他 時(shí)間: 2025-4-1 13:50 作者: manifestation 時(shí)間: 2025-4-1 15:18 作者: BRIEF 時(shí)間: 2025-4-1 21:50
