標(biāo)題: Titlebook: Earthquake Hazard and Risk; Vladimír Schenk Book 1996 Kluwer Academic Publishers 1996 Geoinformationssysteme.aftershock.earthquake.microse [打印本頁(yè)] 作者: angiotensin-I 時(shí)間: 2025-3-21 17:13
書(shū)目名稱(chēng)Earthquake Hazard and Risk影響因子(影響力)
書(shū)目名稱(chēng)Earthquake Hazard and Risk影響因子(影響力)學(xué)科排名
書(shū)目名稱(chēng)Earthquake Hazard and Risk網(wǎng)絡(luò)公開(kāi)度
書(shū)目名稱(chēng)Earthquake Hazard and Risk網(wǎng)絡(luò)公開(kāi)度學(xué)科排名
書(shū)目名稱(chēng)Earthquake Hazard and Risk被引頻次
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書(shū)目名稱(chēng)Earthquake Hazard and Risk年度引用學(xué)科排名
書(shū)目名稱(chēng)Earthquake Hazard and Risk讀者反饋
書(shū)目名稱(chēng)Earthquake Hazard and Risk讀者反饋學(xué)科排名
作者: 商業(yè)上 時(shí)間: 2025-3-21 23:59
The Probability of the Time Occurrence of Strong Earthquake for Some Zones in Albaniaones and lines of Albania, in this paper we have made use of property that the time interval sequence of earthquakes follows the logarithmic normal distribution, as proved by the test of normality..Eventually, for the different seismic regions we obtained the different time interval that the next st作者: 廚師 時(shí)間: 2025-3-22 03:01
Statistical Estimation of the Maximum Magnitude and its Uncertainty from a Catalogue Including Magniually there are errors in earthquake magnitudes of modern and historic events. Taking into account the standard deviations of errors in earthquake magnitudes results in modified distribution of observed magnitudes. The new magnitude distribution slightly differs from the Gutenberg-Richter’s one for 作者: Adulterate 時(shí)間: 2025-3-22 05:23
Estimation of Upper Bound Magnitude in Earthquake Hazard Assessment in Sloveniaified causative faults. The analysis of the earthquake catalogue of Slovenia and surrounding areas showed that for the region of Slovenia a doubly truncated exponential frequency-magnitude relationship may serve directly for this purpose, taking into account the following assumptions:.(1) The value 作者: APO 時(shí)間: 2025-3-22 11:00 作者: 滑動(dòng) 時(shí)間: 2025-3-22 14:01
Changes of the State of Stress and Deformation in Epicentral Zones During the Aftershock Periodes and a prediction of strong aftershocks. The high precision geodetic, magnetometric and gravimetric repeated measurements after a main shock have been carried out in the epicentral zones of earthquakes with M≥7..During a gradual descent of seismic activity, the trend and oscillatoring changes of g作者: 滑動(dòng) 時(shí)間: 2025-3-22 20:32 作者: maverick 時(shí)間: 2025-3-22 22:36
Preliminary Seismic Hazard Assessment for the Italian Seismic Coderesented. They have been obtained by applying two methodologies (the Cornell approach and the mixed method), and refer to two stages of elaboration: after having summarised the products performed during a previous national project, and after the first release of the products developed ad hoc for the作者: 小歌劇 時(shí)間: 2025-3-23 02:21
Earthquake Hazard Assessment for the Czech Republic and Adjacent Areaoth a review of the calculations obtained and an outlook of possible new methodological aspects in earthquake hazard calculations are summarized. The hazard calculations have been made mainly for the region of 48.5°-51.2°N, 12°-19°E, which belongs to an area of relatively low seismicity, and which i作者: Bricklayer 時(shí)間: 2025-3-23 09:15 作者: GLARE 時(shí)間: 2025-3-23 11:08
Recent Trends in Regional and Global Seismic Hazard Assessment cooperation of seismologists, geologists and engineers. Here we review problems and limitations in the practice of seismic hazard assessment, the use of different probabilistic approaches in different tectonic areas and the implementation and significance of geological input in seismic hazard asses作者: lavish 時(shí)間: 2025-3-23 17:06 作者: pellagra 時(shí)間: 2025-3-23 18:28
Expert System for Earthquake Hazard Assessment: ESEHAman and man-made structures. It has been put into practice by implementation of artificial intelligence techniques and expert systems. In this paper, first the significance and methodology for developing for the Expert System for Earthquake Hazard Assessment abbreviated ESEHA is described; secondly,作者: ARENA 時(shí)間: 2025-3-24 00:33
Estimating Losses from Future Earthquakes in China relief work are based. The loss caused by earthquakes is determined by the following two factors: a) The temporal and spatial distribution of seismic activities which is dealt with by the seismic hazard analysis and b) The degree of damage done by earthquakes on the society, economy and people is t作者: BARK 時(shí)間: 2025-3-24 03:45
Earthquake Risk Assessment in Greecen each region, i, has been determined as a convolution of earthquake hazard, buildings oldness coefficient, average population density and regional Gross Domestic Product per capita. A relative risk scale was adopted by assinging each region with R. = R./min R.. The final product is a map of large-s作者: ENDOW 時(shí)間: 2025-3-24 09:27
The Optical Disk “Spitak Earthquake of 1988” natural environment, the performance of man-made structures, and the earthquake itself. Recent advances in digital data storage have made it possible to collect these data onto a single compact disk, greatly simplifying the process of data access and distribution. The authors have endeavored to col作者: 尖牙 時(shí)間: 2025-3-24 12:20 作者: 錯(cuò)事 時(shí)間: 2025-3-24 15:03 作者: rheumatism 時(shí)間: 2025-3-24 21:25 作者: 粘連 時(shí)間: 2025-3-25 01:03
1878-9897 Seismology and Physics of the Earth‘s Interior(Wellington, January 1994). .The papers, rigorously scrutinized by an international board ofreferees, cover some recent aspects of current research in earthquakehazard and seismic risk. They address the algorithms and methodologyused in seismological app作者: happiness 時(shí)間: 2025-3-25 06:55
A Just Society for Ireland? 1964-1987stribution, as proved by the test of normality..Eventually, for the different seismic regions we obtained the different time interval that the next strong earthquake might occur..The results may help the study of seismic zoning, microzoning, seismic risk and other problems.作者: JOT 時(shí)間: 2025-3-25 09:57
https://doi.org/10.1007/978-3-319-98092-8et, where a focal mechanism tensor is treated as a random object. The procedure of numerical simulation of random focal mechanism tensors is proposed. We also describe the process of numerical simulation of a set of random focal mechanism tensors corresponding to the given probability density function.作者: deciduous 時(shí)間: 2025-3-25 15:36
Critique: Between Theory and Method,fter having summarised the products performed during a previous national project, and after the first release of the products developed ad hoc for the present GNDT project. Maps of horizontal and vertical PGA referring to 100 and 500 year return periods and maps of exceedance probability for intensity VII MCS in 50 years are shown and commented.作者: POWER 時(shí)間: 2025-3-25 19:29
https://doi.org/10.1007/978-3-031-50539-3first the significance and methodology for developing for the Expert System for Earthquake Hazard Assessment abbreviated ESEHA is described; secondly, its content composition, logical structure, knowledge-base, major algorithms, case study and its results are introduced; finally some conclusion and discussion are given.作者: 顛簸下上 時(shí)間: 2025-3-25 20:18 作者: 生命 時(shí)間: 2025-3-26 01:23 作者: 螢火蟲(chóng) 時(shí)間: 2025-3-26 08:18
Reading the Ancient World with Chicano Eyes,arried out in the framework of GNDT (National protection Against Earthquake of the National Council of Research).data base of observed intensities compiled by the same research group..Significant differences were found which, in particular, show the importance of observed site intensities for a reliable hazard assessment.作者: 詩(shī)集 時(shí)間: 2025-3-26 09:07 作者: arrogant 時(shí)間: 2025-3-26 16:18 作者: Breach 時(shí)間: 2025-3-26 19:22 作者: 赤字 時(shí)間: 2025-3-27 00:43 作者: Genistein 時(shí)間: 2025-3-27 04:27
Expert System for Earthquake Hazard Assessment: ESEHAfirst the significance and methodology for developing for the Expert System for Earthquake Hazard Assessment abbreviated ESEHA is described; secondly, its content composition, logical structure, knowledge-base, major algorithms, case study and its results are introduced; finally some conclusion and discussion are given.作者: 花爭(zhēng)吵 時(shí)間: 2025-3-27 06:51
Earthquake Risk Assessment in Greeceoss Domestic Product per capita. A relative risk scale was adopted by assinging each region with R. = R./min R.. The final product is a map of large-scale, relative earthquake risk distribution in Greece, which allows the elaboration of strategic plans for the risk mitigation.作者: 大氣層 時(shí)間: 2025-3-27 11:37
https://doi.org/10.1007/978-1-349-00178-1l variations of fractal dimensions in spatial distribution of events was investigated..The resulting criteria for evaluation of “completion of development” of earthquake epicentral fields in BRZ may be used in estimations of average long-term parameters of seismic regime of the territory.作者: 劇毒 時(shí)間: 2025-3-27 14:42
Guiding Principles, Hard Cases,sment. We also present a survey of global and regional cooperative programs in multinational and multidisciplinary seismic hazard assessment and we review the status and plan of the UN/IDNDR Global Seismic Hazard Assessment Program.作者: 導(dǎo)師 時(shí)間: 2025-3-27 18:29 作者: 葡萄糖 時(shí)間: 2025-3-28 00:22 作者: 單調(diào)性 時(shí)間: 2025-3-28 05:00
Statistical Estimation of the Maximum Magnitude and its Uncertainty from a Catalogue Including Magnimaximum of observed values. On the example of artificially generated catalogues the behaviour of the estimates for the different sample sizes and different levels of the magnitude errors is analysed. It is shown that the uncertainty in the M. is usually much higher then the errors in initial magnitu作者: enchant 時(shí)間: 2025-3-28 07:49
Estimation of Upper Bound Magnitude in Earthquake Hazard Assessment in Sloveniasmic sources in the same area with the incremental technique..There is an indication that such least-squares estimates are similar to or a bit greater than Kijko and Sellevol’s maximum likelihood estimates (1989). Both might be used with reasonable weights as alternatives for upper bound magnitudes 作者: rheumatism 時(shí)間: 2025-3-28 11:31
Changes of the State of Stress and Deformation in Epicentral Zones During the Aftershock Periodn at two stages of post-seismic activity: an intensive fissuring, leading to formation of blocks on a different scale (from metres to kilometres), and a consolidation of aftershock zone by smoothing of tectonic stress gradients at the block boundaries.作者: Systemic 時(shí)間: 2025-3-28 17:39 作者: 持續(xù) 時(shí)間: 2025-3-28 22:08
Importance of Geological Data in Probalistic Seismic Hazard Assessments: A Case Study from ETNE, Wesments through an example from Etne in western Norway..Detailed lineament studies conducted on satellite images, have revealed possible active fault zones in the Sunnhordland District, including the Etne Fault Zone (EFZ). The parallelism between a recently discovered NW-SE trending regional aeromagne作者: 合群 時(shí)間: 2025-3-29 00:23 作者: 地名表 時(shí)間: 2025-3-29 05:35
1878-9897 nterested in earthquake hazard andseismic risk research as well as a more general audience ofseismologists, geophysicists and Earth scientists. It is also usefu978-94-010-6592-4978-94-009-0243-5Series ISSN 1878-9897 Series E-ISSN 2213-6959 作者: Allowance 時(shí)間: 2025-3-29 09:54
https://doi.org/10.1057/9780230618558nergy was released at the beginning of the sequence, with the highest magnitude M. = 3.6. Most events were felt by the population, but they caused no damage..Fault plane solutions calculated for a selected number of events show that most of the mechanisms have T axes oriented in an anti-apenninic di作者: condemn 時(shí)間: 2025-3-29 13:33 作者: 進(jìn)步 時(shí)間: 2025-3-29 17:31 作者: FAWN 時(shí)間: 2025-3-29 21:19
David Nightingale,Christopher Spencern at two stages of post-seismic activity: an intensive fissuring, leading to formation of blocks on a different scale (from metres to kilometres), and a consolidation of aftershock zone by smoothing of tectonic stress gradients at the block boundaries.作者: HAIRY 時(shí)間: 2025-3-30 02:25
Susanne MacGregor,Betsy Ettorre, classification of dependent and independent events, normalization of the earthquake regime per period of observation and/or the size of the area under study, and application of different attenuation laws, effects of near-surface sedimentary deposits) upon the final hazard values have been taken in作者: Perceive 時(shí)間: 2025-3-30 06:44 作者: conceal 時(shí)間: 2025-3-30 10:23 作者: ungainly 時(shí)間: 2025-3-30 15:02
Book 1996a-plate tectonic settings. Of particularinterest is hazard assessment in regions of rare large earthquakes..The book is suitable for those interested in earthquake hazard andseismic risk research as well as a more general audience ofseismologists, geophysicists and Earth scientists. It is also usefu作者: 談判 時(shí)間: 2025-3-30 18:17
https://doi.org/10.1007/978-94-009-0243-5Geoinformationssysteme; aftershock; earthquake; microseism; seismic; seismology; hydrogeology
