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Earthquake Disaster Simulation in Immersive 3D Environment
Earthquake Disaster Simulation in Immersive 3D Environment

... be professionals related to construction industry, search-and-rescue professionals, engineering/ architecture faculty and students, government officials or other specific target groups, with each group influencing the simulation details. The selection is also affected by exact training purpose, whic ...
KE3418281832
KE3418281832

Model - KFUPM Faculty List
Model - KFUPM Faculty List

... stacked data, and applying coherence to each volume. In general, stacking all the data into a single volume using an inaccurate velocity smears the data, thereby increasing the overall coherence of the image, blurring edges and other discontinuities. While having lower fold and hence exhibiting lowe ...
Seismic Waves
Seismic Waves

... out in all directions. The rocks then rebound to their former shapes but at new locations relative to each other. Fault ...
Earthquakes and the Earth`s Interior
Earthquakes and the Earth`s Interior

Multi-Story Wood Construction
Multi-Story Wood Construction

... average home for 1,194 years.4 ...
Stress evolution following the 1811–1812 large earthquakes in the
Stress evolution following the 1811–1812 large earthquakes in the

earthquakes and earth`s interior
earthquakes and earth`s interior

Interpreting Earthquake Magnitude Data
Interpreting Earthquake Magnitude Data

Global pattern of earthquakes and seismic energy distributions
Global pattern of earthquakes and seismic energy distributions

... that can be considered a lower bound for energy accuracy. More recently, Kagan (2003) has re-evaluated the magnitude accuracy by testing different catalogues, obtaining an upper bound for the standard deviation of 0.275 that would increase the energy uncertainty to about 95%. The problem of magnitud ...
Earthquakes in South Carolina
Earthquakes in South Carolina

Term Project Exercise 1
Term Project Exercise 1

Document
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... Comparisons of source durations scaled for event moment (following the procedure of Bilek and Lay [1999]) also suggest variations between the earthquakes. The normalized source durations for these events are 6.7 s (1983), 3.7 s (1990), and 3.5 s (1999), clearly distinguishing the 1983 Osa earthquake ...
Earthquake Hazards and Large Dams in Western China
Earthquake Hazards and Large Dams in Western China

... seismic hazard. The remaining 50.4 percent are located in zones of moderate seismic hazard, and only 1.4 percent are located in zones of low seismic hazard (see Table 3). With respect to power generation capacity, 67.2 percent of the combined total megawatt capacity is located in high to very high s ...
Notes - Earthquakes 2 - Seismic Waves / HW Questions
Notes - Earthquakes 2 - Seismic Waves / HW Questions

Lithospheric Plates, Benioff Zones, and Volcanoes
Lithospheric Plates, Benioff Zones, and Volcanoes

A Multivariate Non-Parametric Hazard Model for Earthquake
A Multivariate Non-Parametric Hazard Model for Earthquake

... the temporal domain, by selecting small seismic areas where the hypothesis of spatially homogeneous sampling probably holds. Unfortunately, these small areas do not usually contain a sufficient number of earthquakes to test adequately any hypothesis and model (Jackson and Kagan, 1993). For this reas ...
recent experience and practice for strong motion observation in china
recent experience and practice for strong motion observation in china

... With the lack of digital strong motion stations, most of central city in China, learned the lessons of Wenchuan Earthquake, plan to install a dense strong-motion network around the city. In Law of the People’s Republic of China on Protecting Against and Mitigating Earthquake Disasters, Article 31 me ...
Mica, deformation fabrics and the seismic properties of the
Mica, deformation fabrics and the seismic properties of the

... The sample is typical of Nanga Parbat massif gneisses, containing quartz, plagioclase and orthoclase feldspars, together with abundant biotite and muscovite micas that contribute to the domains of strong S and C foliations. The domainal nature of the deformation allows the two distinct fabric elemen ...
Accelerating Seismicity and Stress Accumulation Before Large
Accelerating Seismicity and Stress Accumulation Before Large

EARTHQUAKE VULNERABILITY MAPPING OF RESIDENTIAL BUILDINGS BASED ON
EARTHQUAKE VULNERABILITY MAPPING OF RESIDENTIAL BUILDINGS BASED ON

estimation of input seismic energy by means
estimation of input seismic energy by means

... where tr is the total duration of the acceleration trace. The introduction of CAD, also allows a combination of the definitions of the significant and bracketed duration, since the gradient of the time integral is equal to the absolute velocity. For each ground motion, a threshold relative to a perc ...
designing structures in expansive clay
designing structures in expansive clay

Key_Personnel_files/Corsair Resume
Key_Personnel_files/Corsair Resume

... back, soil nail and MSE walls on the project. The proximity of the US 54 bridge to the tie back walls required that spread footings used to support the existing US 54 bridge be underpinned with micro piling. Mr. Galvan designed the footing underpinning details and provided construction phasing detai ...
MS Earthquakes Worksheets
MS Earthquakes Worksheets

... The earliest earthquake scale was the Mercalli scale. This scale measures earthquake intensity. There are several problems with the Mercalli scale. The damage from an earthquake is affected by many things in addition to the energy released during the quake. Also, different people may experience an e ...
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Seismic retrofit



Seismic retrofitting is the modification of existing structures to make them more resistant to seismic activity, ground motion, or soil failure due to earthquakes. With better understanding of seismic demand on structures and with our recent experiences with large earthquakes near urban centers, the need of seismic retrofitting is well acknowledged. Prior to the introduction of modern seismic codes in the late 1960s for developed countries (US, Japan etc.) and late 1970s for many other parts of the world (Turkey, China etc.), many structures were designed without adequate detailing and reinforcement for seismic protection. In view of the imminent problem, various research work has been carried out. State-of-the-art technical guidelines for seismic assessment, retrofit and rehabilitation have been published around the world - such as the ASCE-SEI 41 and the New Zealand Society for Earthquake Engineering (NZSEE)'s guidelines. These codes must be regularly updated; the 1994 Northridge earthquake brought to light the brittleness of welded steel frames, for example.The retrofit techniques outlined here are also applicable for other natural hazards such as tropical cyclones, tornadoes, and severe winds from thunderstorms. Whilst current practice of seismic retrofitting is predominantly concerned with structural improvements to reduce the seismic hazard of using the structures, it is similarly essential to reduce the hazards and losses from non-structural elements. It is also important to keep in mind that there is no such thing as an earthquake-proof structure, although seismic performance can be greatly enhanced through proper initial design or subsequent modifications.
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