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Cost Modeling of Reinforced Concrete Buildings Designed for
Cost Modeling of Reinforced Concrete Buildings Designed for

... and loading characteristics including the importance of the building based on its utility. The structural configuration which is evolved from architectural and functional requirements refers to the overall building geometry, column spacing with the resulting beam spans and slab systems. The loading ...
? AN  EVALUATION OF  CHINESE ANNUAL
? AN EVALUATION OF CHINESE ANNUAL

... at the time they are made they are confidential. An objective evaluation of the CSB predictions is certainly worthwhile. In this paper, we evaluate the CSB predictions in the 1990s only, because since 1990 the form of these CSB predictions has been more uniform. Our evaluation is based on the origin ...
Research on the Earthquake Disaster Thematic Electric Map
Research on the Earthquake Disaster Thematic Electric Map

Structure and evolution of the "Olistostrome" - E
Structure and evolution of the "Olistostrome" - E

Possible stress states adjacent to the rupture
Possible stress states adjacent to the rupture

Quaternary
Quaternary

non-ductile rc frames and alternative improved
non-ductile rc frames and alternative improved

... technologies and related educational initiatives. RC frame construction is frequently used in regions of high seismic risk across the world. Recent earthquakes have revealed major seismic deficiencies in these buildings, some of which led to catastrophic collapses and significant death tolls. Causes ...
102_2012_Wang_et_al_.. - Description
102_2012_Wang_et_al_.. - Description

Canterbury Earthquakes – Impact on the Ministry
Canterbury Earthquakes – Impact on the Ministry

shear-wave splitting, new geophysics, and earthquake stress
shear-wave splitting, new geophysics, and earthquake stress

Your continued donations keep Wikipedia running! Reflection
Your continued donations keep Wikipedia running! Reflection

... the transition zone and marine (shallow and deep water): Land - The land environment is self explanatory, but can cover just about every type of terrain that exists on Earth (such as jungle, desert, arctic tundra, swamp, forest, urban settings, mountain regions and savannah). Transition Zone (TZ) - ...
Vortex Tectonics: The Primary Factors Which
Vortex Tectonics: The Primary Factors Which

... the exact middle of the arctic circle and that the Earth rotates sedately around it at a constant speed. This is, however, a geographical illusion created by our need for maps. In reality the location of the spin axis is unstable and the axis is constantly changing location by as much as 15 meters ( ...
IOSR Journal of Mechanical and Civil Engineering (IOSR-JMCE) e-ISSN: 2278-1684,p-ISSN: 2320-334X,
IOSR Journal of Mechanical and Civil Engineering (IOSR-JMCE) e-ISSN: 2278-1684,p-ISSN: 2320-334X,

... Abstract: This paper deals with the step-by-step retrofitting of buildings by using steel plate shear walls (SPSWs) with the aid of SAP2000 programme. One type of reinforced concrete building is selected for evaluation. This building represents the most used forms of residential buildings in the Sud ...
OBSERVED BEHAVIOR OF SEISMICALLY ISOLATED BUILDINGS
OBSERVED BEHAVIOR OF SEISMICALLY ISOLATED BUILDINGS

2003 Miyagi-Hokubu (Japonya) - YERBİLİMLERİ
2003 Miyagi-Hokubu (Japonya) - YERBİLİMLERİ

... have been recently undertaken to progress on short-term prediction. As also shown by the author, the stress rates derived from the GPS deformation rates can be effectively used to locate the areas with high seismic risk. Furthermore, daily variations of derived strain-stress rates from dense GPS net ...
Earthquake geotechnical engineering practice
Earthquake geotechnical engineering practice

... damaging ground shaking at a site. Ground failure from site instability, soil softening especially liquefaction, and lateral spreading are significant earthquake hazards. The design of foundations, retaining structures, roads, and buried infrastructure to resist earthquake shaking and ground failure ...
Earthquake Disasters in China
Earthquake Disasters in China

Earthquake swarm and b-value characterization of the Yellowstone
Earthquake swarm and b-value characterization of the Yellowstone

... and geographic network coverage with more instruments. This left 23,054 events in the data set hereafter referred to as the catalog of earthquakes. The average MC for the time period of 1984 to 2006 is 1.0, and only 10% of the earthquakes have MC > 2.0. Earthquake swarms were then identified and were ...
Earthquake Tips
Earthquake Tips

Deaths and Injuries due to the Earthquake in Armenia: A Cohort
Deaths and Injuries due to the Earthquake in Armenia: A Cohort

Deliverable 3.2 - version 2 - Website for the dissemination of long
Deliverable 3.2 - version 2 - Website for the dissemination of long

... complemented with the descriptions of the steps that the SHARE catalogue underwent since its first release in April 2011, which are briefly summarized in the following. 1. SHEEC was first released on 13 April 2011, as deliverable D3.2 of the Project. The catalogue was made available as two separate ...
Performance-Based Seismic Design Code for Buildings in Japan
Performance-Based Seismic Design Code for Buildings in Japan

... produce the maximum possible effects on the structural safety of a building. The possible level of a maximum earthquake is determined on the basis of historical earthquake data, past recorded strong motions, seismic and geologic tectonics, active faults and other factors. This earthquake motion leve ...
Two species of microcracks
Two species of microcracks

... volume of material to be examined is small (a sample in a laboratory stress-cell, say), AE can be used to study FFM microcracks as they open (Lockner, 1993). If the volume to be examined is large enough to be spanned by several seismic wavelengths (a volume of in situ rock, say), a range of seismic ...
Subduction of the Chile Ridge - Geological Society of America
Subduction of the Chile Ridge - Geological Society of America

Seismicity models based on Coulomb stress calculations
Seismicity models based on Coulomb stress calculations

< 1 2 3 4 5 6 7 ... 45 >

1992 Cape Mendocino earthquakes



The 1992 Cape Mendocino earthquakes (or 1992 Petrolia earthquakes) occurred along the Lost Coast of Northern California on April 25 and 26. The three largest events were the M7.2 thrust mainshock that struck near the unincorporated community of Petrolia midday on April 25 and two primary strike-slip aftershocks measuring 6.5 and 6.6 that followed early the next morning. The sequence encompassed both interplate and intraplate activity that was associated with the Mendocino Triple Junction, a complex system of three major faults (including the Cascadia subduction zone, San Andreas Fault, and Mendocino Fracture Zone) that converge near Cape Mendocino. The total number of aftershocks that followed the events exceeded 2,000.The three shocks damaged and destroyed homes and businesses in Humboldt County and injured 356 people, but the single largest loss was due to a post-earthquake fire that consumed a business center in Scotia. Accelerometers that had been in place in the Cape Mendocino area since the late 1970s recorded the event and the readings were moderate to strong, with the exception of the instruments closest to the epicenter, which went off scale a few seconds into the recording. No surface ruptures were present in the epicentral area, but landslides closed roads and railroad tracks for at least a week while cleanup took place. Also discovered was about 1 m (3 ft 3 in) of coastal uplift near Cape Mendocino and Punta Gorda.As the largest earthquake in California since the 1989 Loma Prieta event several years earlier, the mainshock caused a non-destructive tsunami that quickly reached the coast, and eventually Alaska and Hawaii several hours later. The tsunami was significant not because of its run-up, but because of the speed with which it reached the coast and for how long the waves persisted. Other strong earthquakes have affected the same area, with some that were clearly associated with the (interplate) Mendocino Fracture Zone, and others (like the two shocks on April 26) were intraplate earthquakes that ruptured within the Gorda Plate, but events that are unequivocally associated with the Cascadia subduction zone are very infrequent.
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