標(biāo)題: Titlebook: Earthquake Prediction and Rock Mechanics; Max Wyss Book 1975 Springer Basel AG 1975 behavior.deformation.granite.Gravity.high pressure.mag [打印本頁] 作者: opioid 時間: 2025-3-21 18:30
書目名稱Earthquake Prediction and Rock Mechanics影響因子(影響力)
書目名稱Earthquake Prediction and Rock Mechanics影響因子(影響力)學(xué)科排名
書目名稱Earthquake Prediction and Rock Mechanics網(wǎng)絡(luò)公開度
書目名稱Earthquake Prediction and Rock Mechanics網(wǎng)絡(luò)公開度學(xué)科排名
書目名稱Earthquake Prediction and Rock Mechanics被引頻次
書目名稱Earthquake Prediction and Rock Mechanics被引頻次學(xué)科排名
書目名稱Earthquake Prediction and Rock Mechanics年度引用
書目名稱Earthquake Prediction and Rock Mechanics年度引用學(xué)科排名
書目名稱Earthquake Prediction and Rock Mechanics讀者反饋
書目名稱Earthquake Prediction and Rock Mechanics讀者反饋學(xué)科排名
作者: 聽覺 時間: 2025-3-22 00:04
Clifford Algebra in Euclidean 3-Space,me these data permit quantitative comparison of seismic velocities or their ratio and dilatant volumetric strain. In air-dry samples ../.. decreases by a few per cent at strains of 10.; in saturated materials with high pore pressure, ../.. increases by a comparable amount. Decreases in seismic veloc作者: Predigest 時間: 2025-3-22 00:24
A New Approach to Dogs and Dog Trainingn uniaxial stress. Excess pore fluid (kerosene) is available during the deformations which are performed under light confinement (2.5 MPa) at an average strain rate of about 5 × 10. s.. ../.. increases monotonically with shear stress (～13%) until failure. These data are consistent with either: 1) a 作者: HATCH 時間: 2025-3-22 07:24
https://doi.org/10.1007/978-94-015-1138-4ace and pressure vessel. Suitable choice of materials allowed the transmission of signals sufficiently large for measurement and analysis. Acoustic emissions were also monitored during the fracture runs at room temperature and could be compared with earlier studies. As observed previously, the emiss作者: 鍵琴 時間: 2025-3-22 11:36
Yoshinori Hara,Senko Ikenobo,Spring H. Hanthe biaxial compression tests have been chosen. During the deformation the cross-like zone, consisting of a great number of small cracks, appeared followed by the development of macrofracture in the central part of the specimen. The strong minimums in velocity of ultrasonic waves, changes of strain 作者: nepotism 時間: 2025-3-22 16:24
Robyn Klingler-Vidra,Yu Ching Kuo shield has been examined. For samples with an induced IRM parallel to the axis of compression, remanent magnetization decreased linearly up to the onset of dilatancy. As increased stress produced additional dilatancy, the variation of remanent magnetization became nonlinear, and the stress dependen作者: nepotism 時間: 2025-3-22 17:37
Brazil: MSMEs Development and Prospects, of 6 kb the amount of stable creep is very small or absent. Two orders of magnitude change in strain rate has no effect on the distance of stable sliding. Our results suggest that in the earth, fault creep should predominate in the shallow crust but in the deep crustal layer most of the stresses ar作者: mechanism 時間: 2025-3-22 23:50 作者: 低三下四之人 時間: 2025-3-23 03:05
https://doi.org/10.1007/978-3-030-20675-8e surface and at shallow depths..It is consistent with the available geochemical data that such gouges can exist at depths down to 10 km. If extensive gouge materials exist in a fault zone then their properties will determine, to a large extent, the behavior of the fault. From known properties of cl作者: 手術(shù)刀 時間: 2025-3-23 09:29 作者: homocysteine 時間: 2025-3-23 12:15 作者: Individual 時間: 2025-3-23 14:36
Fundamental Aspects of Scattering,nto the dilatant zone produces further elastic uplift. Since the time between resaturation of the dilatant zone and the earthquake is shorter than the life of the ../.. anomaly, the elastic uplift is less than the inelastic. The magnitude of the ../.. anomaly gives a lower bound on the compressibili作者: Fabric 時間: 2025-3-23 21:43 作者: muscle-fibers 時間: 2025-3-23 23:22
Generative-Transformational Grammar,on the basis of a dilatancy model. It is demonstrated that the precursor time interval (τ) vs. . relation approximately fits in that for the τ vs. typical length of earthquake zone provided the above formulas hold good. A diffusion process in a dilatant region seems also to account for these approxi作者: Omniscient 時間: 2025-3-24 05:58 作者: Entrancing 時間: 2025-3-24 07:31 作者: exercise 時間: 2025-3-24 12:24
Background and State of the Art,ted in the model is that dilatancy is caused by the opening of cracks, where the cracks open in the least compressive stress direction .., 1966). Its simplicity and compatibility with numerical techniques, involving the simulation of both static and dynamic stress fields, permits prediction of dilat作者: 多節(jié) 時間: 2025-3-24 15:12 作者: 自然環(huán)境 時間: 2025-3-24 21:21
Sapna Raghav,Ritu Painuli,Dinesh Kumarchanges very little down the transition so that changes in rock resistivity will be almost solely due to dilatant volume change. Experiments with partly saturated rocks at room temperature suggest that rocks containing mixtures of fluid and vapor, along the transition, will generally behave electric作者: cluster 時間: 2025-3-24 23:36 作者: 破裂 時間: 2025-3-25 05:15 作者: 慢跑 時間: 2025-3-25 09:45 作者: 異端邪說下 時間: 2025-3-25 13:07 作者: Ejaculate 時間: 2025-3-25 16:33 作者: Enliven 時間: 2025-3-25 21:13 作者: airborne 時間: 2025-3-26 01:34 作者: cloture 時間: 2025-3-26 07:45 作者: semiskilled 時間: 2025-3-26 11:00 作者: Dri727 時間: 2025-3-26 15:37
A Theoretical Model of the Dilatant Behavior of a Brittle Rock,simplicity and compatibility with numerical techniques, involving the simulation of both static and dynamic stress fields, permits prediction of dilatancy induced effects for stress states and loading conditions which are not experimentally attainable.作者: 推崇 時間: 2025-3-26 17:58 作者: 致詞 時間: 2025-3-26 22:08 作者: 宏偉 時間: 2025-3-27 03:15 作者: 逢迎春日 時間: 2025-3-27 08:07 作者: MITE 時間: 2025-3-27 12:21
Sapna Raghav,Ritu Painuli,Dinesh Kumarally during dilatancy as though they were fluid saturated. Observed resistivity changes before earthquakes give the dilatant volume change directly and thus may be used to further constrain the dilatancy-diffusion model, independent of observed uplift or velocity changes.作者: acrophobia 時間: 2025-3-27 15:40
Clifford Algebra in Euclidean 3-Space,r results suggest that such anomalies will occur only in regions where pore fluid source to sink dimensions are of the order of 10 km or more, or in regions where the rocks are not saturated to begin with.作者: 小畫像 時間: 2025-3-27 19:57 作者: canvass 時間: 2025-3-28 01:39
Yoshinori Hara,Senko Ikenobo,Spring H. Hanlowed by the development of macrofracture in the central part of the specimen. The strong minimums in velocity of ultrasonic waves, changes of strain rate, and self-electric potential reliably pointed to the approaching moment of failure.作者: Calibrate 時間: 2025-3-28 04:43 作者: Missile 時間: 2025-3-28 09:34
https://doi.org/10.1007/978-3-030-20675-8 gouge materials exist in a fault zone then their properties will determine, to a large extent, the behavior of the fault. From known properties of clays in the presence of water we can infer that, in such cases, the tectonic stress and the stress drops for earthquakes will be low and substantial creep will take place before earthquakes.作者: Antigen 時間: 2025-3-28 13:17 作者: 地名表 時間: 2025-3-28 15:05
,,/,, in Saturated Granodiorite Loaded to Failure,high rate of fluid flow of the same order as the increase in dilatant volume with time; or 2) an increase in total porosity with a decrease in mean aspect ratio of the pores (MPa = 10. N/m. ? 10 bars).作者: hypertension 時間: 2025-3-28 22:18
Dilatancy and Crustal Uplift,ty of the dilatant zone. Velocity and uplift measurements lead to the conclusion that if dilatancy occurred before the 1971 San Fernando earthquake, the pore pressure in the hypocentral region at the time of the event must have been at least an order of magnitude below hydrostatic.作者: Conducive 時間: 2025-3-28 23:03
Theory of Earthquakes,, are shown to be a natural consequence of the physical processes leading to failure in dry rock. The effects of fluids on failure in the focal region of a potential earthquake are considered in terms of the scale independent inclusion theory.作者: Verify 時間: 2025-3-29 04:11 作者: malapropism 時間: 2025-3-29 08:09 作者: paroxysm 時間: 2025-3-29 13:06 作者: Aromatic 時間: 2025-3-29 15:41
,,/,, in Saturated Granodiorite Loaded to Failure,n uniaxial stress. Excess pore fluid (kerosene) is available during the deformations which are performed under light confinement (2.5 MPa) at an average strain rate of about 5 × 10. s.. ../.. increases monotonically with shear stress (～13%) until failure. These data are consistent with either: 1) a 作者: Ambulatory 時間: 2025-3-29 20:25
Acoustic Emission During High-Temperature Frictional Sliding,ace and pressure vessel. Suitable choice of materials allowed the transmission of signals sufficiently large for measurement and analysis. Acoustic emissions were also monitored during the fracture runs at room temperature and could be compared with earlier studies. As observed previously, the emiss作者: Facilities 時間: 2025-3-30 02:25 作者: 財產(chǎn) 時間: 2025-3-30 06:28
Magnetism of Rocks and Volumetric Strain in Uniaxial Failure Tests, shield has been examined. For samples with an induced IRM parallel to the axis of compression, remanent magnetization decreased linearly up to the onset of dilatancy. As increased stress produced additional dilatancy, the variation of remanent magnetization became nonlinear, and the stress dependen作者: 人類 時間: 2025-3-30 11:22 作者: COST 時間: 2025-3-30 14:50
The Sliding Characteristics of Sandstone on Quartz Fault-Gouge, Tennessee Sandstone sliding on an artificial layer of quartz gouge; 2) fractured Coconino Sandstone sliding along experimentally produced shear fractures; and 3) a fine-grained quartz aggregate deformed in compression. The specimens were deformed to 2.0 kb confining pressure at room temperature and作者: rods366 時間: 2025-3-30 19:29
Clay Gouges in the San Andreas Fault System and their Possible Implications,e surface and at shallow depths..It is consistent with the available geochemical data that such gouges can exist at depths down to 10 km. If extensive gouge materials exist in a fault zone then their properties will determine, to a large extent, the behavior of the fault. From known properties of cl作者: 繼而發(fā)生 時間: 2025-3-30 21:17 作者: angina-pectoris 時間: 2025-3-31 01:26 作者: DRILL 時間: 2025-3-31 05:42
Dilatancy and Crustal Uplift,nto the dilatant zone produces further elastic uplift. Since the time between resaturation of the dilatant zone and the earthquake is shorter than the life of the ../.. anomaly, the elastic uplift is less than the inelastic. The magnitude of the ../.. anomaly gives a lower bound on the compressibili作者: 使人入神 時間: 2025-3-31 11:29
Aseismic Faulting Following the 1973 Nemuro-Oki Earthquake, Hokkaido, Japan (a possibility),sula, Hokkaido, Japan, 17 June, 1973. The main purpose of this paper is to obtain a comprehensive view of the land movement in eastern Hokkaido with respect to the seismic cycle there. This region, particularly the Nemuro peninsula area, has been subject to extensive land subsidence in the past seve作者: 譏諷 時間: 2025-3-31 16:21
Dilatancy Model and Empirical Formulas for an Earthquake Area,on the basis of a dilatancy model. It is demonstrated that the precursor time interval (τ) vs. . relation approximately fits in that for the τ vs. typical length of earthquake zone provided the above formulas hold good. A diffusion process in a dilatant region seems also to account for these approxi作者: condescend 時間: 2025-3-31 18:14 作者: 尾隨 時間: 2025-4-1 01:04
Two Models for Earthquake Forerunners,cal models are used to explain these phenomena. According to a model developed by US seismologists, the so-called dilatancy diffusion model, the earthquake occurs near maximum stress, following a period of dilatant crack expansion. Diffusion of water in and out of the dilatant volume is required to 作者: 軌道 時間: 2025-4-1 03:38
A Theoretical Model of the Dilatant Behavior of a Brittle Rock,ted in the model is that dilatancy is caused by the opening of cracks, where the cracks open in the least compressive stress direction .., 1966). Its simplicity and compatibility with numerical techniques, involving the simulation of both static and dynamic stress fields, permits prediction of dilat作者: 性學(xué)院 時間: 2025-4-1 08:01
A Note on the Constitutive Law for Dilatancy,e law. For a power law of the form . (where γ is dilatant strain, δ is a constant and .. is the deviatoric stress invariant) the ratio of dilatant scale to depth of faulting is significantly less than unity for . = 2 (‘microcrack dilatancy’), about unity for . = 1 (‘joint dilatancy’), and much large作者: Obstreperous 時間: 2025-4-1 11:09
Dilatancy-Related Electrical Resistivity Changes in Rocks,changes very little down the transition so that changes in rock resistivity will be almost solely due to dilatant volume change. Experiments with partly saturated rocks at room temperature suggest that rocks containing mixtures of fluid and vapor, along the transition, will generally behave electric
