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| 1 | A Hazard Assessment Method for Potential Earthquake-Induced Landslides – A Case Study in Huaxian County, Shaanxi Province显示文摘The hazard assessment of potential earthquake-induced landslides is an important aspect of the study of earthquake-induced landslides. In this study, we assessed the hazard of potential earthquake-induced landslides in Huaxian County with a new hazard assessment method. This method is based on probabilistic seismic hazard analysis and the Newmark cumulative displacement assessment model. The model considers a comprehensive suite of information, including the seismic activities and engineering geological conditions in the study area, and simulates the uncertainty of the intensity parameters of the engineering geological rock groups using the Monte Carlo method. Unlike previous assessment studies on ground motions with a given exceedance probability level, the hazard of earthquake-induced landslides obtained by the method presented in this study allows for the possibility of earthquake-induced landslides in different parts of the study area in the future. The assessment of the hazard of earthquake-induced landslides in this study showed good agreement with the historical distribution of earthquake-induced landslides. This indicates that the assessment properly reflects the macroscopic rules for the development of earthquake-induced landslides in the study area, and can provide a reference framework for the management of the risk of earthquakeinduced landslides and land planning. | LIU Jiamei GAO Mengtan WU Shuren WANG Tao WU Jian | 2016 | Acta Geologica Sinica(English Edition)2016，90，2： | 8 |
| 2 | Discussion on the influence of truncation of ground motion residual distribution on probabilistic seismic hazard assessment显示文摘Recent studies on assessment of a very low annual probability of exceeding (APE) ground motions, 10-4 or less, have highlighted the importance of the upper bound of ground motions when very low probability results are acquired. The truncation level adopted in probabilistic seismic hazard analysis (PSHA) should be determined by an aleatory uncertainty model (i.e., distribution model) of ground motions and the possible maximum and minimum ground motion values of a specific earthquake. However, at the present time, it is impossible to establish the upper bound model for ground motions based on the source characteristics and/or ground motion propagation. McGuire suggested a truncation level be fixed at a number of = 6, or the distribution of residuals be truncated in such a manner that site intensity cannot be greater than the epicenter intensity. This study aims to find a reasonable and feasible truncation level to be used in PSHA when the physical mechanism is not available to find the extreme ground motion. A mathematical analysis of the influence of the truncation level on PSHA, case studies of sites in different seismotectonic settings, and a distribution analysis of ground motion residuals are conducted in this study. It is concluded that = 4 is the minimum acceptable value for engineering applications for APEs within 0.002 to 10-4, and for low APEs, such as 10-5 and 10-6, the value of should be no less than 5 in most regions of China. | Wu Jian Gao Mengtan Chen Kun Huang Bei | 2011 | Earthquake Engineering and Engineering Vibration2011，10，3： | 3 |
| 3 | Standardization of probability of earthquakes in seismic fortification 显示文摘 | Yan Jiaquan Chen Jiageng Gao Mengtan | 2000 | Recent Developments in World Seismology2000，，9： | 1 |
| 4 | Magnetic constraints on the spatial distribution of seismic activity显示文摘The lithospheric magnetic field(LMF) in China and its surrounding are calculated using the spherical harmonic coefficients given by the NGDC-720 model. The LMF comes from the magnetization of minerals in the crust and in the uppermost mantle. It may, therefore, provide unique insight into lithospheric tectonic processes and mechanisms. Here, we study the geomagnetic manifestation of active tectonic blocks, and find a close correlation between the LMF and seismicity. Many large faults are found to closely overlap with magnetic anomalies, or are distributed along the boundaries of magnetic anomalies.Earthquakes in these fault regions have occurred on the boundaries of magnetic anomalies, or in the transition zones between positive and negative anomalies. We analyze the components of the LMF, and the LMFs at different altitudes, finding that the vertical component, Bzat200 km, is the most related to seismic activity. Relevant physical mechanisms are also discussed. We propose that the stress or viscosity differences caused by temperature variations, which manifest in the LMF, may be the predominant reason for the correlation between the LMF and seismic activity along large faults. | Liguo Jiao Huaran Chen Mengtan Gao | 2013 | Earthquake Science2013，26，2： | 1 |
| 5 | Research on the ShakeMap System with Consideration of Site Effects显示文摘In accordance with the principle of similarity in geology and topography,the V3S0(the average shear-velocity down to a 30m depth below the surface) approximation of sites is acquired by correlation between V3S0 and slopes after calculating the maximum slope of topography using the 30-sec Chinese Mainland DEM(Digital Elevation Model) data set.Site-amplification factors are then quantified with V3S0 and applied to the ShakeMap system developed by this study to revise ground-motion amplitudes on bedrock estimated from empirical relationships.Finally,the distribution of ground motion parameters on the surface is obtained.This article also introduces the calculation process,calculation models of the ShakeMap systems and related software systems.In conclusion,certain examples indicate that the ShakeMap system is feasible in the Chinese Mainland. | Chen Kun Yu Yanxian Gao Mengtan | 2010 | Earthquake Research in China2010，24，2： | 1 |
| 6 | Preliminary Study on Probabilistic Prediction of Seismic Hazard in a Period of 10 Years显示文摘Many uncertainty factors need be dealt with in the prediction of seismic hazard for a 10-year period.Restricted by these uncertainties,the result of prediction is also uncertain to a certain extent,so the probabilistic analysis method of seismic hazard should be adopted.In consideration of the inhomogeneity of the time,location,and magnitude of future earthquakes and the probabilistic combination of the background of long-term seismic hazard(geology,geophysical field,etc.)and the precursors of earthquake occurrence,a model of probabilistic prediction of seismic hazard in a period of 10 years s proposed.Considering the inhomogeneity of data and earthquake precursors for different regions in China,a simplified model is also proposed in order to satisfy the needs of different regions around the country.A trial in North China is used to discuss the application of the model.The method proposed in this paper can be used in the probabilistic prediction of seismic hazard in a period of 10 years.According to | Gao Mengtan and Wang JianInstitute of Geophysics,SSB,Beijing 100081,China | 1995 | Earthquake Research in China1995，9，4： | 1 |
| 7 | Seismic Damage Characteristics of the Wenchuan Great Earthquake on May 12,2008 and Suggestions for Disaster Prevention显示文摘The paper introduces the tectonic background,focal mechanism and distribution of aftershock of the Wenchuan earthquake on May 12,2008. The earthquake is considered to be the result of long-term interaction between the eastward movement of the Bayan Har Block and the Sichuan Basin. Most of the earthquake energy was released in an area (the seismic source body) 330km long,52km wide and 20km deep over 100s. Energy release in the source body was extremely uneven,and strong ground motion in the epicenter area shows obvious asymmetrical character in the time and space scale. The high-intensity area is distributed along the source body,and the intensity distribution bears an obvious anomalous characteristic. The investigation results indicate that more than 90 percent of casualties caused by this earthquake were in the areas of intensity IX or above. Houses,schools and hospitals etc. suffered serious damage. Lifelines such as transportation,water conservation etc. also suffered significant damage. Besides,earthquake-triggered avalanches,landslides,mud-rock flows and so on were extremely serious. The tremendous earthquake disaster highlighted the deficiencies in disaster prevention and mitigation management,scientific earthquake research,technology and application of earthquake disaster prevention,and publicity of earthquake preparedness and disaster reduction. | Gao Mengtan Zhou Bengang Pan Hua | 2009 | Earthquake Research in China2009，23，4： | 1 |
| 8 | A discussion on the mean annual rate of large earthquakes 显示文摘 | Gao Mengtan | 1988 | Recent Development in World Seismology1988，，1： | 1 |
| 9 | The application of extreme value theory in engineering seismology 显示文摘 | Gao Mengtan Iia Sujuan | 1988 | Acta Seismologica Sinica1988，10，3： | 1 |
| 10 | Seismic Hazard Analysis of China's Mainland Based on a New Seismicity Model显示文摘Based on the seismic source model in the Fifth Generation Seismic Ground Motion Parameters Zonation Map of China(FGSGMPZMC),a new seismic fault model,the new zonation of seismic risk areas(SRAs),and the estimation of seismicity rates for 2021-2030,this study constructed a new time-dependent seismic source model of China’s mainland,and used the probabilistic seismic hazard analysis method to calculate seismic hazard by selecting the ground motion models(GMMs)suitable for seismic sources in China.It also provided the probabilities of China’s mainland being affected by earthquakes of modified Mercalli intensity(MMI)Ⅵ,Ⅶ,Ⅷ,Ⅸ,and≥Ⅹin 2021-2030.The spatial pattern of seismic hazards presented in this article is similar to the pattern of the FGSGMPZMC,but shows more details.The seismic hazards in this study are higher than those in the FGSGMPZMC in the SRAs and fault zones that can produce large earthquakes.This indicates that the seismic source model construction in this study is scientific and reasonable.There are certain similarities between the results in this study and those of Rong et al.(2020)and Feng et al.(2020),but also disparities for specific sites due to differences in seismic source models,seismicity parameters,and GMMs.The results of seismic hazard may serve as parameter input for future seismic risk assessments.The hazard results can also be used as a basis for the formulation of earthquake prevention and mitigation policies for China’s mainland. | Weijin Xu Jian Wu Mengtan Gao | 2023 | International Journal of Disaster Risk Science2023，14，2： | 0 |
| 11 | Preliminary Analysis of Non-tidal Variation in the Baijiatuan Gravity Station,Beijing and the Relevance of Gravity Changes and Water Storage显示文摘The non-tidal variation gained from continuous gravity observations in stations usually reflects the regional continuous gravity changes. In this paper we focus on studying the non-tidal variation of Baijiatuan station,Beijing where there are two different gravimeters( namely,L&R-804 and PET-031). Based on the original raw tidal records of two gravimeters from 2008 to 2011,we first remove various interference from raw data by the standard procedure software-Tsoft; then we model the solid earth tides, ocean tidal loading and pole tide through related parameters; after that we adopt a new segmented polynomial fitting method based on Tsoft to fit the complex drift of spring gravimeter; and finally we calculate the atmospheric loading effects by a linear regression model. After a series of processing we gain the non-tidal variation of the two gravimeters at Baijiatuan site,Beijing. Furthermore,to analyze the non-tidal variation preliminarily,we study the main component of related tidal data by power spectral density. Comparing the non-tidal variation of two different gravimeters,we find seasonal fluctuations in non-tidal results, which are in accordance with the water storage change. Therefore,we take into account the relevance of gravity changes and water storage based on the gravity data of GRACE and water data of the CMAP model from 2003 to 2011 at different sites in the Chinese mainland( Beijing, Chengdu, Shenyang and Shiquanhe), and make a preliminary analysis on the relationship between gravity changes and water storage. | Xu Weimin Chen Shi Gao Mengtan Shi Lei Lu Hongyan | 2014 | Earthquake Research in China2014，28，1： | 0 |
| 12 | Study on the Relationship of Seismic Design Ground Motion at Different Fortification Levels in the Xinjiang Region显示文摘The seismic risk analysis results of 79 cities in Xinjiang are presented, and the bedrock peak ground accelerations under three seismic levels and their ratios are discussed. Then, the relationship between earthquake environments and the seismic risk analysis results of different exceeding probabilities are researched. The results show that minor and major earthquake motion parameters calculated from moderate earthquakes do not have a consistent probability and the ratio of bedrock peak accelerations under different exceedance probabilities are closely correlated with earthquake environments. | Tang Lihua Gao Mengtan and Jiang Hui | 2007 | Earthquake Research in China2007，21，4： | 0 |
| 13 | Seismic Zonation of Central-Southern Hunan Province, China显示文摘Based on basic data used in compiling the Zonation Map of Earthquake Ground Motion Parameters in China, recent research on seismic safety assessment for engineering sites in central-southern Hunan Province, the new attenuation relationships of moderate earthquakes and the background seismicity data obtained by modern instrumental earthquake records since 1970, a new result of seismic zonation of central-southern Hunan Province is provided. The result shows that the area with PGA=0.05g has obviously increased in the new map compared with the previous one and is relatively consistent with the seismic disaster characteristics of moderate earthquakes that took place in the central-southern part of Hunan in recent years. This result will benefit the research and compilation of a new-generation seismic zonation map of earthquake ground motion parameters and the seismic hazard assessment in the moderate earthquake active regions in the central and eastern part of China. | Li Ying Xu Guangyin Chen Kun Gao Mengtan | 2007 | Earthquake Research in China2007，21，4： | 0 |
| 14 | Review and Prospects of the Global Earthquake Model Project ( GEM)显示文摘This paper reviewed the main target,functions,tool( Open Quake software) and research achievements of the Global Earthquake Model( GEM) Foundation,and made a simple prospect on the development and application of projects of GEM in the future. Learning from GEM and Open Quake is helpful to improve the seismic hazard model of China and enhance the scientificity of the seismic hazard assessment for metropolitans and major engineering facilities near major seismogenic structures. | Li Changlong Wu Jian Xu Weijin Gao Mengtan | 2017 | Earthquake Research in China2017，31，1： | 0 |
| 15 | The Role of the National Significant Seismic Monitoring and Protection Regions Institution:From the Perspective of the RiskSociety Theory显示文摘Earthquake disaster risk,as a typical social disaster risk,is one of the most important risks in modern Chinese society.This study gives definitions of the institution,describes the formation history,the connotations and development and analyzes its role in the control of major social risks caused by earthquakes.Finally,the paper presents recommendations for continuous improvement of this institution under the guidance of risk society theory,and for its application to the government reform and social governance. | Gao Mengtan Wu Guochun Wu Xinyan Lang Cong | 2015 | Earthquake Research in China2015，29，1： | 0 |
| 16 | Conclusions on the Implementation of Regulation of the National Significant Seismic Monitoring and Protection Regions from 1996 to 2012 in the Chinese Mainland显示文摘The regulation of the National Significant Seismic Monitoring and Protection Regions(NSSMPR for short) is defined by the Law of the Peoples Republic of China on Protecting Against and Mitigating Earthquake Disasters.The first stage of implementation of the regulation of NSSMPR in the Chinese mainland was finished from 1996 to 2005.The second stage is being carried on from 2006 to 2020.With the support of the National Social Science Foundation,this paper follows up and evaluates the implementation of the regulation of NSSMPR from 1996 to 2012 in the Chinese mainland.Based on analysis of earthquake examples and investigation data,we find that the effect of disaster mitigation is good,and on this basis,some suggestions are proposed to improve the regulation of NSSMPR. | Chao Hongtai Gao Mengtan Li Bo Chen Shijun Liang Kaili Ma Yuxiang Wang Feng Wu Guochun Lang Cong Wu Xinyan | 2015 | Earthquake Research in China2015，29，1： | 0 |
| 17 | Role of NGOs in the National Significant Seismic Monitoring and Protection Regions显示文摘In this paper,we analyzed the One Foundations relief and reconstruction activities after the Yaan earthquake.The analysis shows that the participation of NGOs in disaster relief activities has undergone different stages.In the Jiujiang earthquake,NGOs participation was in the rudimentary stage.In the Wenchuan earthquake,they became one of the active participants.In the Yaan earthquake,they played an active role through a cooperation mechanism.That means NGOs have had the capability of resource mobilization and cooperation with them will improve disaster management capacities,especially in the national significant seismic monitoring and protection regions. | Wu Guochun Gao Mengtan | 2015 | Earthquake Research in China2015，29，1： | 0 |
| 18 | Simulation of strong earthquake characteristics of a scenario earthquake(M_(S)7.5)based on the enlightenment of 2022 M_(S)6.9 earthquake in Menyuan显示文摘The Menyuan area is an important transportation hub in the Hexi Corridor.The Menyuan M_(S)6.9 earthquake that occurred on January 8,2022 had a major impact on the local infrastructure and transportation of this region.Due to the high possibility of similar strong earthquakes occurring in this area in the future,preliminary assessment of the seismic intensity characteristics of destructive earthquakes in this region is essential for effective disaster control.This paper uses the empirical Green′s function(EGF)method as a numerical simulation tool to predict the ground motion intensity of Datong Autonomous County under the action of the scenario earthquake(M_(S)7.5).Seismic records of aftershocks of the 2016 Menyuan M_(S)6.4 earthquake were used as Green’s functions for this simulation.The uncertainties associated with various source parameters were considered,and 36possible earthquake scenarios were simulated to obtain 72 sets of horizontal ground motions in Datong County.The obtained peak ground acceleration(PGA)vs.time histories of the horizontal ground motion were screened using the attenuation relationships provided by the fifth-edition of China’s Seismic Ground Motion Parameter Zoning Map and the NGA-West2dataset.Ultimately,32 possible acceleration-time histories were selected for further analysis.The screened PGA values ranged from 78.8 to 153 cm/s^(2).The uncertainty associated with the initial rupture point was found to greatly affect the results of the earthquake simulation.The average acceleration spectrum of the selected acceleration-time history exceeded the expected spectrum of a intermediate earthquake,which means that buildings in Datong County might sustain some damage should the scenario earthquake occur.This research can provide reliable ground motion input for urban earthquake damage simulation and seismic design in Datong County.Growing the dataset of small earthquakes recorded in this region will facilitate the large-scale simulation of ground motions under different earthquake scenarios. | Zhiwei Ji Zongchao Li Mengtan Gao Jize Sun Xiangyun Guo | 2022 | Earthquake Science2022，35，6： | 0 |
| 19 | Shaking Intensity Distribution of the April 14,2010 Yushu,China Earthquake显示文摘Two hours after the 2010 Yushu Earthquake, the shaking intensity distribution was obtained using the ShakeMap Rapid Generation System Based on Site Effects,developed by the author,which integrates the information of tectonic settings,the strike and scale of causative faults, focal mechanism solutions, fault rupture process and attenuation relationship in Western China,as well as local site effects. The results are as follows: ① The major axis of shaking intensity distribution is directed NW-SE,parallel to the Yushu fault; ② The meizoseismal area reaches an intensity Ⅸ and covers 300km2; ③ The intensity Ⅸ area is mainly distributed in the area 40km southeast and 15km northwest of the epicenter along the causative fault; ④ Due to local soil conditions,the northwestern part of the area with intensity Ⅸ on bedrock shows an intensity Ⅷ when converting from the bedrock to the soil; ⑤ Areas with intensity Ⅷ,Ⅶ,Ⅵ measure 3,000km2,8,000km2,and 24,000km2, respectively. | Chen Kun Yu Yanxiang Gao Mengtan | 2010 | Earthquake Research in China2010，24，3： | 0 |
| 20 | Discussion on the Relationship between “Anti-great Earthquakes” and Ground Motion with a Low Probability of Exceedance显示文摘In this paper we discuss the differences and relationship between'great earthquakes',rare ground motion,and very rare ground motion.Taking the Beichuan-Yingxiu potential seismic source zone in Longmenshan seismic belt as an example,we revealed the relationship between the effects of'great earthquakes'and rare ground and very rare ground motion.After pointing out scientific and technical problems in the current seismic fortification system,we suggest that very rare ground motion should be considered if we want to deduce the potential hazard of great earthquakes in the future. | Chen Kun Gao Mengtan Li Wansheng | 2013 | Earthquake Research in China2013，27，4： | 0 |
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