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標題: Titlebook: Advancing Culture of Living with Landslides; Volume 4 Diversity o Matja? Miko?,Nicola Casagli,Kyoji Sassa Conference proceedings 2017 Sprin [打印本頁]

作者: Encounter    時間: 2025-3-21 16:58
書目名稱Advancing Culture of Living with Landslides影響因子(影響力)




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書目名稱Advancing Culture of Living with Landslides被引頻次




書目名稱Advancing Culture of Living with Landslides被引頻次學科排名




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書目名稱Advancing Culture of Living with Landslides年度引用學科排名




書目名稱Advancing Culture of Living with Landslides讀者反饋




書目名稱Advancing Culture of Living with Landslides讀者反饋學科排名





作者: 受辱    時間: 2025-3-21 23:50

作者: 壯麗的去    時間: 2025-3-22 02:54
https://doi.org/10.1007/978-3-319-53485-5Landslide science; Landslide forms; Earthquake-induced landslides; Rainfall-induced landslides; Rapid la
作者: 散步    時間: 2025-3-22 07:24
978-3-030-10415-3Springer International Publishing AG 2017
作者: 誘騙    時間: 2025-3-22 12:33
https://doi.org/10.1007/978-94-015-8275-9This session is devoted to the description of events, processes and mechanisms associated to the occurrence of landslides triggered by earthquakes. Fourteen manuscripts have been submitted to this session.
作者: macrophage    時間: 2025-3-22 13:00
Session Introduction Earthquake-Induced LandslideThis session is devoted to the description of events, processes and mechanisms associated to the occurrence of landslides triggered by earthquakes. Fourteen manuscripts have been submitted to this session.
作者: Efflorescent    時間: 2025-3-22 18:38
The New Synthese Historical Library Landslides, as any geological phenomena, formed due to simultaneous action of exogenous and endogenous forces. We consider simultaneous formation in the different areas of large landslides caused by the influence of these forces as a trigger effect. The nature of this connection, it is not only cha
作者: Engaging    時間: 2025-3-23 00:09

作者: AVANT    時間: 2025-3-23 02:10

作者: 大罵    時間: 2025-3-23 06:01
https://doi.org/10.1007/978-3-030-86622-8g Newmark displacement analysis. The critical displacement, usually obtained from laboratory shear tests under low and constant shear rates, is defined as the coseismic displacement beyond which strength of sliding surface reach residual values. The typical value ranges a few centimeters, depending
作者: 機構(gòu)    時間: 2025-3-23 11:21

作者: 星星    時間: 2025-3-23 15:58

作者: 咯咯笑    時間: 2025-3-23 19:39
CoCo Bonds and Bail-in Mechanism,ms to reevaluate the earthquake-induced landslides occurred at the time of The 2015 Nepal Gorkha Earthquake. In the analysis, nonlinear material properties of the ground as well as 3D topography, geological conditions and input motion are taken into account appropriately. Those factors strongly infl
作者: Assignment    時間: 2025-3-24 00:47

作者: pacific    時間: 2025-3-24 03:07
https://doi.org/10.1057/97811374916269,332 landslides have been identified covering 61.5?km. of land in about 20,500 km. area of investigation using Google Earth imagery. Their spatial distribution characteristics and relation to the triggering mechanism is studied. Interesting regional localization and angular distribution characteris
作者: 平項山    時間: 2025-3-24 09:29
https://doi.org/10.1057/9781137491626than 1700 geohazards, most notably the large Hongshiyan, Wangjiapo, and Ganjiazhai landslides. In 2014, the Jinggu (.. 6.6) and Yingjiang (.. 6.1) earthquakes also occurred in the same region. In this study, the authors compared the relationships between geohazards and earthquake magnitude, fault ac
作者: 擦掉    時間: 2025-3-24 14:34
Person-Affecting Principles and Beyond,luses and natural slopes of an area characterized by low relief. These instabilities were characterized by: (1) very small size, most of them with volumes lower than 1?m., and (2) to occur in rock masses affected by multiple discontinuities, which pre-defined blocks that fell down during the shaking
作者: 變異    時間: 2025-3-24 17:11

作者: Reclaim    時間: 2025-3-24 22:09
https://doi.org/10.1007/978-94-007-2765-6e Julian Alps. The application of intensity scales based mainly on damage to buildings was limited in the epicentral area, because it is a high mountain area and thus very sparsely populated. On the other hand the effects on the natural environment were prominent and widespread. These facts and the
作者: 死亡率    時間: 2025-3-25 02:27

作者: CHECK    時間: 2025-3-25 06:15

作者: Spina-Bifida    時間: 2025-3-25 09:44
Mathematical Problems Posed by the Theory,es from the period 2000–2014 were analyzed on a regional scale, using existing climatic and landslide regionalizations. The classification provides a time series of landslide classes and Kruskal-Wallis tests and chi-tests were conducted to analyze how well the classification performs for each landsl
作者: 滔滔不絕地說    時間: 2025-3-25 13:46
Conference proceedings 2017ternational Consortium on Landslides and President of the Slovenian NationalPlatform for Disaster Risk Reduction..Prof. Nicola Casagli is Founding member of the International Consortium on Landslides(ICL), professor at the University of Florence and founder of the UNESCO Chair on geohydrological haz
作者: 過分自信    時間: 2025-3-25 18:44

作者: follicular-unit    時間: 2025-3-25 21:11

作者: Irrepressible    時間: 2025-3-26 00:44

作者: Minikin    時間: 2025-3-26 06:28

作者: 清楚    時間: 2025-3-26 10:42
Geophysical Investigation of the Landslide-Prone Slope Downstream from the Rogun Dam Construction Sih assessment of possible landslide risk scenarios. This report describes the main results of the comprehensive studies, calculations and dynamic modeling of stability of the right-bank landslide-prone slope, which suggest that the potentially unstable mass of strongly weathered rocks with the volume
作者: gusher    時間: 2025-3-26 16:16

作者: Dna262    時間: 2025-3-26 20:41

作者: 冷淡一切    時間: 2025-3-26 21:43

作者: LIKEN    時間: 2025-3-27 04:52

作者: bibliophile    時間: 2025-3-27 07:33

作者: 某人    時間: 2025-3-27 10:10

作者: 不幸的人    時間: 2025-3-27 17:38
https://doi.org/10.1007/978-3-319-67378-3d by this earthquake surpassed some events of M?=?7 or greater due to the serious landslides disaster. Base on the distribution features of coseismic landslides caused by the Ludian earthquake, this paper analyses the statistics relationship between the local terrain relief condition and large lands
作者: 宣傳    時間: 2025-3-27 19:52
https://doi.org/10.1007/978-3-030-86622-8anent displacement before rapid slide occurred. The influence of the strength and seismic parameters on the newly defined critical displacement is assessed using Newmark displacement analysis incorporating velocity-displacement dependent friction law. The dip angle of sliding surface is assumed as 1
作者: Decline    時間: 2025-3-28 00:33
Evans and the Varieties of Contingency, as inputs for 2D, 2.5D and 3D dynamic numerical simulations completed with the UDEC (Itasca) software. For some sites, a full back-analysis was carried out to assess the possibility of a seismic triggering of the landslide. For others, we simulated a series of possible future earthquake scenarios a
作者: 憤慨一下    時間: 2025-3-28 02:26
https://doi.org/10.1007/978-3-030-86622-8al modelling was carried out using several seismic inputs with Arias intensity (AI) values ranging from 1 and 0.01?m/s and characteristic periods, T., ranging from 0.3 to 16.5?s. Depending on the landslide dimensions (thickness and length), characteristic periods for thicknesses (T.) and lengths (T.
作者: antenna    時間: 2025-3-28 08:47
https://doi.org/10.1007/978-3-319-92501-1h assessment of possible landslide risk scenarios. This report describes the main results of the comprehensive studies, calculations and dynamic modeling of stability of the right-bank landslide-prone slope, which suggest that the potentially unstable mass of strongly weathered rocks with the volume
作者: Memorial    時間: 2025-3-28 10:41
https://doi.org/10.1057/9781137491626s in the parameter values and distribution plots to co-seismic landslides in other parts of world. These results provide valuable information about the slope response characteristics in case of seismic activation in thrust faulting Himalayan landscapes, and this is important in further researches on
作者: mechanical    時間: 2025-3-28 16:33

作者: curriculum    時間: 2025-3-28 19:22
Person-Affecting Principles and Beyond,of instabilities induced by these earthquakes were rock/soil falls, being other typologies of landslides very rare. In all cases, the size of instabilities triggered were small, usually with volumes of 1?m. or less, reaching the larger volumes up to 500–1000?m.. Data available from these events poin
作者: collagen    時間: 2025-3-28 23:27
https://doi.org/10.1007/978-94-007-2765-6were registered) are widespread enough to be used for intensity assessment, together with the total size of affected area, which is around 180?km.. Rockfalls were classified into five categories according to their volume. The volumes of the two largest rockfalls were quantitatively assessed by compa
作者: cardiopulmonary    時間: 2025-3-29 06:54

作者: 正論    時間: 2025-3-29 10:40
Mathematical Problems Posed by the Theory,highest predictive power in terms of landslide occurrence. In these regions, with the exception of one, the models are significantly better than a null model, and the models are good in predicting weather-induced landslide occurrence. The highest predictive probability of weather-induced landslide o
作者: Gullible    時間: 2025-3-29 14:35
International Consortium on Landslides and President of the Slovenian NationalPlatform for Disaster Risk Reduction..Prof. Nicola Casagli is Founding member of the International Consortium on Landslides(ICL), professor at the University of Florence and founder of the UNESCO Chair on geohydrological haz978-3-030-10415-3978-3-319-53485-5
作者: PRE    時間: 2025-3-29 17:26

作者: semble    時間: 2025-3-29 20:52
Finite Element Simulation for Seismic Ground Response in Mountainous Areas in Nepalfacts in local areas, it can be concluded that the proposed numerical method has a sufficient ability to predict the phenomena and can be possibly utilized for predicting overall distribution of earthquake-induced landslide which would be helpful for developing landslide susceptibility maps in mountainous areas in Nepal.
作者: Infantry    時間: 2025-3-30 01:16
Evaluation of Ground Shaking Characteristics in Residential Land Based on T/R Frequency Ratio of Micstics focused on not only peak frequency (Ridge frequency) but also Trough frequency were evaluated. As a result, the T/R frequency ratio of microtremor is one of effective indices to evaluate the ground shaking characteristics in a residential land.
作者: 思想    時間: 2025-3-30 04:11

作者: 全等    時間: 2025-3-30 08:24
CoCo Bonds and Bail-in Mechanism,facts in local areas, it can be concluded that the proposed numerical method has a sufficient ability to predict the phenomena and can be possibly utilized for predicting overall distribution of earthquake-induced landslide which would be helpful for developing landslide susceptibility maps in mountainous areas in Nepal.
作者: Petechiae    時間: 2025-3-30 14:15

作者: 厭煩    時間: 2025-3-30 17:29
https://doi.org/10.1007/978-3-319-67378-3stics focused on not only peak frequency (Ridge frequency) but also Trough frequency were evaluated. As a result, the T/R frequency ratio of microtremor is one of effective indices to evaluate the ground shaking characteristics in a residential land.
作者: PARA    時間: 2025-3-30 22:13

作者: 要素    時間: 2025-3-31 01:49

作者: Ferritin    時間: 2025-3-31 08:13

作者: PAC    時間: 2025-3-31 09:33

作者: Ingest    時間: 2025-3-31 14:42

作者: Antimicrobial    時間: 2025-3-31 19:16

作者: 煩人    時間: 2025-3-31 23:01
Local Terrain Relief: An Important Factor Influencing the Generation of Large Earthquake-Triggered Lse more serious damages. The study of the factors controlling large earthquake-induced landslides by the 2008 Ms8.0 Wenchuan Earthquake demonstrated that this kind of large and deep slope failures could be specifically tied to some particular geologic settings after analyzing their distribution char
作者: 軟弱    時間: 2025-4-1 04:30

作者: Cerebrovascular    時間: 2025-4-1 09:42
Critical Displacement of Earthquake-Triggered Catastrophic Landslidesg Newmark displacement analysis. The critical displacement, usually obtained from laboratory shear tests under low and constant shear rates, is defined as the coseismic displacement beyond which strength of sliding surface reach residual values. The typical value ranges a few centimeters, depending




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