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Artykuły w czasopismach na temat „Earthquake”

Autor: Grafiati

Data publikacji: 4 czerwca 2021

Data aktualizacji: 25 lipca 2025

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1

Isik, Ercan, Coskun Sagir, Zuhal Tozlu, and Umit Salim Ustaoglu. "Determination of Urban Earthquake Risk for Kırşehir, Turkey." Earth Sciences Research Journal 23, no. 3 (2019): 237–47. http://dx.doi.org/10.15446/esrj.v23n3.60255.

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Predicting the outcomes of earthquakes before they occur is one of the fundamental components of modern disaster management. Loss estimation analyses have an important place at the assessment stage of earthquakes and in estimation of losses that earthquakes may lead to. With these analyses, it is possible to access information that is relevant to potential damages and losses. In this paper, loss estimation analyses were carried out by using the earthquake scenario which foresaw a previous earthquake that was experienced in an around Kırşehir which is seismically active and located in the Centr

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Hidayawan, Ahmad, Andri Kurniawan, Bagas Wahyu Adhi, Beni Setiyanto, and Hayu Rahayu. "Analisis Penentuan Parameter Gempa Untuk Perhitungan Stabilitas Bendungan." MoDuluS Media Komunikasi Dunia Ilmu Sipil 6, no. 1 (2024): 1–7. https://doi.org/10.32585/modulus.v6i1.5529.

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Dams have an important role in controlling floods and providing water supply for infrastructure and community needs. The construction of the Pidekso Dam, as part of government efforts, requires research to determine earthquake parameters to ensure the safety of its structure. Pidekso Dam, located in the downstream Bengawan Solo river, is prone to earthquakes because it is adjacent to areas where earthquakes often occur. This study aims to determine the parameters of the earthquake coefficient Operating Basis Earthquakeee (OBE) and MaximumaDesignaEarthquakee (MDE) based on the 2017 earthquake m

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Dai, Xiaofeng, Xin Liu, Rui Liu, et al. "Coseismic Slip Distribution and Coulomb Stress Change of the 2023 MW 7.8 Pazarcik and MW 7.5 Elbistan Earthquakes in Turkey." Remote Sensing 16, no. 2 (2024): 240. http://dx.doi.org/10.3390/rs16020240.

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On 6 February 2023, the MW 7.8 Pazarcik and the MW 7.5 Elbistan earthquakes occurred in southeastern Turkey, close to the Syrian border, causing many deaths and a great deal of property destruction. The Pazarcik earthquake mainly damaged the East Anatolian Fault Zone (EAFZ). The Elbistan earthquake mainly damaged the Cardak fault (CF) and the Doğanşehir fault (DF). In this study, Sentinel-1A ascending (ASC) and descending (DES) orbit image data and pixel offset tracking (POT) were used to derive surface deformation fields in the range and azimuth directions induced by the Pazarcik and Elbistan

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Kertanah, Alissa Chintyana, Chandrawati, Basirun, Mutia Rosiana Nita Putri, and Nasibatul Mahmudah. "A Study of Grouping of Earthquake Damage from Magnitude Scale in Lombok Using K-Means Modeling." Kappa Journal 8, no. 3 (2024): 399–403. https://doi.org/10.29408/kpj.v8i3.27563.

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This study aims to group earthquake damage from its magnitude scale and visualize it on a geographical map. The magnitude of the earthquake was grouped using the K-means model. It is one of the most popular and effective clustering models in grouping data, such as earthquake data. The dataset used in this study is earthquake data for the last ten years on Lombok Island. The optimal number of clusters was used which is 2 in this case, based on the highest Silhouette score of 0.930. The highest Silhouette score shows the optimal number of clusters. The cluster on the geographical map shows most

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5

Cui, Yueju, Jianan Huang, Zhaojun Zeng, and Zhenyu Zou. "CO Emissions Associated with Three Major Earthquakes Occurring in Diverse Tectonic Environments." Remote Sensing 16, no. 3 (2024): 480. http://dx.doi.org/10.3390/rs16030480.

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Significant amounts of gases are emitted from the earth’s crust into the atmosphere before, during, and after major earthquakes. To understand the relationship between gas emissions, earthquakes, and tectonics, we conducted a thorough investigation using satellite data from AQUA AIRS. We focused on three major earthquakes: the 12 May 2008 Wenchuan MW 7.9 earthquake in China’s intra-continental plate, the 26 December 2004 Sumatra-Andaman MW 9.1 earthquake in Indonesia Island, and the 4 April 2010 Baja California MW 7.2 earthquake in Mexico’s active plate margin. Anomalies in the total column (T

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6

Nanjo, Kazuyoshi Z. "Predicting the unpredictable." Impact 2020, no. 6 (2020): 35–37. http://dx.doi.org/10.21820/23987073.2020.6.35.

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Better understanding of hazardous natural phenomena means improved preparedness and the opportunity to mitigate the damaging impact of these natural hazards. For example, improving knowledge about earthquakes can enable safer buildings to be built, as well as disaster prevention measures to be implemented, ultimately saving lives. This is particularly important in a country like Japan, which is earthquake-prone and where earthquakes prove to be very unpredictable. A team of Japanese researchers is seeking to reduce uncertainty in earthquake hazards by conducting statistical analyses of seismic

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Dhea Fitria, Syafriani Syafriani, Hamdi Hamdi, and Letmi Dwiridal. "Earthquake Decay Analysis to Determine the Afters Thock end Time in West Sumatra in 2021-2023 Using The Omori-Utsu Method." Uranus : Jurnal Ilmiah Teknik Elektro, Sains dan Informatika 3, no. 2 (2025): 55–64. https://doi.org/10.61132/uranus.v3i2.780.

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West Sumatra, situated at the convergence of the Indo-Australian and Eurasian tectonic plates, experiences frequent earthquakes and aftershocks due to the complex geological setting. This study utilizes the Omori-Utsu method, a modified version of Omori’s law by seismologist Tokiji Utsu, to estimate aftershock duration. Data on aftershocks from significant earthquakes (magnitude ≥5.5M) between 2021 and 2023 were accessed through the BMKG earthquake catalog. The study finds that aftershock durations vary significantly depending on the earthquake's tectonic origin. The longest recorded aftershoc

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Tiwari, Ram Krishna, and Harihar Paudyal. "Spatial mapping of b-value and fractal dimension prior to November 8, 2022 Doti Earthquake, Nepal." PLOS ONE 18, no. 8 (2023): e0289673. http://dx.doi.org/10.1371/journal.pone.0289673.

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An earthquake of magnitude 5.6 mb (6.6 ML) hit western Nepal (Doti region) in the wee hours of wednesday morning local time (2:12 AM, 2022.11.08) killing at least six people. Gutenberg-Richter b-value of earthquake distribution and correlation fractal dimension (D2) are estimated for 493 earthquakes with magnitude of completeness 3.6 prior to this earthquake. We consider earthquakes in western Nepal Himalaya and adjoining region (80.0–83.5°E and 27.3–30.5°N) for the period of 1964 to 2022 for the analysis. The b-value 0.68±0.03 implies a high stress zone and the spatial correlation dimension 1

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9

Hough, Susan E., and Stacey S. Martin. "Which Earthquake Accounts Matter?" Seismological Research Letters 92, no. 2A (2021): 1069–84. http://dx.doi.org/10.1785/0220200366.

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Abstract Earthquake observations contributed by human observers provide an invaluable source of information to investigate both historical and modern earthquakes. Commonly, the observers whose eyewitness accounts are available to scientists are a self-selected minority of those who experience a given earthquake. As such these may not be representative of the overall population that experienced shaking from the event. Eyewitness accounts can contribute to modern science only if they are recorded in the first place and archived in an accessible repository. In this study, we explore the extent to

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10

Lai, Junyan, Lu Ding, Yuan Zhang, et al. "Development of NERSS Training Program for Earthquake Emergency Response Capacity Building of Local Governments." Journal of Disaster Research 10, no. 2 (2015): 263–69. http://dx.doi.org/10.20965/jdr.2015.p0263.

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Responses to medium-magnitude earthquakes are as significant as to catastrophic earthquakes, because medium-magnitude temblors occur as many as a dozen times more than catastrophic earthquakes – at least from the year 1900. In China, local governments are obligated to protect residents against earthquakes that have a magnitude of <bm>Ms</bm>$6.0. The ways in which local governments perform these obligations differ, however, due to obstacles such as inadequate disaster planning, a lack of public earthquake awareness, and a shortage of qualified emergency managers. When an earthquake

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11

Purba, Siti M., Yaumil F. Alyssa, Mustika Nadia, Nadiatul Asra, and Umar Muksin. "The Influence of Seismometer Coverage on the Earthquake Focal Mechanism Solution (Case Study: Toba Swarm Earthquake)." IOP Conference Series: Earth and Environmental Science 1479, no. 1 (2025): 012014. https://doi.org/10.1088/1755-1315/1479/1/012014.

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Abstract The focal mechanism of an earthquake is necessary to describe the plane and characteristics of the fault. In the case of local earthquakes, the focal mechanism is often determined based on the first polarity of the primary wave. Therefore, the quality of the earthquake focal mechanism depends on the station coverage and the number of first polarities of primary waves. This study aims to investigate the variation in solution and quality of earthquake focal mechanisms with different station coverage. We conducted experiments on Toba swarm earthquake data for the May-June 2021 period wit

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12

Anderson, John G., Steven G. Wesnousky, and Mark W. Stirling. "Earthquake size as a function of fault slip rate." Bulletin of the Seismological Society of America 86, no. 3 (1996): 683–90. http://dx.doi.org/10.1785/bssa0860030683.

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Abstract Estimates of the potential size of earthquakes on mapped active faults are generally based on regressions of earthquake magnitude (Mw) versus length (L) of fault rupture for historical earthqukes. The fault slip rate (S) has been ignored in formal prediction equations, but more accurate predictions of future earthquake magnitudes on mapped faults may be obtained when it is included. A least-squares regression for a data set of 43 earthquakes occurring on faults for which slip rates are reported shows Mw = 5.12 + 1.16 log L − 0.20 log S, where L is in units of Km and S is in units of m

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13

Brimzhanova, S. S., А. А. Akhmadiya, N. Nabiyev, and Kh Moldamurat. "Determination of the earthquake epicenter using the maximum displacement method obtained by Sentinel-1A/B data via ESA SNAP software." Bulletin of the National Engineering Academy of the Republic of Kazakhstan 84, no. 2 (2022): 55–69. http://dx.doi.org/10.47533/2020.1606-146x.154.

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This article discusses a method for determining an earthquake’s epicenter using modern radar data from the Sentinel-1A/b remote sensing satellite. To determine the epicenter of the earthquake, finding the maximum displacement from the radar image data was used. The displacement (displacement) of the earth’s crust was obtained by processing on the ESA SNAP software. Two earthquakes that occurred in 2020 were studied to determine the epicenters in the ascending and descending orbits of the satellite. These earthquakes occurred in Western Xizang, China, and Doganyol, Turkey. The maximum deviation

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Li, Yujiang, Yongsheng Li, Xingping Hu, and Haoqing Liu. "Fault Geometry and Mechanism of the Mw 5.7 Nakchu Earthquake in Tibet Inferred from InSAR Observations and Stress Measurements." Remote Sensing 13, no. 24 (2021): 5142. http://dx.doi.org/10.3390/rs13245142.

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Different types of focal mechanism solutions for the 19 March 2021 Mw 5.7 Nakchu earthquake, Tibet, limit our understanding of this earthquake’s seismogenic mechanism and geodynamic process. In this study, the coseismic deformation field was determined and the geometric parameters of the seismogenic fault were inverted via Interferometric Synthetic Aperture Radar (InSAR) processing of Sentinel-1 data. The inversion results show that the focal mechanism solutions of the Nakchu earthquake are 237°/69°/−70° (strike/dip/rake), indicating that the seismogenic fault is a NEE-trending, NW-dipping fau

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Fan, Gang, Jun Wang, Shunchao Qi, Gongda Lu, Xingguo Yang, and Jiawen Zhou. "Spatiotemporal Evolution of Earthquakes in Longmenshan Fault and Adjacent Area, before and after the 2008 Wenchuan Earthquake." Shock and Vibration 2021 (November 24, 2021): 1–13. http://dx.doi.org/10.1155/2021/9400276.

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Seismicity sequence following a main earthquake usually contains much meaningful information for unveiling the focal mechanism and predicting the reoccurrence interval of large earthquakes. The spatiotemporal evolution of earthquakes before and after the 2008 Wenchuan earthquake (Ms 8.0) is analysed comprehensively in this study. The frequency-magnitude relation of the 3493 earthquake events retrieved from the database of the International Seismological Centre indicates that the adopted catalogue is complete for magnitudes ≥Ms 3.4. The seismicity during the 10 years before the Wenchuan earthqu

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Liu, Meiqin, Hiroyuki Mitsuhara, and Masami Shishibori. "A Mobile Application for Earthquake Education Targeting Foreigners Intending to Visit Japan." International Journal of Interactive Mobile Technologies (iJIM) 16, no. 24 (2022): 170–90. http://dx.doi.org/10.3991/ijim.v16i24.35479.

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Japan is in the Pacific Rim Seismic Belt, and earthquakes happen frequently. Foreigners who lack the necessary earthquake knowledge and escape skills may not survive strong earthquakes in Japan. Therefore, it is essential to provide earthquake education to these foreigners. Since rich-formed earthquake education has been available for foreigners living in Japan, this research works to improve the earthquake education situation for foreigners who intend to visit Japan. Receiving earthquake education in advance helps enhance foreigners’ earthquake risk awareness, gain more opportunities to maste

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Hori, Takane. "Earthquake and Tsunami Scenarios as Basic Information to Prepare Next Nankai Megathrust Earthquakes." Journal of Disaster Research 12, no. 4 (2017): 775–81. http://dx.doi.org/10.20965/jdr.2017.p0775.

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This paper describes earthquake and tsunami scenarios as basic information for preparing for the next Nankai megathrust earthquakes. Models to clarify the size of the Nankai megathrust earthquake and changes in occurrence intervals, simulations using such models, and simulations of crustal deformations and tsunamis based on the simulations were employed. This paper re-examines past earthquakes and tsunamis, the possibility of slightly larger earthquakes and tsunamis, their sizes, the necessity of countermeasures against subsidence caused by earthquakes in the Inland Sea, the possibility of the

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Omote, Syun'itiro. "Earthquake Disasters and Earthquake Engineering in Japan." Journal of Disaster Research 1, no. 1 (2006): 26–45. http://dx.doi.org/10.20965/jdr.2006.p0026.

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Major earthquakes occur somewhere every year with accompanying devastations. For example, the center of the city of Managua was destroyed completely in December 1972 with the loss of more than 15,000 lives. Government buildings also did not escape destruction which brought about a paralysis in Governmental functioning for a short time. In April of the same year, in Iran an earthquake of magnitude 6.9 attacked the town of Ghir causing the loss of 5,000 lives. Large earthquakes accompanied by large losses of life occur frequently in Iran. Another type of earthquake destruction was caused in Peru

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Justo, J. L., and C. Salwa. "The 1531 Lisbon earthquake." Bulletin of the Seismological Society of America 88, no. 2 (1998): 319–28. http://dx.doi.org/10.1785/bssa0880020319.

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Abstract In January 1531, the Tagus River Estuary was hit by a strong earthquake, the intensity of which in Lisbon was, according to relevant authors, greater than that of the 1755 earthquake. It was cited by most of the European annalists of the time and was responsible for the destruction of structures, the loss of lives, and enormous panic, thus making it one of the most disastrous earthquakes in the history of Portugal. If we give credit to the detailed descriptions, the maximum intensity was probably X MSK. According to our study, the seismic event was probably caused by the Lower Tagus f

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Simanjuntak, Andrean V. H., and Olymphia Olymphia. "Perbandingan Energi Gempa Bumi Utama dan Susulan (Studi Kasus : Gempa Subduksi Pulau Sumatera dan Jawa)." Jurnal Fisika FLUX 14, no. 1 (2017): 19. http://dx.doi.org/10.20527/flux.v14i1.3776.

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Indonesia is located on the third meeting of the active tectonic world plates which are Eurasian Indian - Australia and the Pacific Plate. This condition makes Indonesia as a tectonically active area with seismicity level or pattern of high seismicity. Occurrence of devastating earthquake followed by aftershocks of earthquakes, often increase the level of social unrest. The purpose of this study is calculate the energy of devastating earthquakes and followed by aftershocks, so it can be compared to the amount of energy released by both of them. By obtaining these comparisons, the study is base

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Pırtı, Atınç. "Investigation of the effects of Kahramanmaraş earthquake series on Cyprus Arc, Dead Sea fault, Hatay regions and stations close to two earthquakes epicenters." Geodesy and cartography 50, no. 3 (2024): 113–26. http://dx.doi.org/10.3846/gac.2024.19634.

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In various parts of the globe, there have been several earthquakes of a modest size. Monitoring the change of the points over time is a key component of typical techniques for extracting dynamic responses. This technique was unable to completely extract all of the earthquake’s dynamic properties. The GNSS precise point positioning (PPP) may be a useful tool for obtaining values of the point’s displacement that are more exact up to millimeters, which can help to overcome these flaws and evaluate the seismic wave of such earthquakes. Ultimately, PPP is a crucial tool for getting the precise obse

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Obara, Kazushige, and Takuya Nishimura. "Main Results from the Program Promotion Panel for Subduction-Zone Earthquakes." Journal of Disaster Research 15, no. 2 (2020): 87–95. http://dx.doi.org/10.20965/jdr.2020.p0087.

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Understanding the occurrence mechanism of subduction zone earthquakes scientifically is intrinsically important for not only forecast of future subduction earthquakes but also disaster mitigation for strong ground motion and tsunami accompanied by large earthquakes. The Program Promotion Panel for Subduction-zone earthquakes mainly focused on interplate megathrust earthquakes in the subduction zones and the research activity included collection and classification of historical data on earthquake phenomena, clarifying the current earthquake phenomena and occurrence environment of earthquake sou

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Meng, Qingjun, Benchun Duan, and Bin Luo. "Using a dynamic earthquake simulator to explore tsunami earthquake generation." Geophysical Journal International 229, no. 1 (2021): 255–73. http://dx.doi.org/10.1093/gji/ggab470.

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SUMMARY Observations of historical tsunami earthquakes reveal that ruptures of these earthquakes propagate slowly at shallow depth with longer duration, depletion in high-frequency radiation and larger discrepancy of Mw–Ms than ordinary megathrust earthquakes. They can effectively generate tsunami and lead to huge damage to regional populated areas near the coast. In this study, we use a recently developed dynamic earthquake simulator to explore tsunami earthquake generation from a physics-based modelling point of view. We build a shallow-dipping subduction zone model in which locally locked,

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Wang, Xi, Zeyuan Zhong, Yuechen Yao, et al. "Small Earthquakes Can Help Predict Large Earthquakes: A Machine Learning Perspective." Applied Sciences 13, no. 11 (2023): 6424. http://dx.doi.org/10.3390/app13116424.

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Earthquake prediction is a long-standing problem in seismology that has garnered attention from the scientific community and the public. Despite ongoing efforts to understand the physical mechanisms of earthquake occurrence, there is no convincing physical or statistical model for predicting large earthquakes. Machine learning methods, such as random forest and long short-term memory (LSTM) neural networks, excel at identifying patterns in large-scale databases and offer a potential means to improve earthquake prediction performance. Differing from physical and statistical approaches to earthq

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KORKMAZ, Burak Can. "The Position and Importance of Earthquake Education in the World." EDUCATIONE 2, no. 2 (2023): 246–61. http://dx.doi.org/10.58650/educatione.1330891.

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Earthquake education is significant for students to raise awareness and improve knowledge related to earthquakes. Literature on earthquakes emphasizes that people with high awareness and increased knowledge can effectively cope with the devastating effects. At this point, traditional teaching methods, such as drills and theoretical lessons, are inadequate, but innovative methods like virtual reality (VR) technology is more promising. However, there is no consensus on the ideal type of earthquake education. In the world, earthquake education significantly differs. Even though some countries are

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Jiao, Yuyu, and Nobuoto Nojima. "Probabilistic Tsunami Hazard Assessment Considering the Sequence of the First and Second Earthquakes Along the Nankai Trough." Journal of Disaster Research 18, no. 8 (2023): 839–51. http://dx.doi.org/10.20965/jdr.2023.p0839.

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The Earthquake Research Committee (ERC) of the Headquarters for Earthquake Research Promotion conducted a probabilistic tsunami hazard assessment due to large earthquakes along the Nankai Trough for the next 30 years. Utilizing the basic data of earthquake source models and calculated maximum tsunami heights, the authors propose a method to evaluate the hazard curves of the first and second earthquakes separately, considering the sequence of earthquake occurrence in one cycle of large earthquake activities along the Nankai Trough. First, based on the relative weights allocated to the 176 occur

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Kaneko, Hiroyuki. "Evaluation of Tsunami Disasters Caused by the 1923 Great Kanto Earthquake." Journal of Disaster Research 18, no. 6 (2023): 578–89. http://dx.doi.org/10.20965/jdr.2023.p0578.

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The 1923 Great Kanto Earthquake is one of the earthquakes that have occurred multiple times in the past as part of the Sagami Trough earthquakes. These earthquakes, which occurred at the plate boundary, occurred in 1495 (Meio Earthquake), 1703 (Genroku Earthquake), and again in 1923, causing significant damage to various areas in Kanto, including Tokyo and Yokohama, and it came to be known as the Great Kanto Earthquake. The Sagami Trough earthquakes have consistently brought strong tsunami disasters to various areas in Kanto, extending from the Sagami Bay coast to the Boso Peninsula, and resid

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Kerr, R. A. "Earthquake--or Earthquack?" Science 250, no. 4980 (1990): 511. http://dx.doi.org/10.1126/science.250.4980.511.

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Reitherman, Robert. "Earthquakes that have initiated the development of earthquake engineering." Bulletin of the New Zealand Society for Earthquake Engineering 39, no. 3 (2006): 145–57. http://dx.doi.org/10.5459/bnzsee.39.3.145-157.

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The recent 75th anniversary of the 1931 Hawke’s Bay Earthquake reminds us that a particular earthquake can have a great effect on the development of engineering methods to contend with this natural hazard. Factors other than the occurrence of a single earthquake are also present before and after such a historically important event, and there are examples of countries that began on the path toward modern earthquake engineering in the absence of any particular earthquake playing an important causal role. An earthquake that was large in seismological (e.g. magnitude) or engineering (e.g. destruct

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Inoue, Yuta, Kazutomo Ohashi, Yuko Ohno, et al. "Pregnant women’s migration patterns before childbirth after large-scale earthquakes and the added impact of concerns regarding radiation exposure in Fukushima and five prefectures." PLOS ONE 17, no. 8 (2022): e0272285. http://dx.doi.org/10.1371/journal.pone.0272285.

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The 2011 Great East Japan Earthquake (within Fukushima, Iwate, and Miyagi prefectures) was a complex disaster; it caused a tsunami and the Fukushima Daiichi Nuclear Power Plant accident, resulting in radiation exposure. This study investigated the earthquake’s effects on the migration patterns of pregnant women and their concerns regarding radiation exposure. We also considered the following large-scale earthquakes without radiation exposure: Great Hanshin-Awaji (Hyogo prefecture), Niigata-Chuetsu, and Kumamoto. Pregnant women were categorized as outflow and inflow pregnant women. Data on the

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Khalisa, Cut Lutfia, Halida Yunita, and Munira Sungkar. "Analysis of the Value of Maximum Ground Acceleration in Earthquake Disaster Mitigation Efforts on the Lan." E3S Web of Conferences 476 (2024): 01021. http://dx.doi.org/10.1051/e3sconf/202447601021.

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The Aceh region itself has a location that is within the scope of the Sumatran fault, areas on active faults can experience a high possibility of earthquakes. Earthquake epicenters on the mainland can occur due to shifts in the Sumatran fault which is indicated by the number of earthquakes along the fault and generally has shallow depths. The research was conducted to determine the value of the earthquake acceleration on the ground around the East Aceh Alue Genteng bridge. The results of this study found that the magnitude of the earthquake can affect the level of acceleration of the earthquak

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Maslyaev, A. V. "RUSSIAN CONSTRUCTION SYSTEM DOES NOT RECOGNIZE THE IMPACT OF REPEATED EARTHQUAKES ON CONSTRUCTION SITES." ASJ. 1, no. 38 (2020): 41–49. http://dx.doi.org/10.31618/asj.2707-9864.2020.1.38.12.

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Today, many learned builders know that earthquakes in the territory of, for example, a settlement can manifest themselves in the form of the first most powerful earthquake (main underground shock), which is usually followed by a series of weaker repeated earthquakes (repetitive shocks). There are many examples of such a sequence of manifestations of strong earthquakes in a certain territory, when tens of thousands of people die in destroyed buildings during repeated exposure earthquakes. It is thanks to these examples that scientists, builders, understand the main cause of death due to repeate

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Zhang, Tao, Guangyuan Tan, Weihua Bai, et al. "A Disturbance Frequency Index in Earthquake Forecast Using Radio Occultation Data." Remote Sensing 15, no. 12 (2023): 3089. http://dx.doi.org/10.3390/rs15123089.

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Earthquake forecasting is the process of forecasting the time, location, and magnitude of an earthquake, hoping to gain some time to prepare to reduce the disasters caused by earthquakes. In this paper, the possible relationship between the maximum electron density, the corresponding critical frequency, and the occurrence of earthquakes is explored by means of radio occultation data based on mechanism analysis and actual earthquake-nearby data. A new disturbance frequency index is proposed in this paper as a novel method to help forecast earthquakes. Forecasting of the location and timing of e

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Yulita, Tiara, Chaterine Theresia Lubis, and Agus Sofian Eka Hidayat. "PENENTUAN PREMI MURNI DI KABUPATEN KEPAHIANG PROVINSI BENGKULU DENGAN MEMPERHITUNGKAN PELUANG KEJADIAN GEMPA BUMI DAN RASIO KERUSAKAN BANGUNAN." VARIANCE: Journal of Statistics and Its Applications 5, no. 2 (2023): 147–58. http://dx.doi.org/10.30598/variancevol5iss2page147-158.

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Indonesia is a country that is very vulnerable to earthquakes, one of which is in Bengkulu Province, especially Kepahiang Regency. To deal with risks or losses caused by earthquakes, insurance can be purchased. Therefore, in this study, earthquake insurance premiums will be determined by taking into account the probability of an earthquake occurring and the ratio of damage to buildings in Kepahiang Regency. The PSHA (Probabilistic Seismic Hazard Analysis) method is used to determine the probability of an earthquake occurring. In the PSHA process, earthquake data will be collected and analyzed

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Monica, Fadilla, Vira Friska, Deasy Arisa, and Marzuki Marzuki. "Comparison of Deformation Vectors Due to Earthquake in Subduction Zone and Sumatran Fault for Each Phase of Earthquake Cycle." JURNAL ILMU FISIKA | UNIVERSITAS ANDALAS 14, no. 2 (2022): 73–85. http://dx.doi.org/10.25077/jif.14.2.73-85.2022.

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This study compares the deformation in West Sumatra due to the earthquakes in the subduction zone and the Sumatran Fault. The Mw6.0 Mentawai earthquake 2019 with a thrust fault mechanism and the Mw5.4 South Solok earthquake 2019 with a strike-slip fault mechanism were used as case studies for the subduction zone and Sumatran Fault, respectively. The deformation was observed using 12 SuGAr (Sumatra GPS Array) and 8 InaCORS (Indonesian Continuously Operating Reference Station) stations, which were processed using GAMIT/GLOBK software. There are differences in the deformation vectors of the two e

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Zhang, Yihe. "Causes and recommendations for post-disaster reconstruction earthquake in Turkey." Applied and Computational Engineering 9, no. 1 (2023): 210–15. http://dx.doi.org/10.54254/2755-2721/9/20230091.

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Earthquake, also known as ground motion and ground vibration, is a natural phenomenon caused by the rapid release of energy from the earth's crust, during which seismic waves are generated. The current level of science and technology cannot predict the arrival of earthquakes, and earthquakes will be unpredictable for a long time in the future. The so-called examples of successful earthquake prediction are basically coincidences. For earthquakes, what we should do is to improve the seismic level of buildings and do a good job of defence, rather than predicting earthquakes. Turkey experienced a

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Rubinstein, Justin L., Andrew J. Barbour, and Jack H. Norbeck. "Forecasting Induced Earthquake Hazard Using a Hydromechanical Earthquake Nucleation Model." Seismological Research Letters 92, no. 4 (2021): 2206–20. http://dx.doi.org/10.1785/0220200215.

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Abstract In response to the dramatic increase in earthquake rates in the central United States, the U.S Geological Survey began releasing 1 yr earthquake hazard models for induced earthquakes in 2016. Although these models have been shown to accurately forecast earthquake hazard, they rely purely on earthquake statistics because there was no precedent for forecasting induced earthquakes based upon wastewater injection data. Since the publication of these hazard models, multiple physics-based methods have been proposed to forecast earthquake rates using injection data. Here, we use one of these

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Madlazim, M. "COULOMB STRESS CHANGES DUE TO RECENT ACEH EARTHQUAKES." Jurnal Penelitian Fisika dan Aplikasinya (JPFA) 5, no. 1 (2015): 9. http://dx.doi.org/10.26740/jpfa.v5n1.p9-14.

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Coulomb stress change analysis has been applied to understand whether the 2013/07/02 (Mw=6.1) has been triggered by 2013/01/21 earthquake (Mw=6.1) the proximity to failure on the Aceh segment of Sumatra Fault Zone (SFZ). We examine the problem of how one earthquake might trigger another using Coulomb stress changes plotting. To plot the Coulomb stress changes, we used Global CMT data for the both earthquakes and used GEOFON data for manually revised epicenters of its aftershocks. The earthquakes are located on Aceh segment of the historic no recorded large earthquake. Coulomb stress changes mo

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Cao, Xu-Yang. "An Iterative PSD-Based Procedure for the Gaussian Stochastic Earthquake Model with Combined Intensity and Frequency Nonstationarities: Its Application into Precast Concrete Structures." Mathematics 11, no. 6 (2023): 1294. http://dx.doi.org/10.3390/math11061294.

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Earthquakes cause severe damage to human beings and financial development, and they are commonly associated with a lot of uncertainties and stochastic factors regarding their frequency, intensity and duration. Thus, how to accurately select an earthquake record and determine an earthquake’s influence on structures are important questions that deserve further investigation. In this paper, the author developed an iterative power spectral density (PSD)-based procedure for the Gaussian stochastic earthquake model with combined intensity and frequency nonstationarities. In addition, they applied th

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Chang, J. C., D. A. Lockner, and Z. Reches. "Rapid Acceleration Leads to Rapid Weakening in Earthquake-Like Laboratory Experiments." Science 338, no. 6103 (2012): 101–5. http://dx.doi.org/10.1126/science.1221195.

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After nucleation, a large earthquake propagates as an expanding rupture front along a fault. This front activates countless fault patches that slip by consuming energy stored in Earth’s crust. We simulated the slip of a fault patch by rapidly loading an experimental fault with energy stored in a spinning flywheel. The spontaneous evolution of strength, acceleration, and velocity indicates that our experiments are proxies of fault-patch behavior during earthquakes of moment magnitude (Mw) = 4 to 8. We show that seismically determined earthquake parameters (e.g., displacement, velocity, magnitud

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Lv, Zhao. "The Seismic Analysis of an Exhibition in Shanxi." Applied Mechanics and Materials 275-277 (January 2013): 1540–43. http://dx.doi.org/10.4028/www.scientific.net/amm.275-277.1540.

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In order to quantify the goal of earthquake-proof, such as minor earthquake, earthquake repair and earthquake does not fall, the project will analyze the seismic performance in three stages according to the sub-structure of small earthquakes, moderate earthquake, large earthquake. First, in the small earthquakes stage the method of MIDAS finite element analysis software will be used to calculate and analyze, meanwhile, the method of flexible schedule analysis will be as a supplementation to seismic checking. Second, in the stage of moderate earthquake, the data is calculated by adjusting the c

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Li, Siyuan, Yuanzhi Zhou, and Qiuming Cheng. "Unveiling Temporal Cyclicities in Seismic b-Values and Major Earthquake Events in Japan by Local Singularity Analysis and Wavelet Methods." Fractal and Fractional 8, no. 6 (2024): 359. http://dx.doi.org/10.3390/fractalfract8060359.

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Studying the temporal characteristics of earthquake activity contributes to enhancing earthquake prediction capabilities. The seismic b-value is a key indicator describing the relationship between seismic frequency and magnitude. This study investigates the correlation between the occurrence of major earthquakes and seismic b-values using earthquake activity records in Japan from 1990 to 2023. Local singularity analysis and wavelet analysis of earthquake frequency and b-value time series reveal significant 5-year periodic features in seismic activity in Japan. Furthermore, our research identif

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Suparmanto, Gatot, and Ika Subekti Wulandari. "Penyuluhan Kesehatan Tentang Prosedur Evakuasi Saat Terjadinya Gempa Bumi Di Desa Wonorejo Karanganyar." Pelita Masyarakat 3, no. 1 (2021): 1–5. http://dx.doi.org/10.31289/pelitamasyarakat.v3i1.5580.

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Earthquakes in Indonesia cause physical damage as well as fatalities, high mortality rates and disability when an earthquake occurs, it is necessary to reduce or prevent it by increasing people's knowledge and skills about how to evacuate during an earthquake. Earthquakes that are not resolved with resilience and lack of human resources that can handle earthquakes from pre-disaster, during disaster and post-disaster. Earthquakes are caused by the movement of the Earth's crust (Earth's plates). The frequency of a region, refers to the type and size of earthquakes experienced over a period of ti

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Jenkins, Alex, Alison Rust, and Juliet Biggs. "relationship between large earthquakes and volcanic eruptions: A global statistical study." Volcanica 7, no. 1 (2024): 165–79. http://dx.doi.org/10.30909/vol.07.01.165179.

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It is now generally accepted that large earthquakes can promote eruptions at nearby volcanoes. However, the prevalence of “triggered” eruptions, as well as the distance and timescale over which triggering occurs, remain unclear. Here, we use modern global earthquake and eruption records to compare volcanic eruption rates before and after large earthquakes with the time- averaged background eruption rate. We quantify the significance of observed deviations from the average eruption rate using Monte Carlo simulations. To integrate our findings with previous eruption triggering studies, we system

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Zheng, Tongyan, Lei Li, Chong Xu, and Yuandong Huang. "Spatiotemporal Analysis of Earthquake Distribution and Associated Losses in Chinese Mainland from 1949 to 2021." Sustainability 15, no. 11 (2023): 8646. http://dx.doi.org/10.3390/su15118646.

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A comprehensive earthquake hazard database is crucial for comprehending the characteristics of earthquake-related losses and establishing accurate loss prediction models. In this study, we compiled the earthquake events that have caused losses since 1949, and established and shared a database of earthquake hazard information for the Chinese mainland from 1949 to 2021. On this basis, we preliminarily analyzed the spatiotemporal distribution characteristics of 608 earthquake events and the associated losses. The results show the following: (1) The number of earthquakes is generally increasing, w

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J.Sankar*, E.V.Raghava Rao N.Chennakesavulu. "DESIGN OF G+4 HOSPITAL BUILDING FOR EARTHQUAKE RESISTANT." INTERNATIONAL JOURNAL OF ENGINEERING SCIENCES & RESEARCH TECHNOLOGY 5, no. 12 (2016): 546–52. https://doi.org/10.5281/zenodo.203980.

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It has been said that “Earthquake don’t kill people but buildings kill people”. By taking care to make the constructions earthquake proof, we cannot only reduce economic loss but also loss of precious lives. Major earthquakes in India have damaged or destroyed numerous buildings. By monitoring how buildings respond to earthquake and applying the knowledge gained engineers are improving the ability of structures to survive major earthquakes. Designing a building is always a challenge and that challenge is compounded when they are built in earthquake prone. As earth scientists learn more about g

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Hashimoto, Tetsuo, and Takashi Yokota. "Successive Occurrence of Large Earthquakes Along the Kuril Trench." Journal of Disaster Research 17, no. 6 (2022): 1059–67. http://dx.doi.org/10.20965/jdr.2022.p1059.

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Large earthquakes have repeatedly occurred from Hokkaido to the Kamchatka Peninsula along the Kuril Trench. First, we confirmed the successive occurrence of large earthquakes of similar magnitude in nearby regions and within a short time interval using earthquake catalogs issued by international organizations. The searching criteria was whether a succeeding earthquake (Mw ≥ 7.75) had occurred within 500 km and 3 years of a preceding earthquake (Mw ≥ 7.70) in the period between 1890 and 2014. The pairs of successively occurring earthquakes were the June 1893 and March 1894 earthquakes, the Sept

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Fauzi. "Factors Influencing the Selection of Housing Location Post Earthquake 2007 in Solok." JURNAL PEMBANGUNAN WILAYAH & KOTA 8, no. 1 (2016): 13. http://dx.doi.org/10.14710/pwk.v8i1.11554.

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ABSTRACTSolok City is within range of the Sumatera active fault where destructive earthquakes have happenedfrequently (Padang Panjang earthquake 1926, Singkarak earthquake 1943 and 2004, and Solokearthquake 2007). Problems arise when most of the population often quickly forget the danger offuture earthquakes and the mitigation efforts to reduce disaster hazards. New housings were stillbuilt in areas highly prone to earthquakes. The study investigated the factors affecting thelocational choice for housing in post‐earthquake Solok City using qualitative descriptive format.Post earthquake locatio

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Erlangga, Wisnu, Mochamad Teguh, Malik Mushthofa, Imam Trianggoro Saputro, and Gunawan Setiadi. "SEBARAN GEMPA UTAMA BERDASARKAN MAGNITUDO DAN KEDALAMAN DI WILAYAH MAMUJU DAN SEKITARNYA." Teknisia 27, no. 2 (2022): 122–31. http://dx.doi.org/10.20885/teknisia.vol27.iss2.art6.

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Sulawesi is one of Indonesia's large islands with a high vulnerability to earthquakes due to its geographical location, which lies between the confluence of tectonic plates and several active faults. The earthquake events' intensity was relatively high with small to large magnitudes. One area recently hit by a large earthquake that caused material losses and casualties was found in Mamuju. Given this condition, it is essential to determine the latest seismicity mitigation in the Mamuju area and its surroundings to look at the distribution of the mainshock based on the magnitude and depth of th

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Van Dissen, R., J. Begg, and Y. Awata. "Preliminary paleoearthquake investigations of active faults on Awaji Island, Japan, in relation to the 1995 Great Hanshin (Kobe) earthquake." Bulletin of the New Zealand Society for Earthquake Engineering 29, no. 3 (1996): 172–77. http://dx.doi.org/10.5459/bnzsee.29.3.172-177.

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Approximately one year after the Great Hanshin (Kobe) Earthquake, two New Zealand geologists were invited to help with the Geological Survey of Japan's paleoearthquake/active fault studies in the Kobe/Awaji area. Trenches excavated across the Nojima fault, which ruptured during the Great Hanshin Earthquake, showed evidence of past surface rupture earthquakes, with the age of the penultimate earthquake estimated at approximately 2000 years. A trench across the Higashiura fault, located 3-4 km southeast of the Nojima fault, revealed at least two past surface rupture earthquakes. The timing of th

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