標題: Titlebook: Geophysical Data Inversion Methods and Applications; Proceedings of the 7 Andreas Vogel,Charles O. Ofoegbu,Bjorn Ursin Conference proceedin [打印本頁] 作者: incontestable 時間: 2025-3-21 18:22
書目名稱Geophysical Data Inversion Methods and Applications影響因子(影響力)
書目名稱Geophysical Data Inversion Methods and Applications影響因子(影響力)學科排名
書目名稱Geophysical Data Inversion Methods and Applications網(wǎng)絡(luò)公開度
書目名稱Geophysical Data Inversion Methods and Applications網(wǎng)絡(luò)公開度學科排名
書目名稱Geophysical Data Inversion Methods and Applications被引頻次
書目名稱Geophysical Data Inversion Methods and Applications被引頻次學科排名
書目名稱Geophysical Data Inversion Methods and Applications年度引用
書目名稱Geophysical Data Inversion Methods and Applications年度引用學科排名
書目名稱Geophysical Data Inversion Methods and Applications讀者反饋
書目名稱Geophysical Data Inversion Methods and Applications讀者反饋學科排名
作者: 單片眼鏡 時間: 2025-3-21 21:05
Mineral Deposits and Metallogenic Conceptserative inversion for seismic and gravimetric data is discussed in detail. It is noted that uniqueness for cooperative inversion arises regardless of the uniqueness of inversion for both seismic and gravimetric data for 3-D inhomogeneous media.作者: eulogize 時間: 2025-3-22 02:11
Cooperative Approach to Solving Inverse Problems in Integral Geophysics (Theoretical Aspects)erative inversion for seismic and gravimetric data is discussed in detail. It is noted that uniqueness for cooperative inversion arises regardless of the uniqueness of inversion for both seismic and gravimetric data for 3-D inhomogeneous media.作者: 濃縮 時間: 2025-3-22 04:43 作者: Incommensurate 時間: 2025-3-22 12:26
https://doi.org/10.1007/978-1-349-16679-4vity anomalies due to a horizontal cylinder can also be used to interpret the gravity anomalies due to a fault. The method is easy to apply, but may be automated if desired. The method is tested on a field example from the Gulf of Suez region, Egypt.作者: 幼兒 時間: 2025-3-22 14:43
https://doi.org/10.1007/978-3-319-04639-6n. Furthermore, the density perturbations under subduction zones show the penetration of downwelling slabs into the lower mantle, which means that a model of whole mantle convection is favored over stratified convection divided by sharp chemical boundary near the 650-km discontinuity.作者: 幼兒 時間: 2025-3-22 20:02
A Statistical Approach to Depth Determination from Gravity Gradientsvity anomalies due to a horizontal cylinder can also be used to interpret the gravity anomalies due to a fault. The method is easy to apply, but may be automated if desired. The method is tested on a field example from the Gulf of Suez region, Egypt.作者: Armory 時間: 2025-3-22 22:46 作者: 卷發(fā) 時間: 2025-3-23 02:56 作者: 詼諧 時間: 2025-3-23 07:03
https://doi.org/10.1007/978-981-10-6074-8 by . which has some relations to a robustified Krige type prediction. The performance of the proposed iteration scheme with particular regard to its convergence properties is shown by an example from geodesy.作者: Oscillate 時間: 2025-3-23 12:56 作者: 紡織品 時間: 2025-3-23 14:04 作者: Latency 時間: 2025-3-23 18:02 作者: FEIGN 時間: 2025-3-24 01:33
Overview: 978-3-528-06396-2978-3-322-89416-8作者: prediabetes 時間: 2025-3-24 02:58 作者: predict 時間: 2025-3-24 10:27
https://doi.org/10.1007/978-1-4615-5143-0here. The basic reason was because of their polynomial nature and their simple mathematical structure. There are, however, several disadvantages in applying spherical harmonics, for example the computability of spherical harmonics of higher orders, oscillating properties in interpolation, and convergence problems in series expansions.作者: mortgage 時間: 2025-3-24 10:55 作者: 嬉耍 時間: 2025-3-24 16:47
https://doi.org/10.1007/978-1-349-03855-8ion is paid to the paleomagnetic case. Modelling of insufficient and nonuniformly scattered data required the introduction of a new technique for solving the Least (±) Squares Problem arising from the “global data fitting”.作者: 廣口瓶 時間: 2025-3-24 23:04 作者: 怕失去錢 時間: 2025-3-24 23:44 作者: amorphous 時間: 2025-3-25 04:20
Obtaining Materic Bodies through Concentration and Optimization of a Linear Functionalmateric (from the Latin word mater = mother) The method originates from Zidarov’s concentration method which, in general, is not uniquely determined. We determine this method by adding a linear functional which should be minimized at every step.作者: reaching 時間: 2025-3-25 10:10 作者: 鞭打 時間: 2025-3-25 13:36
https://doi.org/10.1007/978-3-322-89416-8Algorithmen; Anomalie; Base; Element; Experiment; Geophysik; Metall; Mineral; Penetration; Potential; Streuthe作者: PLIC 時間: 2025-3-25 16:15 作者: glacial 時間: 2025-3-25 22:53
Boundary Element Analysis of Inverse Problems of Linear ViscoelasticityApplying Laplace transform boundary integral equations for initial boundary value problems of the linear viscoelasticity are derived. Then the inverse problem, when the solution is given at t = t. , is formulated and analysed.作者: invert 時間: 2025-3-26 01:38
Geophysical Data Inversion Methods and ApplicationsProceedings of the 7作者: ADAGE 時間: 2025-3-26 07:12 作者: stroke 時間: 2025-3-26 12:00 作者: meretricious 時間: 2025-3-26 15:14 作者: 流浪 時間: 2025-3-26 19:29
Optimisation of Magnetic Anomalies via Singular Value Decompositiontion of three smoothing factors varying with decrease of the objective function, results in more stable iterations than using single factors. The addition of a small number less than 1.0 on singular values as damping factor, increases the rate of convergence slightly in comparison with no damping, w作者: 無意 時間: 2025-3-26 22:10 作者: Flatus 時間: 2025-3-27 02:48 作者: 祖先 時間: 2025-3-27 07:12
,Bretton Woods in Action, 1959–1973,material to another one is no longer by crossing the boundary between two layers but can still be identified approximately as the place where the parameters quite rapidly vary. In most models of either kind the geometries are exceedingly simple — one or two dimensional only : one aims at obtaining t作者: 鬼魂 時間: 2025-3-27 09:40 作者: Coordinate 時間: 2025-3-27 14:42 作者: 戲服 時間: 2025-3-27 19:25 作者: CERE 時間: 2025-3-28 01:16 作者: discord 時間: 2025-3-28 05:46
Robust Predictors and an Alternative Iteration Scheme for Ill-posed Problemsom effects models. Hence not only the iteration scheme of . (1979) or . (1984) can easily be derived in full analogy to the . (Best inhomogeneously LInear Predictor), but also an apparently new scheme is readily developed following the . (Best homogeneously Linear weakly Unbiased Predictor) approach作者: cognizant 時間: 2025-3-28 08:12 作者: Cosmopolitan 時間: 2025-3-28 12:25
Cooperative Approach to Solving Inverse Problems in Integral Geophysics (Theoretical Aspects)ta for different geophysical methods allow one to extend the uniqueness and stability domain with respect to the separate inversion. It is also shown that the cooperative inversion brings about the increase of the accuracy of the solution and its noise stability. There is proposed a constructive alg作者: amplitude 時間: 2025-3-28 15:03 作者: AORTA 時間: 2025-3-28 20:38 作者: 表示向前 時間: 2025-3-29 00:19
Obtaining Materic Bodies through Concentration and Optimization of a Linear Functionalmateric (from the Latin word mater = mother) The method originates from Zidarov’s concentration method which, in general, is not uniquely determined. We determine this method by adding a linear functional which should be minimized at every step.作者: PRE 時間: 2025-3-29 04:29 作者: anaerobic 時間: 2025-3-29 10:42
Optimisation of Magnetic Anomalies via Singular Value Decompositionnetic anomalies. The algorithm used in decomposing the matrix is the compact version developed by Nash. The Jacobian matrix is factorised in three matrices, one of which is the diagonal matrix containing singular values. The three matrices together with residual vector are used to calculate the para作者: foppish 時間: 2025-3-29 12:54
A Statistical Approach to Depth Determination from Gravity Gradients the present paper, an interpretive technique based on the correlation factors is formulated in the case of first horizontal and vertical derivatives of gravity due to two geometries: the sphere, and the horizontal cylinder. It is demonstrated that correlation values can be used to determine the dep作者: foppish 時間: 2025-3-29 16:32 作者: farewell 時間: 2025-3-29 20:04 作者: 過去分詞 時間: 2025-3-30 03:21 作者: Allege 時間: 2025-3-30 05:30 作者: 來就得意 時間: 2025-3-30 10:14 作者: 譏笑 時間: 2025-3-30 12:25 作者: 有說服力 時間: 2025-3-30 18:51
Why Emigrants Do Not Return to Albania,specimen. More specifically, a macroscopic physical property in a given direction is the mean value of the corresponding property of the individual crystallites with respect to the statistical distribution of their orientations. Thus, the orientation distribution is a mathematical approach of descri作者: Postulate 時間: 2025-3-31 00:12
Mineral Deposits and Metallogenic Conceptsta for different geophysical methods allow one to extend the uniqueness and stability domain with respect to the separate inversion. It is also shown that the cooperative inversion brings about the increase of the accuracy of the solution and its noise stability. There is proposed a constructive alg作者: 物種起源 時間: 2025-3-31 02:18
