资源简介

% CREWES elastic finite-difference seismic modelling % The top boundary is a free surface suitable for propagating surface % (Rayleigh) waves. %% CREWES elastic finite-difference seismic modelling % The top boundary is a free surface suitable for propagating surface % (Rayleigh) waves. %

资源截图

代码片段和文件信息

clear;
clc;

fm=30;
dt=0.001;
t=dt:dt:1;
dist=1:48;
t0=0.05;
tran=48;
data=zeros(100048);
v(1)=100;v(2)=300;v(3)=500;


s=(1-2*(pi.*fm.*(t-t0)).^2).*exp(-(pi.*fm.*(t-t0)).^2);
dt1=1/v(1);dt2=1/v(2);dt3=1/v(3);
for j=1:3
dtt=dist/v(j);
for luoi=1:tran
ds=round(dtt(luoi)/dt);
tem=zeros(10001);
tem(ds:end)=s(1:length(data(ds:endluoi)));
data(:luoi)=data(:luoi)+tem;
end
end
 seiplot(data48100010.0010.5);

 属性            大小     日期    时间   名称
----------- ---------  ---------- -----  ----
     文件         437  2013-08-23 19:54  F-K\dizhenjilu.m
     文件        4239  2013-08-23 19:54  F-K\fftrl.m
     文件        1523  2013-08-23 19:54  F-K\fk_separate.m
     文件        4145  2013-08-23 19:54  F-K\fktran.m
     文件        4032  2013-08-23 19:54  F-K\ifftrl.m
     文件        2265  2013-08-23 19:54  F-K\zhenyuanmoni.m
     目录           0  2015-09-17 13:01  F-K\

评论

共有 条评论