Terrain correction for gravity data using Nagy, 1973

% A function to perform terrain corrections using the Nagy 
% prism formula. 
% To calculate the terrain correction for a block of topography
% with coordinates (x1,y1) (x2,y1) (x1,y2) (x2,y2) in the x,y plane and
% height h.
%......................................
%............___________
%.........../!........./!?.............
%........../_!________/.!?.............
%..........!.!.......!..!h ............
%..........!.!.......!..!?.............  
%..........!.!.......!..!?.............  
%..........!.!.......!..!?.............  
%..........!.!(x1,y2)!..!(x2,y2).......  
%..........!./.......!./............... 
%(x1,y1)...!/________!/(x2,y1).........
% 
% with density rho;
% the terrain correction T is given by
% T = nagyprism(x1,x2,y1,y2,h,rho)
% 
% The function can handle vectors of coordinates so that correction
% for mutiple pieces of terrain can also be calculated
function [terrc] = nagyprism(x1,x2,y1,y2,h,rho)
twopiG = 0.0419; % for g in mgal, h in m and rho in Mg/m3
G=twopiG/(2*pi);
fac11=sqrt(x1.^2+y1.^2);
fac11h=sqrt(x1.^2+y1.^2+h.^2);
fac12=sqrt(x1.^2+y2.^2);
fac12h=sqrt(x1.^2+y2.^2+h.^2);
fac21=sqrt(x2.^2+y1.^2);
fac21h=sqrt(x2.^2+y1.^2+h.^2);
fac22=sqrt(x2.^2+y2.^2);
fac22h=sqrt(x2.^2+y2.^2+h.^2);
fac2h=sqrt(y2.^2+h.^2);
fac1h=sqrt(y1.^2+h.^2);
y2h=y2.^2+h.^2;
y1h=y1.^2+h.^2;
terrc=x2.*(log( (y2+fac22)./(y2+fac22h))-...
    log( (y1+fac21)./(y1+fac21h))) -...
    x1.*( log( (y2+fac12)./(y2+fac12h))-log( (y1+fac11)./(y1+fac11h))) +...
    y2.*(log( (x2+fac22)./(x2+fac22h))-log( (x1+fac12)./(x1+fac12h))) -...
    y1.*(log( (x2+fac21)./(x2+fac21h))-log( (x1+fac11)./(x1+fac11h))) +...
    h.*(asin( (y2h +y2.*fac22h)./( (y2+fac22h).*fac2h))-...
    asin( (y2h +y2.*fac12h)./( (y2+fac12h).*fac2h))-...
    asin( (y1h +y1.*fac21h)./( (y1+fac21h).*fac1h))+...
    asin( (y1h +y1.*fac11h)./( (y1+fac11h).*fac1h)));
terrc=sum(G.*rho.*terrc);
end

文章作者: 物探网
版权声明: 本博客所有文章除特別声明外,均采用 CC BY 4.0 许可协议。转载请注明来源 物探网 !
 上一篇
康拉德面 康拉德面
地球内部的次级不连续面。在地壳中平均深度约20km(指陆地)处。其深度变化较大,最深约40km,陆地最浅约10km,海洋上明显浅得多,甚至没有。 一般认为此面以上平均化学组成与花岗岩相似(密度2.7左右),以下的一层与玄武岩相似(密度2.
2012-04-27
下一篇 
Ten kinds of state analysis in the English submission process Ten kinds of state analysis in the English submission process
Ten kinds of state analysis in the English submission process, the following are ten states in the English submission pr
2012-03-12
  目录