📄 paperinfo.aspx
字号:
<?xml version="1.0" encoding="iso-8859-1"?>
<!DOCTYPE html PUBLIC "-//W3C//DTD XHTML 1.0 Strict//EN"
"http://www.w3.org/TR/xhtml1/DTD/xhtml1-strict.dtd" >
<html xmlns="http://www.w3.org/1999/xhtml" xml:lang="en">
<head>
<title>ACTA Press • Scientific & Technical Publications • Journals, Proceedings & Papers</title>
<meta http-equiv="Content-Type" content="text/html; charset=iso-8859-1" />
<style type="text/css" media="all">
@import url("css/simple.css");
</style>
</head>
<body>
<div id="container">
<div id="main">
<div id="header">
<img id="Header2_imgLogo" src="images/actalong3.gif" alt="actapress.com" border="0" />
<img id="Header2_imgBanner" src="images/bannerbookhalf.jpg" alt="open book" border="0" style="width:720px;" />
</div>
<div id="content">
<table cellSpacing="0" cellPadding="0" width="720" border="0">
<TR>
<TD align="center"><br>
<STRONG><FONT color="#000099" size="5">
<span id="lblTitle" style="font-size:16px;">Three Dimensional Simulation of Elastic Wave Propagation in the Izmit Bay</span></FONT></STRONG></TD>
</TR>
<TR>
<TD style="HEIGHT: 35px" align="center">
<span id="lblAuthors" style="font-size:13px;">S. Üsküplü, H. Saygin, and S. Ergintav (Turkey)</span>
</TD>
</TR>
<TR>
<TD style="FONT-SIZE: 13px; HEIGHT: 30px" vAlign="bottom" align="left" width="584"><STRONG>Keywords:</STRONG>
</TD>
</TR>
<TR>
<TD><font style="LINE-HEIGHT: 5px"> </font><br>
<span id="lblKeywords" style="font-size:12px;">3-D Modeling, Earth System Modeling, Simulation, Finite
Differences</span></TD>
</TR>
<TR>
<TD align="left" width="584" style="FONT-SIZE: 13px; HEIGHT: 30px"><STRONG>Abstract:</STRONG></TD>
</TR>
<TR>
<TD align="left">
<span id="lblAbstract" style="font-size:12px;LINE-HEIGHT: 18px">One of the most important problems of the seismology
is modeling the propagation of the body and surface
waves. Lots of numerical methods are used to model
wave propagation in accordance with a realistic earth
model. In this work, a 3-D staggered-grid finite difference
scheme is presented to simulate elastic wave propagation.
3-D seismic response of the earth is computed for
the heterogeneous medium, whose density and velocity
distribution is known. Our approach is based on the
velocity and stress formulation of the wave propagation
and the formulation is discretised by a staggered-grid
finite difference scheme fourth-order accurate in space and
second-order accurate in time. This modeling approach
is applied to Eastern Marmara Sea region, Turkey. In the
aftermath of the 1999 earthquakes (Mw=7.4 and 7.2) in this
area, the general consensus has been that the floor of the
Marmara Sea became a target for the next big earthquake
of the North Anatolian Fault system. Our goal is to display
the ground response of the 1999 earthquakes and estimate
ground response of the future devastating earthquake in the
Marmara Sea.</span>
</TD>
</TR>
<TR>
<TD align="left" style="FONT-SIZE: 13px; "><br>
<span id="lblDOI" style="font-size:12px;"></span>
</TD>
</TR>
<TR>
<TD align="left" height="10"> </TD>
</TR>
<TR>
<TD align="left"><br>
<span id="lblParent" style="font-size:12px;"><i>From Proceeding</i> <a href='Content_Of_Proceeding.aspx?ProceedingID=242'>(410) Applied Simulation and Modelling - 2003</a></span>
</TD>
</TR>
<TR>
<TD align="left" height="10"> </TD>
</TR>
<TR>
<TD align="left"><span id="lblAddToCart"><a href='PaperInfo.aspx?PaperToCart=15593'>Add this paper to Cart</a></span></TD>
</TR>
<TR>
<TD align="left" height="30">
</TD>
</TR>
</table>
</div>
</td>
</tr>
</table>
</FORM>
</div>
</div>
</body>
</html>⌨️ 快捷键说明
复制代码
Ctrl + C
搜索代码
Ctrl + F
全屏模式
F11
切换主题
Ctrl + Shift + D
显示快捷键
?
增大字号
Ctrl + =
减小字号
Ctrl + -