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標(biāo)題: Titlebook: Induced Seismicity; Harsh K. Gupta (Director),Rajender K. Chadha (Scie Book 1995 Birkh?user Verlag 1995 Geoinformationssysteme.Geologie.Ge [打印本頁]

作者: deferential    時間: 2025-3-21 18:44
書目名稱Induced Seismicity影響因子(影響力)




書目名稱Induced Seismicity影響因子(影響力)學(xué)科排名




書目名稱Induced Seismicity網(wǎng)絡(luò)公開度




書目名稱Induced Seismicity網(wǎng)絡(luò)公開度學(xué)科排名




書目名稱Induced Seismicity被引頻次




書目名稱Induced Seismicity被引頻次學(xué)科排名




書目名稱Induced Seismicity年度引用




書目名稱Induced Seismicity年度引用學(xué)科排名




書目名稱Induced Seismicity讀者反饋




書目名稱Induced Seismicity讀者反饋學(xué)科排名





作者: Lasting    時間: 2025-3-21 23:34
978-3-7643-5237-0Birkh?user Verlag 1995
作者: 嘲笑    時間: 2025-3-22 01:17
Induced Seismicity978-3-0348-9238-4Series ISSN 2504-3625 Series E-ISSN 2504-3633
作者: Radiation    時間: 2025-3-22 05:11

作者: 削減    時間: 2025-3-22 09:30
Assessment of Potential Strength of an Induced Earthquake by Using Fuzzy Multifactorial Evaluation,ing the method of fuzzy multifactorial evaluation from a fuzzy set theory. As an illustration of the above-mentioned method, this paper has applied the method to assessing the potential strength of induced earthquakes due to water reservoir.
作者: 畢業(yè)典禮    時間: 2025-3-22 14:22
Pageoph Topical Volumeshttp://image.papertrans.cn/i/image/463862.jpg
作者: SOW    時間: 2025-3-22 17:38
Harsh K. Gupta,R. K. Chadhap currents, resulting in inconsistent initial conditions and impulsive network variables that can not be handled by conventional numerical integration methods..To formulate the circuit equations of mixed-mode switching circuits, we have examined the reasons why only modified nodal analysis formulati
作者: 跳脫衣舞的人    時間: 2025-3-22 23:48

作者: 彈藥    時間: 2025-3-23 02:10
Elena O. Kremenetskaya,Victor M. Trjapitsinminimized by utilizing the adjoint network theory of periodically switched linear circuits presented in Chapter 10, in particular, the frequency reversal theorem. Distortion of several periodically switched nonlinear circuits has been analyzed and the results compare well with those from transient-F
作者: Cougar    時間: 2025-3-23 07:55

作者: Plaque    時間: 2025-3-23 13:12

作者: 鋸齒狀    時間: 2025-3-23 15:05
Mohamed Awad,Megume Mizoueminimized by utilizing the adjoint network theory of periodically switched linear circuits presented in Chapter 10, in particular, the frequency reversal theorem. Distortion of several periodically switched nonlinear circuits has been analyzed and the results compare well with those from transient-F
作者: 誘使    時間: 2025-3-23 21:42

作者: lambaste    時間: 2025-3-23 22:56
F. G. Piccinelli,M. Mucciarelli,P. Federici,D. Albarellon under a rich set of deformations. The variance accounted for between the experimental data and model data ranged from 79% for the Gasser et al. (.) model to 96% for the Bischoff et al. (.) model. Estimated pre-stresses ranged from 7 kPa in the lip region to 53 kPa in the central cheek region.
作者: 音樂等    時間: 2025-3-24 03:30
B. K. Rastogi,R. K. Chadha,C. S. P. Sarmavariety of input fluoroscopy views, both in terms of the time it takes to reconstruct bony anatomy and the accuracy of the reconstruction. Based on these initial findings, we conclude that this method shows promise for use in the operating room as an adjunct to conventional intra-operative imaging c
作者: Diastole    時間: 2025-3-24 07:44

作者: Arthr-    時間: 2025-3-24 11:28
V. S. Panfilov,G. A. Sobolevtions and other microstructural properties of the AC substructures are approximated by defining the approximate normalized depth. The pre-stressed state is calculated in around six hours, revealing the noted depth-dependent stresses. To facilitate future research, the PSA is open-sourced at ..
作者: degradation    時間: 2025-3-24 18:24
Deyi Feng,Xuejun Yu,Jinqping Gug. Results illustrate that the heating time for causing irreversible thermal damage to the entire tumor is 916 s using the selected laser intensity and spot size. Although cold-water droplets are sprayed at the skin surface to protect skin and its surrounding healthy tissue, it is found that collate
作者: 豐滿中國    時間: 2025-3-24 22:51

作者: 說笑    時間: 2025-3-24 23:41
Pradeep Talwanierical procedures of optimum design or solution of inverse problems. A nonlinear model in the framework of damage theory is presented in details for modeling and sensitivity analysis. The example of an elastic body with a rigid inclusion and a crack located at the boundary of the inclusion is consid
作者: Judicious    時間: 2025-3-25 06:20
U. Ravalerical procedures of optimum design or solution of inverse problems. A nonlinear model in the framework of damage theory is presented in details for modeling and sensitivity analysis. The example of an elastic body with a rigid inclusion and a crack located at the boundary of the inclusion is consid
作者: 傳染    時間: 2025-3-25 10:38
Mohamed Awad,Megume Mizoueerial. Restrictions on the strain energy function of the CPE have been developed which ensure that the CPE reproduces the exact constitutive response to all nonlinear homogeneous deformations. Consequently, the constitutive equations of the CPE analytically satisfy a nonlinear form of the patch test
作者: critic    時間: 2025-3-25 14:55

作者: Halfhearted    時間: 2025-3-25 16:58
nd generating some pathological scenarios related to AAFD before and after applying MCO. Results show that MCO reduces the biomechanical stress in both forefoot and hindfoot. However, as was expected, it generates some stress concentrations around the osteotomy region, which increases when it is use
作者: 流浪    時間: 2025-3-25 23:00
2504-3625 menon itself is still poorly understood. This reality thus makes the study of the induced seismicity very important and this volume timely.978-3-7643-5237-0978-3-0348-9238-4Series ISSN 2504-3625 Series E-ISSN 2504-3633
作者: 初次登臺    時間: 2025-3-26 02:49
Harsh K. Gupta (Director),Rajender K. Chadha (Scie
作者: 變白    時間: 2025-3-26 04:46
Book 1995ucive to this phenomenon. While the changes in pore-fluid pressure have been identified as the key factor in inducing earthquakes, the phenomenon itself is still poorly understood. This reality thus makes the study of the induced seismicity very important and this volume timely.
作者: acrobat    時間: 2025-3-26 10:53
Introduction,thquakes. Such earthquakes began to occur soon after the impoundment of the Shivajisagar Lake in 1962 and continue to occur, the latest being the 12th and 13th of March, 1995 earthquakes exceeding magnitude 4. With the advent of sophisticated instrumentation, borehole measurement, and advanced compu
作者: 騷擾    時間: 2025-3-26 14:06
Source Parameters of Mining-induced Seismic Events: An Evaluation of Homogeneous and Inhomogeneous itself (72 mm). By using Madariaga’s model for the asperity, the slip was over 3 times larger than observed. Peak velocity and acceleration scaling relations with magnitude were investigated by incorporating available South African data, appropriately reduced to Canadian geophysical conditions. The
作者: 魯莽    時間: 2025-3-26 17:17
The CQU Regional Seismic Network and Applications to Underground Mining in Central Queensland, Aust the structure of the Crust and Upper Mantle in Central Queensland..Techniques for monitoring rockbursts and longwall caving in mines are similar to those used for monitoring local earthquakes. CQU has successfully used a single triaxial seismometer to record seismic events produced by the strata fa
作者: Optometrist    時間: 2025-3-27 00:54

作者: FEAT    時間: 2025-3-27 04:02
Earthquake Activity in the Aswan Region, Egypt,the tomographic characteristics of the Aswan region (Awad and Mizoue, this issue), imply that the Aswan seismic activity must be regarded as consisting of two distinct earthquake groups..We also relocated the largest 500 earthquakes to determine their seismotectonic characteristics. The results reve
作者: galley    時間: 2025-3-27 07:33

作者: 歡樂東方    時間: 2025-3-27 11:41
Seismicity of the Koyna Region and Regional Tectonomagmatism of the Western Margin (India),nics strongly indicate that the western margin (WM) is a relic of a mobile arm (MA), that included Madagascar, and which formed a part of the Proterozoic mobile belt of ‘greater India’ (for . > Ma). The mobile nature of the WM facilitates mantle upwellings and transient elevation of isotherms at dep
作者: 勉強    時間: 2025-3-27 17:04
Tomographic Inversion for the Three-dimensional Seismic Velocity Structure of the Aswan Region, Egy crust. The first coincides with a graben structure located between the Kalabsha and Seiyal faults and the second exists between the N-S Kurkur fault and the main axis of Lake Aswan. Both low-velocity zones occupy an area of approximately 30 × 40 km, located along the western bank of the lake. The m
作者: 百科全書    時間: 2025-3-27 21:28

作者: Crumple    時間: 2025-3-28 01:00
Role of Dykes in Induced Seismicity at Bhatsa Reservoir, Maharashtra, India,. It is inferred that these dykes have acted as “barriers” for the diffusion of water from the reservoir, thereby becoming zones of instability due to increased pore pressure not only along them but also over the volume they bound.
作者: jocular    時間: 2025-3-28 04:14

作者: GUISE    時間: 2025-3-28 07:48
2504-3625 f Earth‘s Interior (IASPEI) in Wellington, New Zealand during January 10-21, 1994. This volume presents a collection of 16 papers accepted for publication which accrued from this workshop. The first three papers address mining activity related to induced seismicity. The fourth paper deals with water
作者: 處理    時間: 2025-3-28 12:30
Book 1995Interior (IASPEI) in Wellington, New Zealand during January 10-21, 1994. This volume presents a collection of 16 papers accepted for publication which accrued from this workshop. The first three papers address mining activity related to induced seismicity. The fourth paper deals with water injection
作者: Ischemia    時間: 2025-3-28 17:35
Investigations of June 7, 1988 Earthquake of Magnitude 4.5 near Idukki Dam in Southern India,this earthquake sequence does not qualify to be categorized as induced. The trend of the aftershocks, composite fault plane solution and local tectonics point towards reactivation of a NW-SE fault along the Kallar river. The existence of such a fault is also supported by gravity studies.
作者: 禁止    時間: 2025-3-28 18:46

作者: 忘川河    時間: 2025-3-28 23:57
Induced Seismicity in the Khibiny Massif (Kola Peninsula),ting a trigger mechanism. The largest earthquake, which occurred on 16 April 1989 (.. = 4.1) could be traced along the surface for 1200 m and observed to a depth of at least 220 m. The maximum measured displacement was 15–20 cm.
作者: 十字架    時間: 2025-3-29 03:40

作者: 代替    時間: 2025-3-29 09:28
Introduction,United States of America during the late 1930s. During the 1960s several earthquakes exceeding magnitude 6 occurred in the vicinity of artificial water reservoirs at Xinfengjiang, China (1962); Kariba, Zambia-Zimbabwe border (1963); Cremasta, Greece (1966); and Koyna, India (1967). Over the years, t
作者: patriarch    時間: 2025-3-29 11:46
Source Parameters of Mining-induced Seismic Events: An Evaluation of Homogeneous and Inhomogeneous events located between 640 and 825 m depth at Strathcona mine, Ontario, and having magnitudes ranging between .. 0.8 and 2.7. The derived Brune static stress drops were found to be similar to those observed for natural earthquakes (~ 30 bars), whereas dynamic stress drops were found to range up to
作者: epicardium    時間: 2025-3-29 16:23

作者: 讓步    時間: 2025-3-29 22:18
The CQU Regional Seismic Network and Applications to Underground Mining in Central Queensland, Austmeter stations. The array has an aperture of about 50 km. CQU is able to resolve epicentral co-ordinates to about ± 2 kilometres, with a sample rate of 100 per second, and an absolute time accuracy of 100 milliseconds. This resolution is achieved by using triaxial seismometers which allow better sec
作者: Culmination    時間: 2025-3-30 00:48

作者: Dysarthria    時間: 2025-3-30 06:36
Earthquake Activity in the Aswan Region, Egypt,akes, and is investigated in this study. Earthquake data from June 1982 to late 1991, collected from the Aswan network, are classified into two sets on the basis of focal depth (i.e., shallow, or deeper than 10 km). It is determined that (a) shallow seismicity is characterized by swarm activity, whe
作者: Gratuitous    時間: 2025-3-30 08:40

作者: 厭食癥    時間: 2025-3-30 13:17
The Microseismic Network of the Ridracoli Dam, North Italy: Data and Interpretations,D station. Earthquakes were recorded with completeness from magnitude 0.8 onwards. In the same period, all the parameters relevant to the dam and the environment were measured. This provided a complete data base for RIS studies, unique in its kind in Italy. The main findings of the analyses performe
作者: 健忘癥    時間: 2025-3-30 19:18
Investigations of June 7, 1988 Earthquake of Magnitude 4.5 near Idukki Dam in Southern India,f 5 seismic stations, the aftershocks which continued for 3 1/2 months were monitored. The hypocentral parameters, b value, ../.. ratio indicate that this earthquake sequence does not qualify to be categorized as induced. The trend of the aftershocks, composite fault plane solution and local tectoni
作者: neutralize    時間: 2025-3-31 00:15

作者: 彎彎曲曲    時間: 2025-3-31 02:28

作者: ADJ    時間: 2025-3-31 08:33
Assessment of Potential Strength of an Induced Earthquake by Using Fuzzy Multifactorial Evaluation,ing the method of fuzzy multifactorial evaluation from a fuzzy set theory. As an illustration of the above-mentioned method, this paper has applied the method to assessing the potential strength of induced earthquakes due to water reservoir.
作者: 食品室    時間: 2025-3-31 11:04

作者: CONE    時間: 2025-3-31 13:30

作者: Mindfulness    時間: 2025-3-31 19:11

作者: Chandelier    時間: 2025-4-1 01:36
Tomographic Inversion for the Three-dimensional Seismic Velocity Structure of the Aswan Region, Egyof Egypt. The tomographic inversion presented in this study is based on 1131 .-phase observations at 13 stations from 89 local earthquakes, all of which occurred within the Kalabsha fault zone. The assumed initial velocity model is that deduced from local explosion experiments. The results indicate
作者: WAG    時間: 2025-4-1 05:39





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