نتایج جستجو برای: numerical seismogram
تعداد نتایج: 333110 فیلتر نتایج به سال:
برد عددی ماتریس مربعی a را با w(a) نشان داده و به این صورت تعریف می کنیم w(a)={x8ax:x ?s1} ، که در آن s1 گوی واحد است. در سال 2009، راسل کاردن مساله برد عددی معکوس را به این صورت مطرح کرده است : برای نقطه z?w(a)، بردار x?s1 را به گونه ای می یابیم که z=x*ax، در این پایان نامه ، الگوریتمی برای حل مساله برد عددی معکوس ارانه می دهیم.
The Cretaceous shale intervals of Talhar and Sembar Formations – distributed in the Lower Indus Basin Pakistan are organic-rich shales that can act as gas plays. Two-dimensional seismic using synthetic modeling has been carried out Khewari oil field to identify petroleum This work was completed with help eight processed migrated lines. Based on structural interpretation different geological str...
INTRODUCTION IN 1953, through cooperation of the Bernard Price Geophysical Institute of the University of the Witwatersrand and the University of Natal, a Columbia University-type long-period seismometer (To = 15 sec., Tg = 75 sec.) was installed in the seismological observatory of the University of Natal at Pietermaritzburg, Union of South Africa. This instrument was well situated for receivin...
Accurately predicting the seismic wavefield is important for physics-based earthquake hazard studies and dependent on an accurate source model, a good model of subsurface geology, full physics wave propagation. Here, we conduct numerical experiments to investigate effect different representations Southern California Earthquake Center Harvard community velocity models waveform predictions in vic...
An Efficient Approach to the Seismogram Synthesis for a Basin Structure Using Propagation Invariants
The AN-Lamer method is one of the cheapest methods for synthetic seismograms in irregularly layered media. In this article, we propose a new approach for a two-dimensional S H problem, solved originally by Aki and Lamer (1970). This new approach is not only based on the Rayleigh ansatz used in the original AkiLamer method but also uses further information on wave fields, i.e., the propagation i...
Abstacto We present a correction to a paper by Data Okal and Anderson (1975) about multiple ScS travel-time anomalies. We have reanalyzed data We use the same data as O&A; two deep Peruvian for ScS 2 surface bounces in the South Atlantic events recorded at two South African WWSSN Ocean. From these data n ScS2-S residual of 2Bi6 stations. In addition,we also use seismograms seconds was found by ...
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