scholarly journals TUYABUGUZ EARTHQUAKE on May 25, 2013 with КР=14.1, МS=5.2, I0=7 (Tashkent district, Uzbekistan)

2019 ◽  
pp. 397-408 ◽  
Author(s):  
M. Usmanova ◽  
A. Djuraev ◽  
A. Frolova ◽  
U. Nurmato ◽  
D. Ikramova ◽  
...  
Keyword(s):  
Field Equation ◽  
Active Zone ◽  
Epicentral Zone ◽  
Isoseismal Map ◽  
Macroseismic Field ◽  
Macroseismic Observations ◽  
Focal Area ◽  
Observation Area

The results of instrumental and macroseismic observations of the Tuyabuguz earthquake on May 24, 2013, with КР=14.1, МS=5.2, I0=7 (MSK-64) are presented. The earthquake occurred 35 km southwest of Tashkent and was felt up in many settlements of Uzbekistan. The isoseismal map is given. Correspondence between the intensity of the earthquake manifestation and the regional macroseismic field equation is shown. Geological and geophysical conditions in the epicentral zone are described. The seismicity of the observation area is reviewed. The focal area of the Tuyabuguz earthquake is located in the seismically active zone, where strong historical and instrumentally recorded events occurred with intensity I=7–8 point.

scholarly journals MARJANBULAK EARTHQUAKE on MAY 25, 2013 with КР=14.1, МS=5.2, I0=7 (Djizakh province, Uzbekistan)

2019 ◽  
pp. 409-420
Author(s):  
M. Usmanova ◽  
A. Djuraev ◽  
M. Shermatov ◽  
A. Frolova ◽  
A. Sattarova
Keyword(s):  
Field Equation ◽  
Epicentral Zone ◽  
Instrumental Data ◽  
Isoseismal Map ◽  
Macroseismic Field ◽  
Observation Area ◽  
Geological Conditions ◽  
Engineer Geological ◽  
Macroseismic Survey

The instrumental data and the results of the macroseismic survey of the Marjanbulak earthquake MwMOS=6.2 with an intensity of 8 on the MSK-64 scale, which occurred in Uzbekistan, are presented. The isoseismal map is given. Correspondence between the intensity of the earthquake manifestation and the regional macroseismic field equation is shown. Geological and geophysical, engineer-geological conditions in the epicentral zone are described. The seismicity of the observation area is reviewed.

scholarly journals KAJI-SAIEARTHQUAKEonNovember 14, 2014 withКР=13.7, Mw=5.4, I0=7 (Kyrgyzstan, SouthernIssyk-Kul’)

2020 ◽  
pp. 364-374
Author(s):  
V. Grebennikova ◽  
A. Frolova ◽  
N. Bagmanova ◽  
A. Berezina ◽  
A. Pershina ◽  
...  
Keyword(s):  
Main Shock ◽  
Weather Conditions ◽  
Reverse Fault ◽  
Depth Range ◽  
Southern Coast ◽  
Epicentral Zone ◽  
Isoseismal Map ◽  
Fault Type ◽  
Macroseismic Survey ◽  
H 20

Information on the earthquake with Mw=5.4 that occurred on the southern coast of the Issyk-Kul lake on the southwestern slope of the Tegerek mountains (Kyrgyzstan) on November 14, 2014 is given. The epicenter is located in the Jumgalo-Terskey zone, identified as the Tonsky block, in which felt earthquakes with intensity up to 7 have occurred repeatedly. 231 aftershocks were recorded in the first day, in the second day – 13 aftershocks, then seismic activity decreased. Most of the aftershocks are localized in the depth range of 17–21 km, close to the depth of the main shock (h=20 km). The earthquake had the reverse fault type. Macroseismic survey was fulfilled only in the epicentral zone due to the complex weather conditions (late autumn, highlands). The theoretical isoseismal map was created for receiving the more complete picture of the earthquake impact outside of its epicentral zone.

scholarly journals Determination of parameters of historical earthquakes based on macroseismic data

2020 ◽  
Vol 2 (1) ◽  
pp. 62-75
Author(s):  
Vladlen Cardanets
Keyword(s):  
Field Equation ◽  
Focal Depth ◽  
Historical Earthquakes ◽  
Seismic Effect ◽  
Macroseismic Data ◽  
Earthquake Parameters ◽  
Macroseismic Field ◽  
Carpathian Region ◽  
Wide Range ◽  
Determination Of Parameters

The paper attempts to determine the main parameters of historical earthquakes of the Carpathian region based on macroseismic data, using the macroseismic field equation, indirect parameters, and complex comparison with modern earthquakes. So far, the main source of information about the parameters of historical earthquakes in the Carpathian region has been "New catalog of strong earthquakes ...". In this catalog, all parameters are defined very ap-proximately, with a wide range of values. In addition, over the forty-year period since the release of the catalog, the initial macroseismic data of Carpathian region earthquakes have been substantially replenished and re-evaluated using the MSK-64 macroseismic scale. The study determined such basic parameters of historical earthquakes as the macroseismic epicenter, the intensity at the epicenter, focal depth, and magnitude. As well as additional parameters: direction of the maximum macro-seismic effect, area of intensity zones, distance, and azimuth to the extreme point where the earthquake was felt. The earthquake parameters were calculated using the attenuation formula of the macroseismic field with coefficients obtained by the R.Z. Burtiev for intermediate earthquakes of the Vrancea zone of the Carpathian region, separately in four azimuthal ranges. For crustal earthquakes, the general Blake-Shebalin macroseismic field equation was used. Despite possible errors associated with a correct assessment of intensity at observation points, as well as the accuracy of the coefficients of the macro-seismic field equation used for specific seismic events, it was possible to determine the type of each historical earthquake and obtain more accurate values of their parameters. The re-fined parameters of historical earthquakes will allow making a more holistic picture of the seismic hazard in the Carpathian region.

Comparison of ultra high resolution immersion lens CFESEM and TEM for imaging of semiconductor devices

1990 ◽  
Vol 48 (4) ◽  
pp. 622-623
Author(s):  
Terrence Reilly ◽  
Al Pelillo ◽  
Barbara Miner
Keyword(s):  
High Resolution ◽  
Sample Preparation ◽  
Cross Sections ◽  
Semiconductor Devices ◽  
Ion Milling ◽  
Observation Area ◽  
Transmission Electron ◽  
Milling Machines ◽  
Resolution Imaging ◽  
Electron Microscopes

The use of transmission electron microscopes (TEM) has proven to be very valuable in the observation of semiconductor devices. The need for high resolution imaging becomes more important as the devices become smaller and more complex. However, the sample preparation for TEM observation of semiconductor devices have generally proven to be complex and time consuming. The use of ion milling machines usually require a certain degree of expertise and allow a very limited viewing area. Recently, the use of an ultra high resolution "immersion lens" cold cathode field emission scanning electron microscope (CFESEM) has proven to be very useful in the observation of semiconductor devices. Particularly at low accelerating voltages where compositional contrast is increased. The Hitachi S-900 has provided comparable resolution to a 300kV TEM on semiconductor cross sections. Using the CFESEM to supplement work currently being done with high voltage TEMs provides many advantages: sample preparation time is greatly reduced and the observation area has also been increased to 7mm. The larger viewing area provides the operator a much greater area to search for a particular feature of interest. More samples can be imaged on the CFESEM, leaving the TEM for analyses requiring diffraction work and/or detecting the nature of the crystallinity.

PERKEMBANGANKAWASAN PECINAN SEMARANG

2017 ◽  
Vol 10 (6) ◽  
pp. 361
Author(s):  
Monica Latu Melati ◽  
Ariadne Kristia Nataya ◽  
Alfonsus Arianto Wibowo
Keyword(s):  
Urban Form ◽  
Secondary Data ◽  
Primary Data ◽  
Physical Factors ◽  
Review Analysis ◽  
Urban Heritage ◽  
Observation Area ◽  
Cultural Artefact ◽  
History Of ◽  
Special District

Abstract:Semarang Chinatown  is a special  district in Semarang City  known with its chineese culture, where chineese citizen of Semarang have been living  for centuries. The sustained chineese culture in this area makes Semarang Chinatwon as an urban heritage and cultural artefact in Semarang City. The aims for this paper are to investigate the factors shaping Chinatown Semarang, the development of Chinatown Semarang from time  to time, the urban form elements in Semarang Chinatown, and the correlation between morphological components of Semarang Chinatown. This writing use some review methods, first theoritical overview to get secondary data about physical or non-physical factors forming city, second observation area such as collecting photos and interviewing to get primary data. Data review analysis use qualitative data analysis which is configure with the problems and aims that have been appointed.Keywords:elements of urban form, morphological components, history of Semarang ChinatownAbstrak: Kawasan Pecinan Semarang adalah sebuah kawasan di kota Semarang yang sangat kental dengan budaya Tionghoa. Di sinilah warga keturunan Tionghoa sejak berabad-abad silam menetap di Semarang. Adanya budaya Tionghoa yang masih sangat terjaga menjadikan Kawasan Pecinan Semarang ini sebagai kawasan urban heritage dan artefact budaya di kota Semarang. Tujuan penulisan adalah untuk menemukan faktor pembentuk Kawasan Pecinan Semarang, mengetahui perkembangan Kawasan Pecinan Semarang dari masa ke masa, mengetahui pola bentuk dan elemen kawasan pada Kawasan Pecinan Semarang, serta mengetahui kaitan antara faktor pembentuk kawasan terhadap perkembangan Kawasan Pecinan Semarang. Penulisan ini menggunakan metode kajian berupa tinjauan teori untuk memperoleh data sekunder mengenai faktor-faktor pembentuk kota baik secara fisik maupun non fisik, serta observasi lapangan berupa pengumpulan foto yang dilengkapi dengan wawancara untuk memperoleh data primer. Analisis data kajian dilakukan dengan menggunakan analisis data kualitatif yang disesuaikan dengan permasalahan dan tujuan yang telah ditetapkan.Kata kunci:Elemen Kawasan, Faktor Pembentuk Kawasan, PerkembanganSejarah Kawasan Pecinan Semarang

ON A PERFECT FLUID K¨ AHLER SPACETIME

2016 ◽  
Vol 12 (3) ◽  
pp. 4350-4355
Author(s):  
VIBHA SRIVASTAVA ◽  
P. N. PANDEY
Keyword(s):  
Field Equation ◽  
Perfect Fluid ◽  
Sectional Curvature ◽  
Einstein Field Equation ◽  
Cosmological Term ◽  
Conformal Killing ◽  
Killing Vectors ◽  
Projectively Flat ◽  
Conformal Killing Vectors

The object of the present paper is to study a perfect fluid K¨ahlerspacetime. A perfect fluid K¨ahler spacetime satisfying the Einstein field equation with a cosmological term has been studied and the existence of killingand conformal killing vectors have been discussed. Certain results related to sectional curvature for pseudo projectively flat perfect fluid K¨ahler spacetime have been obtained. Dust model for perfect fluid K¨ahler spacetime has also been studied.

THE EMPIRICAL GREEN’S FUNCTION TECHNIQUE MODIFICATION FOR ACCELEROGRAM SYNTHESIS IN LOWSEISMICITY REGIONS

2018 ◽  
Vol 12 (5-6) ◽  
pp. 72-80
Author(s):  
A. A. Krylov
Keyword(s):  
Green’S Function ◽  
Green's Function ◽  
Main Shock ◽  
Amplitude Spectrum ◽  
Strong Motion ◽  
Function Technique ◽  
Focal Region ◽  
Empirical Green’S Function ◽  
Epicentral Zone ◽  
Empirical Green's Function

In the absence of strong motion records at the future construction sites, different theoretical and semi-empirical approaches are used to estimate the initial seismic vibrations of the soil. If there are records of weak earthquakes on the site and the parameters of the fault that generates the calculated earthquake are known, then the empirical Green’s function can be used. Initially, the empirical Green’s function method in the formulation of Irikura was applied for main shock record modelling using its aftershocks under the following conditions: the magnitude of the weak event is only 1–2 units smaller than the magnitude of the main shock; the focus of the weak event is localized in the focal region of a strong event, hearth, and it should be the same for both events. However, short-termed local instrumental seismological investigation, especially on seafloor, results usually with weak microearthquakes recordings. The magnitude of the observed micro-earthquakes is much lower than of the modeling event (more than 2). To test whether the method of the empirical Green’s function can be applied under these conditions, the accelerograms of the main shock of the earthquake in L'Aquila (6.04.09) with a magnitude Mw = 6.3 were modelled. The microearthquake with ML = 3,3 (21.05.2011) and unknown origin mechanism located in mainshock’s epicentral zone was used as the empirical Green’s function. It was concluded that the empirical Green’s function is to be preprocessed. The complex Fourier spectrum smoothing by moving average was suggested. After the smoothing the inverses Fourier transform results with new Green’s function. Thus, not only the amplitude spectrum is smoothed out, but also the phase spectrum. After such preliminary processing, the spectra of the calculated accelerograms and recorded correspond to each other much better. The modelling demonstrate good results within frequency range 0,1–10 Hz, considered usually for engineering seismological studies.

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